! $Id: dust_dead_mod.f,v 1.11 2007/03/29 20:31:15 bmy Exp $ MODULE DUST_DEAD_MOD 3 ! !****************************************************************************** ! Module DUST_DEAD_MOD contains routines and variables from Charlie Zender's ! DEAD dust mobilization model. Most routines are from Charlie Zender, but ! have been modified and/or cleaned up for inclusion into GEOS-Chem. ! (tdf, rjp, bmy, 4/6/04, 1/25/07) ! ! %%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%% ! %%% NOTE: The current [dust] code was validated at 2 x 2.5 resolution. %%% ! %%% We have found that running at 4x5 we get much lower (~50%) dust %%% ! %%% emissions than at 2x2.5. Recommend we either find a way to scale %%% ! %%% the U* computed in the dust module, or run a 1x1 and store the the %%% ! %%% dust emissions, with which to drive lower resolution runs. %%% ! %%% -- Duncan Fairlie, 1/25/07 %%% ! %%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%% ! %%% NOTE: [We'll] implement the [dust] code in the standard [GEOS-Chem] %%% ! %%% model and put a warning about expected low bias when the simulation %%% ! %%% is run at 4x5. Whoever is interested in running dust at 4x5 in the %%% ! %%% future can deal with making the fix. %%% ! %%% -- Daniel Jacob, 1/25/07 %%% ! %%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%%% ! ! Module Variables: ! ============================================================================ ! (1 ) GAS_CNST_UNV (REAL*8 ) : Universal gas constant [J/mol/K ] ! (2 ) MMW_H2O (REAL*8 ) : Mean mol wt (MMW) of water [kg/mol ] ! (3 ) MMW_DRY_AIR (REAL*8 ) : Mean mol wt (MMW) of dry air [kg/mol ] ! (4 ) CST_VON_KRM (REAL*8 ) : Von Karman constant [fraction] ! (5 ) GRV_SFC (REAL*8 ) : Acceleration due to gravity [m/s2 ] ! (6 ) GAS_CST_DRY_AIR (REAL*8 ) : Gas constant of dry air [J/kg/K ] ! (7 ) RDS_EARTH (REAL*8 ) : Equivalent earth radius [m ] ! (8 ) GAS_CST_H2O (REAL*8 ) : Gas constant of H2O [J/kg/K ] ! (9 ) SPC_HEAT_DRY_AIR (REAL*8 ) : Specific heat of dry air, Cp [J/kg/K ] ! (10) TPT_FRZ_PNT (REAL*8) : Freezing point of water [K ] ! (11) GRV_SFC_RCP (REAL*8) : 1/GRV_SFC [s2/m ] ! (12) CST_VON_KRM_RCP (REAL*8) : 1/CST_VON_KRM [fraction] ! (13) EPS_H2O (REAL*8) : MMW(H2O) / MMW(dry air) [fraction] ! (14) EPS_H2O_RCP_M1 (REAL*8) : Constant for virtual temp. [fraction] ! (15) KAPPA_DRY_AIR (REAL*8) : R/Cp (const. for pot. temp) [fraction] ! (16) DST_SRC_NBR (INTEGER) : # of size distributions in source soil ! (17) MVT (INTEGER) : ! (18) ERD_FCT_GEO (REAL*8 ) : Geomorphic erodibility ! (19) ERD_FCT_HYDRO (REAL*8 ) : Hydrologic erodibility ! (20) ERD_FCT_TOPO (REAL*8 ) : Topographic erodibility (Ginoux) ! (21) ERD_FCT_UNITY (REAL*8 ) : Uniform erodibility ! (22) MBL_BSN_FCT (REAL*8 ) : Overall erodibility factor ! (23) LND_FRC_DRY (REAL*8 ) : Dry Land Fraction [fraction] ! (24) MSS_FRC_CACO3 (REAL*8 ) : Mass Fraction of soil CaCO3 [fraction] ! (25) MSS_FRC_CLY (REAL*8 ) : Mass fraction of clay [fraction] ! (26) MSS_FRC_SND (REAL*8 ) : Mass fraction of sand [fraction] ! (27) SFC_TYP (INTEGER) : Surface type index (0..28) [unitless] ! (28) FLX_LW_DWN_SFC (REAL*8 ) : Downward Longwave flux at sfc [W/m2 ] ! (29) FLX_SW_ABS_SFC (REAL*8 ) : Solar flux absorbed by ground [W/m2 ] ! (30) TPT_GND (REAL*8 ) : Ground temperature [K ] ! (31) TPT_SOI (REAL*8 ) : Soil temperature [K ] ! (32) VWC_SFC (REAL*8 ) : Volumetric water content [m3/m3 ] ! (33) VAI_DST (REAL*8 ) : Vegetation area index [m2/m2 ] ! (34) VAI_DST_BND (REAL*8 ) : Vegetation area index-boundary [m2/m2 ] ! (35) SRC_STR (REAL*8 ) : Source strength [fraction] ! (36) SRC_STR_BND (REAL*8 ) : Source strength-boundary data [fraction] ! (37) PLN_TYP (INTEGER) : LSM plant type index (1-14) [number ] ! (38) PLN_FRC (REAL*8 ) : Plant type weights (sums to 1) [unitless] ! (39) TAI (REAL*8 ) : monthly LAI + Stem Area Index [fraction] ! (40) DMT_VWR (REAL*8 ) : Mass weighted diameter resolved[m ] ! (41) DNS_AER (REAL*8 ) : Particle density [kg/m3 ] ! (42) OVR_SRC_SNK_FRC (REAL*8 ) : Mass Overlap fraction (Mij p5) [fraction] ! (43) OVR_SRC_SNK_MSS (REAL*8 ) : Mass fraction [fraction] ! (44) OROGRAPHY (INTEGER) : 0=ocean; 1=land; 2=ice [unitless] ! (45) DMT_MIN (REAL*8 ) : Bin diameter -- minimums [m ] ! (46) DMT_MAX (REAL*8 ) : Bin diameter -- maximums [m ] ! (47) DMT_VMA_SRC (REAL*8 ) : D'Almeida's (1987) bkgr modes [m ] ! (48) GSD_ANL_SRC (REAL*8 ) : Geometric std deviation [fraction] ! (49) MSS_FRC_SRC (REAL*8 ) : Mass fraction BSM96 p.73 [fraction] ! (50) SRCE_FUNC (REAL*8 ) : GOCART source function [fraction] ! ! Module Routines: ! ============================================================================ ! (1 ) DST_MBL : Driver routine for dust mobilization ! (2 ) SOI_TXT_GET : Gets latitude slice of soil texture ! (3 ) SFC_TYP_GET : Gets latitude slice of surface type ! (4 ) TPT_GND_SOI_GET : Gets latitude slice of soil & gnd tmp ! (5 ) VWC_SFC_GET : Gets latitude slice of VWC ! (6 ) DSVPDT_H2O_LQD_PRK78_FST_SCL : Gets deriv of vapor pressure over water ! (7 ) DSVPDT_H2O_ICE_PRK78_FST_SCL : Gets deriv of vapor pressure over ice ! (8 ) SVP_H2O_LQD_PRK78_FST_SCL : Gets saturation vapor press. over water ! (9 ) SVP_H2O_ICE_PRK78_FST_SCL : Gets saturation vapor press. over ice ! (10) TPT_BND_CLS_GET : Gets temperature in C (-50 < T < 50 C) ! (11) GET_ORO : Gets 2-D orography array ! (12) HYD_PRP_GET : Gets hydrologic properties of soil ! (13) CND_TRM_SOI_GET : Gets thermal properties of soil ! (14) TRN_FSH_VPR_SOI_ATM_GET : Gets factor of transfer from soil->atm ! (15) BLM_MBL : Gets boundary-layer exchange properties ! (16) ORO_IS_OCN : Returns TRUE for ocean grid boxes ! (17) ORO_IS_LND : Returns TRUE for land grid boxes ! (18) ORO_IS_ICE : Returns TRUE for ice grid boxes ! (19) MNO_STB_CRC_HEAT_UNS_GET : Returns M-O stab corr factor for heat ! (20) MNO_STB_CRC_MMN_UNS_GET : Returns M-0 stab corr factor for mom. ! (21) XCH_CFF_MMN_OCN_NTR_GET : Returns neutral 10m drag coefficient ! (22) RGH_MMN_GET : Sets the roughness length ! (23) SNW_FRC_GET : Converts LW snow depth to snow cover ! (24) WND_RFR_GET : Interpolates wind speed to ref. hght ! (25) WND_FRC_THR_SLT_GET : Gets dry friction vel. for saltation ! (26) WND_RFR_THR_SLT_GET : Gets threshold U-wind for saltation ! (27) VWC2GWC : Converts VWC to GWC ! (28) FRC_THR_NCR_WTR_GET : Gets factor: soil moist. incr. USTAR ! (29) FRC_THR_NCR_DRG_GET : Gets factor: roughness incr. USTAR ! (30) WND_FRC_SLT_GET : Gets saltating fricton velocity ! (31) FLX_MSS_CACO3_MSK : Mask dust mass by CaCO3 mass fraction ! (32) FLX_MSS_HRZ_SLT_TTL_WHI79_GET : Gets vert int. streamwise mass flux ! (33) FLX_MSS_VRT_DST_TTL_MAB95_GET : Gets total vertical mass flux of dust ! (34) DST_PSD_MSS : Gets OVR_SRC_SNK_MSS mass overlap ! (35) FLX_MSS_VRT_DST_PRT : Partitions vert mass flux into bins ! (36) TM_2_IDX_WGT : Now deleted ! (37) LND_FRC_MBL_GET : Gets fraction of grid box for mobiliz. ! (38) DST_ADD_LON : Sums property w/in a dust bin ! (39) DST_TVBDS_GET : Gets a latitude slice of VAI data ! (40) OVR_SRC_SNK_FRC_GET : Gets overlap factors betwn src & sink ! (41) ERF : Driver for CALERF ! (42) CALERF : Platform independent erf(x) ! (43) PLN_TYP_GET : Returns info from land sfc model ! (44) GET_TIME_INVARIANT_DATA : Reads time-invariant fields from disk ! (45) GET_MONTHLY_DATA : Reads monthly fields from disk ! (46) INIT_DUST_DEAD : Allocates & zeroes module arrays ! (47) CLEANUP_DUST_DEAD : Deallocates ! ! GEOS-CHEM modules referenced by dust_dead_mod.f ! ============================================================================ ! (1 ) bpch2_mod.f : Module containing routines for binary punch file I/O ! (2 ) dao_mod.f : Module containing arrays for GMAO met fields ! (3 ) directory_mod.f : Module containing GEOS-CHEM data & met field dirs ! (4 ) error_mod.f : Module containing I/O error and NaN check routines ! (5 ) grid_mod.f : Module containing horizontal grid information ! (6 ) time_mod.f : Module containing routines for computing time & date ! (7 ) transfer_mod.f : Module containing routines to cast & resize arrays ! ! NOTES: ! (1 ) Added parallel DO loop in GET_ORO (bmy, 4/14/04) ! (2 ) Now references "directory_mod.f" (bmy, 7/20/04) ! (3 ) Fixed typo in ORO_IS_LND for PGI compiler (bmy, 3/1/05) ! (4 ) Modified for GEOS-5 and GCAP met fields (swu, bmy, 8/16/05) ! (5 ) Now make sure all USE statements are USE, ONLY (bmy, 10/3/05) ! (6 ) Now uses GOCART source function (tdf, bmy, 1/25/07) !****************************************************************************** ! IMPLICIT NONE !================================================================= ! MODULE PRIVATE DECLARATIONS -- keep certain internal variables ! and routines from being seen outside "dust_dead_mod.f" !================================================================= ! Make everything PRIVATE.... PRIVATE ! Except these routines PUBLIC :: DST_MBL PUBLIC :: CLEANUP_DUST_DEAD PUBLIC :: GET_ORO PUBLIC :: GET_TIME_INVARIANT_DATA PUBLIC :: GET_MONTHLY_DATA !================================================================= ! MODULE VARIABLES !================================================================= ! Fundamental physical constants REAL*8, PARAMETER :: GAS_CST_UNV = 8.31441d0 REAL*8, PARAMETER :: MMW_H2O = 1.8015259d-02 REAL*8, PARAMETER :: MMW_DRY_AIR = 28.9644d-3 REAL*8, PARAMETER :: CST_VON_KRM = 0.4d0 REAL*8, PARAMETER :: GRV_SFC = 9.80616d0 REAL*8, PARAMETER :: GAS_CST_DRY_AIR = 287.05d0 REAL*8, PARAMETER :: RDS_EARTH = 6.37122d+6 REAL*8, PARAMETER :: GAS_CST_H2O = 461.65D0 REAL*8, PARAMETER :: SPC_HEAT_DRY_AIR = 1005.0d0 REAL*8, PARAMETER :: TPT_FRZ_PNT = 273.15d0 ! Derived quantities REAL*8, PARAMETER :: GRV_SFC_RCP = 1.0d0 / GRV_SFC REAL*8, PARAMETER :: CST_VON_KRM_RCP = 1.0d0 / CST_VON_KRM REAL*8, PARAMETER :: EPS_H2O = MMW_H2O / MMW_DRY_AIR REAL*8, PARAMETER :: EPS_H2O_RCP_M1 = -1.0d0 + MMW_DRY_AIR & / MMW_H2O REAL*8, PARAMETER :: KAPPA_DRY_AIR = GAS_CST_DRY_AIR & / SPC_HEAT_DRY_AIR ! Fixed-size grid information INTEGER, PARAMETER :: DST_SRC_NBR = 3 INTEGER, PARAMETER :: MVT = 14 ! Time-invariant fields REAL*8, ALLOCATABLE :: ERD_FCT_GEO(:,:) REAL*8, ALLOCATABLE :: ERD_FCT_HYDRO(:,:) REAL*8, ALLOCATABLE :: ERD_FCT_TOPO(:,:) REAL*8, ALLOCATABLE :: ERD_FCT_UNITY(:,:) REAL*8, ALLOCATABLE :: MBL_BSN_FCT(:,:) ! GOCART source function (tdf, bmy, 1/25/07) REAL*8, ALLOCATABLE :: SRCE_FUNC(:,:) ! Land surface that is not lake or wetland (by area) REAL*8, ALLOCATABLE :: LND_FRC_DRY(:,:) REAL*8, ALLOCATABLE :: MSS_FRC_CACO3(:,:) REAL*8, ALLOCATABLE :: MSS_FRC_CLY(:,:) REAL*8, ALLOCATABLE :: MSS_FRC_SND(:,:) INTEGER, ALLOCATABLE :: SFC_TYP(:,:) ! Time-varying surface info from CTM REAL*8, ALLOCATABLE :: FLX_LW_DWN_SFC(:,:) REAL*8, ALLOCATABLE :: FLX_SW_ABS_SFC(:,:) REAL*8, ALLOCATABLE :: TPT_GND(:,:) REAL*8, ALLOCATABLE :: TPT_SOI(:,:) REAL*8, ALLOCATABLE :: VWC_SFC(:,:) ! Variables initialized in dst_tvbds_ntp() and dst_tvbds_ini() REAL*8, ALLOCATABLE :: VAI_DST(:,:) REAL*8, ALLOCATABLE :: SRC_STR(:,:) ! LSM plant type, 28 land surface types plus 0 for ocean ! Also account for 3 different land types in each grid box INTEGER, ALLOCATABLE :: PLN_TYP(:,:) REAL*8, ALLOCATABLE :: PLN_FRC(:,:) REAL*8, ALLOCATABLE :: TAI(:,:) ! Other fields REAL*8, ALLOCATABLE :: DMT_VWR(:) REAL*8, ALLOCATABLE :: DNS_AER(:) REAL*8, ALLOCATABLE :: OVR_SRC_SNK_FRC(:,:) REAL*8, ALLOCATABLE :: OVR_SRC_SNK_MSS(:,:) INTEGER, ALLOCATABLE :: OROGRAPHY(:,:) REAL*8, ALLOCATABLE :: DMT_MIN(:) REAL*8, ALLOCATABLE :: DMT_MAX(:) REAL*8, ALLOCATABLE :: DMT_VMA_SRC(:) REAL*8, ALLOCATABLE :: GSD_ANL_SRC(:) REAL*8, ALLOCATABLE :: MSS_FRC_SRC(:) !================================================================= ! MODULE ROUTINES -- follow below the "CONTAINS" statement !================================================================= CONTAINS !------------------------------------------------------------------------------ SUBROUTINE DST_MBL( DOY, HGT_MDP, LAT_IDX, 1,25 & LAT_RDN, ORO, PRS_DLT, & PRS_MDP, Q_H2O_VPR, DSRC, & SNW_HGT_LQD, TM_ADJ, TPT_MDP, & TPT_PTN_MDP, WND_MRD_MDP, WND_ZNL_MDP, & FIRST, NSTEP ) ! !****************************************************************************** ! Subroutine DST_MBL is the driver for aerosol mobilization (DEAD model). ! It is designed to require only single layer surface fields, allowing for ! easier implementation. DST_MBL is called once per latitude. Modified ! for GEOS-CHEM by Duncan Fairlie and Bob Yantosca (tdf, bmy, 1/25/07) ! ! Arguments as Input: ! ============================================================================ ! (1 ) DOY (REAL*8 ) : Day of year [1.0..366.0) [unitless] ! (2 ) HGT_MDP (REAL*8 ) : Midpoint height above surface [m ] ! (3 ) LAT_IDX (INTEGER) : Model latitude index [unitless] ! (4 ) LAT_RDN (REAL*8 ) : Model latitude [radians ] ! (5 ) ORO (REAL*8 ) : Orography [fraction] ! (6 ) PRS_DLT (REAL*8 ) : Pressure thickness of grid box [Pa ] ! (7 ) PRS_MDP (REAL*8 ) : Pressure @ midpoint of grid box [Pa ] ! (8 ) Q_H2O_VPR, (REAL*8 ) : Water vapor mixing ratio [kg/kg ] ! (9 ) SNW_HGT_LQD (REAL*8 ) : Equivalent liquid water snow depth [m ] ! (10) TM_ADJ, (REAL*8 ) : Adjustment timestep [s ] ! (11) TPT_MDP, (REAL*8 ) : Temperature [K ] ! (12) TPT_PTN_MDP (REAL*8 ) : Midlayer local potential temp. [K ] ! (13) WND_MRD_MDP (REAL*8 ) : Meridional wind component (V-wind) [m/s ] ! (14) WND_ZNL_MDP (REAL*8 ) : Zonal wind component (U-wind) [m/s ] ! (15) FIRST, (LOGICAL) : Logical used ot open output dataset [unitless] ! (16) NSTEP (INTEGER) : Iteration counter [unitless] ! ! Arguments as Output: ! ============================================================================ ! (10) DSRC ! O [kg kg-1] Dust mixing ratio increment ! ! NOTES: ! (1 ) Cleaned up and added comments. Also force double precision with ! "D" exponents. (bmy, 3/30/04) ! (2 ) Now get GOCART source function. (tdf, bmy, 1/25/07) !****************************************************************************** ! ! References to F90 modules USE DAO_MOD, ONLY : USTAR, Z0 USE GRID_MOD, ONLY : GET_AREA_M2 USE ERROR_MOD, ONLY : ERROR_STOP # include "CMN_SIZE" ! Size parameters ! Arguments INTEGER, INTENT(IN) :: LAT_IDX REAL*8, INTENT(IN) :: DOY REAL*8, INTENT(IN) :: HGT_MDP(IIPAR) REAL*8, INTENT(IN) :: LAT_RDN REAL*8, INTENT(IN) :: ORO(IIPAR) REAL*8, INTENT(IN) :: PRS_DLT(IIPAR) REAL*8, INTENT(IN) :: PRS_MDP(IIPAR) REAL*8, INTENT(IN) :: Q_H2O_VPR(IIPAR) REAL*8, INTENT(IN) :: SNW_HGT_LQD(IIPAR) REAL*8, INTENT(IN) :: TM_ADJ REAL*8, INTENT(IN) :: TPT_MDP(IIPAR) REAL*8, INTENT(IN) :: TPT_PTN_MDP(IIPAR) REAL*8, INTENT(IN) :: WND_MRD_MDP(IIPAR) REAL*8, INTENT(IN) :: WND_ZNL_MDP(IIPAR) INTEGER, INTENT(IN) :: NSTEP LOGICAL, INTENT(IN) :: FIRST REAL*8, INTENT(INOUT) :: DSRC(IIPAR,NDSTBIN) !-------------- ! Parameters !-------------- ! Global mass flux tuning factor (a posteriori) [frc] REAL*8, PARAMETER :: FLX_MSS_FDG_FCT = 7.0d-4 ! Reference height for mobilization processes [m] REAL*8, PARAMETER :: HGT_RFR = 10.0d0 ! Zero plane displacement for erodible surfaces [m] REAL*8, PARAMETER :: HGT_ZPD_MBL = 0.0d0 ! Set roughness length momentum for erodible surfaces, S&P, p. 858. [m] REAL*8, PARAMETER :: RGH_MMN_MBL = 1.0d-3 ! rgh_mmn_smt set to 33.3e-6 um, MaB95 p. 16426 recommend 10.0e-6 ! Smooth roughness length MaB95 p. 16426, MaB97 p. 4392, GMB98 p. 6207 ! [m] Z0,m,s REAL*8, PARAMETER :: RGH_MMN_SMT = 33.3d-6 ! Minimum windspeed used for mobilization [m/s] REAL*8, PARAMETER :: WND_MIN_MBL = 1.0d0 !-------------- ! Local Output !-------------- REAL*8 DST_SLT_FLX_RAT_TTL(IIPAR) ! [m-1] Ratio of vertical dust flux to ! streamwise mass flux REAL*8 FLX_MSS_HRZ_SLT_TTL(IIPAR) ! [kg/m/s] Vertically integrated ! streamwise mass flux REAL*8 FLX_MSS_VRT_DST_TTL(IIPAR) ! [kg/m2/s] Total vertical mass ! flux of dust REAL*8 FRC_THR_NCR_DRG(IIPAR) ! [frc] Threshold friction velocity ! increase from roughness REAL*8 FRC_THR_NCR_WTR(IIPAR) ! [frc] Threshold friction velocity ! increase from moisture REAL*8 FLX_MSS_VRT_DST(IIPAR,NDSTBIN) ! [kg/m2/s] Vertical mass flux ! of dust REAL*8 HGT_ZPD(IIPAR) ! [m] Zero plane displacement REAL*8 LND_FRC_MBL_SLICE(IIPAR) ! [frc] Bare ground fraction REAL*8 MNO_LNG(IIPAR) ! [m] Monin-Obukhov length REAL*8 WND_FRC(IIPAR) ! [m/s] Friction velocity REAL*8 WND_FRC_GEOS(IIPAR) ! [m/s] Friction velocity REAL*8 Z0_GEOS(IIPAR) ! [m] roughness height REAL*8 SNW_FRC(IIPAR) ! [frc] Fraction of surface covered ! by snow REAL*8 TRN_FSH_VPR_SOI_ATM(IIPAR) ! [frc] Transfer efficiency of vapor ! from soil to atmosphere REAL*8 wnd_frc_slt(IIPAR) ! [m/s] Saltating friction velocity REAL*8 WND_FRC_THR_SLT(IIPAR) ! [m/s] Threshold friction velocity ! for saltation REAL*8 WND_MDP(IIPAR) ! [m/s] Surface layer mean wind speed REAL*8 WND_RFR(IIPAR) ! [m/s] Wind speed at reference height REAL*8 WND_RFR_THR_SLT(IIPAR) ! [m/s] Threshold 10 m wind speed for ! saltation LOGICAL FLG_CACO3 ! [FLG] Activate CaCO3 tracer LOGICAL FLG_MBL_SLICE(IIPAR) ! [flg] Mobilization candidates CHARACTER(80) FL_OUT ! [sng] Name of netCDF output file INTEGER I ! [idx] Counting index INTEGER IJLOOP ! [idx] counting index INTEGER M ! [idx] Counting index INTEGER MBL_NBR ! [nbr] Number of mobilization candidates INTEGER SFC_TYP_SLICE(IIPAR) ! [idx] LSM surface type lat slice (0..28) REAL*8 CND_TRM_SOI(IIPAR) ! [W/m/K] Soil thermal conductivity REAL*8 DNS_MDP(IIPAR) ! [kg/m3] Midlayer density REAL*8 FLX_LW_DWN_SFC_SLICE(IIPAR) ! [W/m2] Longwave downwelling flux ! at surface REAL*8 FLX_SW_ABS_SFC_SLICE(IIPAR) ! [W/m2] Solar flux absorbed by ground REAL*8 LND_FRC_DRY_SLICE(IIPAR) ! [frc] Dry land fraction REAL*8 MBL_BSN_FCT_SLICE(IIPAR) ! [frc] Erodibility factor REAL*8 MSS_FRC_CACO3_SLICE(IIPAR) ! [frc] Mass fraction of CaCO3 REAL*8 MSS_FRC_CLY_SLICE(IIPAR) ! [frc] Mass fraction of clay REAL*8 MSS_FRC_SND_SLICE(IIPAR) ! [frc] Mass fraction of sand ! GOCART source function (tdf, bmy, 1/25/07) REAL*8 SRCE_FUNC_SLICE(IIPAR) ! GOCART source function REAL*8 LVL_DLT(IIPAR) ! [m] Soil layer thickness REAL*8 MPL_AIR(IIPAR) ! [kg/m2] Air mass path in layer REAL*8 TM_DLT ! [s] Mobilization timestep REAL*8 TPT_GND_SLICE(IIPAR) ! [K] Ground temperature REAL*8 TPT_SOI_SLICE(IIPAR) ! [K] Soil temperature REAL*8 TPT_SOI_FRZ ! [K] Temperature of frozen soil REAL*8 TPT_VRT_MDP ! [K] Midlayer virtual temperature REAL*8 VAI_DST_SLICE(IIPAR) ! [m2/m2] Vegetation area index, ! one-sided REAL*8 VWC_DRY(IIPAR) ! [m3/s] Dry volumetric water content ! (no E-T) REAL*8 VWC_OPT(IIPAR) ! [m3/m3] E-T optimal volumetric water ! content REAL*8 VWC_SAT(IIPAR) ! [m3/m3] Saturated volumetric water ! content (sand-dependent) REAL*8 VWC_SFC_SLICE(IIPAR) ! [m3/m3] Volumetric water content REAL*8 GWC_SFC(IIPAR) ! [kg/kg] Gravimetric water content REAL*8 RGH_MMN(IIPAR) ! [m] Roughness length momentum REAL*8 W10M ! GCM diagnostics ! Dust tendency due to gravitational settling [kg/kg/s] REAL*8 Q_DST_TND_MBL(IIPAR,NDSTBIN) ! Total dust tendency due to gravitational settling [kg/kg/s] REAL*8 Q_DST_TND_MBL_TTL(IIPAR) ! External functions REAL*8, EXTERNAL :: SFCWINDSQR !================================================================= ! DST_MBL begins here! !================================================================= ! Time step [s] TM_DLT = TM_ADJ ! Freezing pt of soil [K] -- assume it's 0C TPT_SOI_FRZ = TPT_FRZ_PNT ! Initialize output fluxes and tendencies Q_DST_TND_MBL(:,:) = 0.0D0 ! [kg kg-1 s-1] Q_DST_TND_MBL_TTL(:) = 0.0D0 ! [kg kg-1 s-1] FLX_MSS_VRT_DST(:,:) = 0.0D0 ! [kg m-2 s-1] FLX_MSS_VRT_DST_TTL(:) = 0.0D0 ! [kg m-2 s-1] FRC_THR_NCR_WTR(:) = 0.0D0 ! [frc] WND_RFR(:) = 0.0D0 ! [m s-1] WND_FRC(:) = 0.0D0 ! [m s-1] WND_FRC_SLT(:) = 0.0D0 ! [m s-1] WND_FRC_THR_SLT(:) = 0.0D0 ! [m s-1] WND_RFR_THR_SLT(:) = 0.0D0 ! [m s-1] HGT_ZPD(:) = HGT_ZPD_MBL ! [m] DSRC(:,:) = 0.0D0 !================================================================= ! Compute necessary derived fields !================================================================= DO I = 1, IIPAR ! Stop occasional haywire model runs IF ( TPT_MDP(I) > 350.0d0 ) THEN CALL ERROR_STOP( 'TPT_MDP(i) > 350.0', & 'DST_MBL ("dust_dead_mod.f")' ) ENDIF ! Midlayer virtual temperature [K] TPT_VRT_MDP = TPT_MDP(I) & * (1.0d0 + EPS_H2O_RCP_M1 * Q_H2O_VPR(I)) ! Density at center of gridbox [kg/m3] DNS_MDP(I) = PRS_MDP(I) & / (TPT_VRT_MDP * GAS_CST_DRY_AIR) ! Commented out !cApproximate surface virtual temperature (uses midlayer moisture) !c tpt_vrt_sfc=tpt_sfc(i)*(1.0+eps_H2O_rcp_m1*q_H2O_vpr(i)) ! [K] !c !c Surface density !c dns_sfc(i)=prs_sfc(i)/(tpt_vrt_sfc*gas_cst_dry_air) ! [kg m-3] ! Mass of air currently in gridbox [kg/m2] MPL_AIR(I) = PRS_DLT(I) * GRV_SFC_RCP ! Mean surface layer horizontal wind speed WND_MDP(I) = SQRT( WND_ZNL_MDP(I)*WND_ZNL_MDP(I) & + WND_MRD_MDP(I)*WND_MRD_MDP(I) ) ENDDO !================================================================= ! Gather input variables from GEOS-CHEM modules etc. !================================================================= ! Get LSM Surface type (0..28) CALL SFC_TYP_GET( LAT_IDX, SFC_TYP_SLICE ) ! Get erodability and mass fractions CALL SOI_TXT_GET( & LAT_IDX, ! I [idx] Latitude index & LND_FRC_DRY_SLICE, ! O [frc] Dry land fraction & MBL_BSN_FCT_SLICE, ! O [frc] Erodibility factor & MSS_FRC_CACO3_SLICE, ! O [frc] Mass fraction of CaCO3 & MSS_FRC_CLY_SLICE, ! O [frc] Mass fraction of clay & MSS_FRC_SND_SLICE ) ! O [frc] Mass fraction of sand ! Get GOCART source function (tdf, bmy, 1/25/07) CALL SRCE_FUNC_GET( ! GOCART source function & LAT_IDX, ! I [idx] Latitude index & SRCE_FUNC_SLICE ) ! O [frc] GOCART source function ! Get volumetric water content from GWET CALL VWC_SFC_GET( & LAT_IDX, ! I [idx] Latitude index & VWC_SFC_SLICE ) ! O [m3 m-3] Volumetric water content ! Get surface and soil temperature CALL TPT_GND_SOI_GET( & LAT_IDX, ! I [idx] Latitude index! & TPT_GND_SLICE, ! O [K] Ground temperature & TPT_SOI_SLICE ) ! O [K] Soil temperature ! Get time-varying vegetation area index CALL DST_TVBDS_GET( & LAT_IDX, ! I [idx] Latitude index & VAI_DST_SLICE) ! O [m2 m-2] Vegetation area index, one-sided ! Get fraction of surface covered by snow CALL SNW_FRC_GET( & SNW_HGT_LQD, ! I [m] Equivalent liquid water snow depth & SNW_FRC ) ! O [frc] Fraction of surface covered by snow !================================================================= ! Use the variables retrieved above to compute the fraction ! of each gridcell suitable for dust mobilization !================================================================= CALL LND_FRC_MBL_GET( & DOY, ! I [day] Day of year [1.0..366.0) & FLG_MBL_SLICE, ! O [flg] Mobilization candidate flag & LAT_RDN, ! I [rdn] Latitude & LND_FRC_DRY_SLICE, ! I [frc] Dry land fraction & LND_FRC_MBL_SLICE, ! O [frc] Bare ground fraction & MBL_NBR, ! O [flg] Number of mobilization candidates & ORO, ! I [frc] Orography & SFC_TYP_SLICE, ! I [idx] LSM surface type (0..28) & SNW_FRC, ! I [frc] Fraction of surface covered by snow & TPT_SOI_SLICE, ! I [K] Soil temperature & TPT_SOI_FRZ, ! I [K] Temperature of frozen soil & VAI_DST_SLICE) ! I [m2 m-2] Vegetation area index, one-sided ! Much ado about nothing if (mbl_nbr == 0) then ctdf print *,' no mobilisation candidates' goto 737 endif !================================================================= ! Compute time-invariant hydrologic properties ! NB flg_mbl IS time-dependent, so keep this in time loop. !================================================================= CALL HYD_PRP_GET( ! NB: These properties are time-invariant & FLG_MBL_SLICE, ! I [flg] Mobilization candidate flag & MSS_FRC_CLY_SLICE, ! I [frc] Mass fraction clay & MSS_FRC_SND_SLICE, ! I [frc] Mass fraction sand & VWC_DRY, ! O [m3/m3] Dry vol'mtric water content (no E-T) & VWC_OPT, ! O [m3/m3] E-T optimal volumetric water content & VWC_SAT) ! O [m3/m3] Saturated volumetric water content CND_TRM_SOI(:) = 0.0D0 LVL_DLT(:) = 0.0D0 !================================================================= ! Get reference wind at 10m !================================================================= DO I = 1, IIPAR W10M = SQRT( SFCWINDSQR( I, LAT_IDX ) ) ! add mobilisation criterion flag IF ( FLG_MBL_SLICE(I) ) THEN WND_RFR(I) = W10M ENDIF ENDDO !================================================================= ! Compute standard roughness length. This call is probably ! unnecessary, because we are only concerned with mobilisation ! candidates, for which roughness length is imposed in blm_mbl !================================================================= CALL RGH_MMN_GET( ! Set roughness length w/o zero plane displacement & ORO, ! I [frc] Orography & RGH_MMN, ! O [m] Roughness length momentum & SFC_TYP_SLICE, ! I [idx] LSM surface type (0..28) & SNW_FRC, ! I [frc] Fraction of surface covered by snow & WND_RFR ) ! I [m s-1] 10 m wind speed !================================================================= ! Introduce Ustar and Z0 from GEOS data !================================================================= DO I = 1, IIPAR IJLOOP = (LAT_IDX-1)*IIPAR+I ! Just assign for flag mobilisation candidates IF ( FLG_MBL_SLICE(I) ) THEN WND_FRC_GEOS(I) = USTAR(I,LAT_IDX) Z0_GEOS(I) = Z0(I,LAT_IDX) ELSE WND_FRC_GEOS(I) = 0.0D0 Z0_GEOS(I) = 0.0D0 ENDIF ENDDO !================================================================= ! Surface exchange properties over erodible surfaces ! DO NEED THIS: Compute Monin-Obukhov and Friction velocities ! appropriate for dust producing regions. ! ! Now calling Stripped down (adiabatic) version tdf 10/27/2K3 ! rgh_mmn_mbl parameter included directly in blm_mbl !================================================================= CALL BLM_MBL( & FLG_MBL_SLICE, ! I [flg] Mobilization candidate flag & RGH_MMN, ! I [m] Roughness length momentum, Z0,m & WND_RFR, ! I [m s-1] 10 m wind speed & MNO_LNG, ! O [m] Monin-Obukhov length & WND_FRC) ! O [m s-1] Surface friction velocity, U* !================================================================= ! Factor by which surface roughness increases threshold friction ! velocity. The sink of atrmospheric momentum into non-erodible ! roughness elements Zender et al., expression (3) !================================================================= !----------------------------------------------------------------------------- ! Prior to 1/25/07: ! For now, instead of calling this routine to get FRC_THR_NCR_DRG, we will ! just set it to 1 (tdf, bmy, 1/25/07) ! ! %%%%% DO NOT DELETE -- LEAVE THIS CODE COMMENTED OUT %%%%% ! ! CALL FRC_THR_NCR_DRG_GET( ! & FRC_THR_NCR_DRG, ! O [frc] Factor increases thresh. fric. veloc. ! & FLG_MBL_SLICE, ! I [flg] Mobilization candidate flag ! & RGH_MMN_MBL, ! I [m] Rgh length momentum for erodible sfcs ! & RGH_MMN_SMT ) ! I [m] Smooth roughness length, Z0,m,s !----------------------------------------------------------------------------- ! Now set roughness factor to 1.0 (tdf, bmy, 1/25/07) FRC_THR_NCR_DRG(:) = 1.0d0 !================================================================= ! Convert volumetric water content to gravimetric water content ! NB: Owen effect included in wnd_frc_slt_get !================================================================= CALL VWC2GWC( & FLG_MBL_SLICE, ! I [flg] Mobilization candidate flag & GWC_SFC, ! O [kg kg-1] Gravimetric water content & VWC_SAT, ! I [m3 m-3] Saturated VWC (sand-dependent) & VWC_SFC_SLICE ) ! I [m3 m-3] Volumetric water content !================================================================= ! Factor by which soil moisture increases threshold friction ! velocity -- i.e. the inhibition of saltation by soil mositure, ! Zender et al., exp(5). !================================================================= CALL FRC_THR_NCR_WTR_GET( & FLG_MBL_SLICE, ! I [flg] Mobilization candidate flag & FRC_THR_NCR_WTR, ! O [frc] Factor by which moisture increases ! threshold friction velocity & MSS_FRC_CLY_SLICE, ! I [frc] Mass fraction of clay & GWC_SFC) ! I [kg kg-1] Gravimetric water content !================================================================= ! Now, compute basic threshold friction velocity for saltation ! over dry, bare, smooth ground. fxm: Use surface density not ! midlayer density !================================================================= CALL WND_FRC_THR_SLT_GET( & FLG_MBL_SLICE, ! I mobilisation flag & DNS_MDP, ! I [kg m-3] Midlayer density & WND_FRC_THR_SLT ) ! O [m s-1] Threshold friction velocity ! Adjust threshold friction velocity to account ! for moisture and roughness DO I = 1, IIPAR WND_FRC_THR_SLT(I) = ! [m s-1] Threshold friction velocity ! for saltation & WND_FRC_THR_SLT(i) ! [m s-1] Threshold for dry, flat ground & * FRC_THR_NCR_WTR(i) ! [frc] Adjustment for moisture & * FRC_THR_NCR_DRG(i) ! [frc] Adjustment for roughness ENDDO ! Threshold saltation wind speed at reference height, 10m DO I = 1, IIPAR IF ( FLG_MBL_SLICE(I) ) THEN WND_RFR_THR_SLT(I) = ! [m s-1] Threshold 10 m wind speed ! for saltation & WND_RFR(I) * WND_FRC_THR_SLT(I) / WND_FRC(i) ENDIF ENDDO !================================================================= ! Saltation increases friction speed by roughening surface ! i.e. Owen effect, Zender et al., expression (4) ! ! Compute the wind friction velocity due to saltation, U*,s ! accounting for the Owen effect. !================================================================= CALL WND_FRC_SLT_GET( & FLG_MBL_SLICE, ! I [flg] Mobilization candidate flag & WND_FRC, ! I [m s-1] Surface friction velocity & WND_FRC_SLT, ! O [m s-1] Saltating friction velocity & WND_RFR, ! I [m s-1] Wind speed at reference height & WND_RFR_THR_SLT ) ! I [m s-1] Thresh. 10 m wind speed for saltation !================================================================= ! Compute horizontal streamwise mass flux, Zender et al., expr. (10) !================================================================= CALL FLX_MSS_HRZ_SLT_TTL_WHI79_GET( & DNS_MDP, ! I [kg m-3] Midlayer density & FLG_MBL_SLICE, ! I [flg] Mobilization candidate flag & FLX_MSS_HRZ_SLT_TTL, ! O [kg m-1 s-1] Vertically integrated ! streamwise mass flux & WND_FRC_SLT, ! I [m s-1] Saltating friction velocity & WND_FRC_THR_SLT ) ! I [m s-1] Threshold friction vel for saltation !----------------------------------------------------------------------------- ! Prior to 1/25/07: ! We now multiply by the GOCART source function, and we will ignore ! the MBL_BSN_FCT_SLICE. (tdf, bmy, 1/25/07) ! ! %%%%% DO NOT DELETE -- LEAVE THIS CODE COMMENTED OUT %%%%% ! !ctdf...prior to Apr/05/06 ! ! Apply land surface and vegetation limitations ! ! and global tuning factor ! DO I = 1, IIPAR ! FLX_MSS_HRZ_SLT_TTL(I) = FLX_MSS_HRZ_SLT_TTL(I) ! [kg m-2 s-1] ! & * LND_FRC_MBL_SLICE(i) ! [frc] Bare ground fraction ! & * MBL_BSN_FCT_SLICE(i) ! [frc] Erodibility factor ! & * FLX_MSS_FDG_FCT ! [frc] Global mass flux tuning ! ! factor (empirical) ! ENDDO !----------------------------------------------------------------------------- ! Now simply multiply by the GOCART source function. ! The vegetation effect has been eliminated in LND_FRC_MBL_GET ! and we also ignore MBL_BSN_FCT. (tdf, bmy, 1/25/07) DO I = 1, IIPAR FLX_MSS_HRZ_SLT_TTL(I) = FLX_MSS_HRZ_SLT_TTL(I) ! [kg m-2 s-1] & * LND_FRC_MBL_SLICE(i) ! [frc] Bare ground fraction & * FLX_MSS_FDG_FCT ! [frc] Global mass flux tuning & * SRCE_FUNC_SLICE(I) ! GOCART source function ENDDO !================================================================= ! Compute vertical dust mass flux, see Zender et al., expr. (11). !================================================================= CALL FLX_MSS_VRT_DST_TTL_MAB95_GET( & DST_SLT_FLX_RAT_TTL, ! O [m-1] Ratio of vertical dust flux to ! streamwise mass flux & FLG_MBL_SLICE, ! I [flg] Mobilization candidate flag & FLX_MSS_HRZ_SLT_TTL, ! I [kg/m/s] Vertically integrated ! streamwise mass flux & FLX_MSS_VRT_DST_TTL, ! O [kg/m2/s] Total vertical mass flux of dust & MSS_FRC_CLY_SLICE ) ! I [frc] Mass fraction clay !================================================================= ! Now, partition vertical dust mass flux into transport bins ! ! OVR_SRC_SNK_MSS needed in FLX_MSS_VRT_DST_PRT ! computed in DST_PSD_MSS, called from "dust_mod.f" (tdf, 3/30/04) !================================================================= CALL FLX_MSS_VRT_DST_PRT( & FLG_MBL_SLICE, ! I [flg] Mobilization candidate flag & FLX_MSS_VRT_DST, ! O [kg m-2 s-1] Vertical mass flux of dust & FLX_MSS_VRT_DST_TTL) ! I [kg m-2 s-1] Total vertical mass flux of dus !================================================================= ! Mask dust mass flux by tracer mass fraction at source !================================================================= FLG_CACO3 = .FALSE. ! [flg] Activate CaCO3 tracer IF ( FLG_CACO3 ) THEN CALL FLX_MSS_CACO3_MSK( & DMT_VWR, ! I [m] Mass weighted diameter resolved & FLG_MBL_SLICE, ! I [flg] Mobilization candidate flag & FLX_MSS_VRT_DST, ! I/O [kg m-2 s-1] Vert. mass flux of dust & MSS_FRC_CACO3_SLICE, ! I [frc] Mass fraction of CaCO3 & MSS_FRC_CLY_SLICE, ! I [frc] Mass fraction of clay & MSS_FRC_SND_SLICE ) ! I [frc] Mass fraction of sand endif ! Now, flx_mss_vrt_dst has units of kg/m2/sec ! Fluxes are known, so adjust mixing ratios DO I=1, IIPAR ! NB: Inefficient loop order IF (FLG_MBL_SLICE(I)) THEN ! Loop over dust bins DO M = 1, NDSTBIN !======================================================== ! Compute dust mobilisation tendency. Recognise that ! what GEOS-CHEM wants is an increment in kg...So, ! multiply by DXYP [m2] and tm_adj [sec] !======================================================== ! use get_area_m2 (Grid box surface area) [m2] instead of DXYP Q_DST_TND_MBL(I,M) = & FLX_MSS_VRT_DST(I,M) * GET_AREA_M2(LAT_IDX) ! [kg/sec] ! Introduce DSRC: dust mixing ratio increment 12/9/2K3 DSRC(I,M) = ! [kg] & TM_ADJ * Q_DST_TND_MBL(I,M) ENDDO ENDIF ENDDO ! Jump to here when no points are mobilization candidates 737 CONTINUE ! Return to calling program END SUBROUTINE DST_MBL !------------------------------------------------------------------------------ SUBROUTINE SRCE_FUNC_GET( LAT_IDX, SRCE_FUNC_OUT ) 1 ! !****************************************************************************** ! Subroutine SRCE_FUNC_GET returns a latitude slice of the GOCART source ! function. This routine is called by DST_MBL. (tdf, bmy, 1/25/07) ! ! Arguments as Input: ! ============================================================================ ! (1 ) LAT_IDX (INTEGER) : GEOS-Chem latitude index ! ! Arguments as Output: ! ============================================================================ ! (1 ) SRCE_FUNC_OUT (REAL*8 ) : GOCART source function [fraction] ! ! NOTES: !****************************************************************************** ! # include "CMN_SIZE" ! Size parameters ! Arguments INTEGER, INTENT(IN) :: LAT_IDX REAL*8, INTENT(OUT) :: SRCE_FUNC_OUT(IIPAR) ! Local variables INTEGER :: LON_IDX !================================================================= ! SRCE_FUNC_GET begins here! !================================================================= ! Loop over longitudes DO LON_IDX = 1, IIPAR ! Save latitude slice in SRCE_FUNC_OUT SRCE_FUNC_OUT(LON_IDX) = SRCE_FUNC(LON_IDX,LAT_IDX) ENDDO ! Return to calling program END SUBROUTINE SRCE_FUNC_GET !------------------------------------------------------------------------------ SUBROUTINE SOI_TXT_GET( J, LND_FRC_DRY_OUT, 1 & MBL_BSN_FCT_OUT, MSS_FRC_CACO3_OUT, & MSS_FRC_CLY_OUT, MSS_FRC_SND_OUT ) ! !****************************************************************************** ! Subroutine SOI_GET_TXT returns a latitude slice of soil texture to the ! calling program DST_MBL. (tdf, bmy, 3/30/04) ! ! Arguments as Input: ! ============================================================================ ! (1 ) J (INTEGER) : Grid box latitude index ! ! Arguments as Output: ! ============================================================================ ! (2 ) lnd_frc_dry_out (REAL*8 ) : Dry land fraction [fraction] ! (3 ) mbl_bsn_fct_out (REAL*8 ) : Erodibility factor [fraction] ! (4 ) mss_frc_CaCO3_out (REAL*8 ) : Mass fraction of CaCO3 [fraction] ! (5 ) mss_frc_cly_out (REAL*8 ) : Mass fraction of clay [fraction] ! (6 ) mss_frc_snd_out (REAL*8 ) : Mass fraction of sand [fraction] ! ! NOTES: ! (1 ) Updated comments, cosmetic changes (bmy, 3/30/04) !****************************************************************************** ! # include "CMN_SIZE" ! Arguments INTEGER, INTENT(IN) :: J REAL*8, INTENT(OUT) :: LND_FRC_DRY_OUT(IIPAR) REAL*8, INTENT(OUT) :: MBL_BSN_FCT_OUT(IIPAR) REAL*8, INTENT(OUT) :: MSS_FRC_CACO3_OUT(IIPAR) REAL*8, INTENT(OUT) :: MSS_FRC_CLY_OUT(IIPAR) REAL*8, INTENT(OUT) :: MSS_FRC_SND_OUT(IIPAR) ! Local variables INTEGER :: I ! Ad hoc globally uniform clay mass fraction [kg/kg] REAL*8, PARAMETER :: MSS_FRC_CLY_GLB = 0.20d0 !================================================================= ! SOI_GET_TXT begins here! !================================================================= DO I = 1, IIPAR ! Save dry land fraction slice LND_FRC_DRY_OUT(I) = LND_FRC_DRY(I,J) ! Change surface source distribution to "geomorphic" tdf 12/12/2K3 MBL_BSN_FCT_OUT(I) = ERD_FCT_GEO(I,J) !fxm: CaCO3 currently has missing value of ! 1.0e36 which causes problems IF ( MSS_FRC_CACO3(I,J) <= 1.0D0 ) THEN MSS_FRC_CACO3_OUT(I) = MSS_FRC_CACO3(I,J) ELSE MSS_FRC_CACO3_OUT(I) = 0.0D0 ENDIF ! fxm Temporarily set mss_frc_cly used in mobilization to globally ! uniform SGS value of 0.20, and put excess mass fraction ! into sand MSS_FRC_CLY_OUT(I) = MSS_FRC_CLY_GLB MSS_FRC_SND_OUT(I) = MSS_FRC_SND(I,J) + & MSS_FRC_CLY(I,J) - MSS_FRC_CLY_GLB ENDDO ! Return to calling program END SUBROUTINE SOI_TXT_GET !------------------------------------------------------------------------------ SUBROUTINE SFC_TYP_GET( J, SFC_TYP_OUT ) 1 ! !****************************************************************************** ! Subroutine SFC_TYP_GET returns a latitude slice of LSM surface type ! to the calling programs DST_MBL & DST_DPS_DRY. (tdf, bmy, 3/30/04) ! ! Arguments as Input: ! ============================================================================ ! (1 ) J (INTEGER) : Grid box latitude index ! ! Arguments as Output: ! ============================================================================ ! (1 ) sfc_typ_out (REAL*8 ) : LSM surface type (0..28) [unitless] ! ! NOTES ! (1 ) Updated comments & cosmetic changes (bmy, 3/30/04) !****************************************************************************** ! # include "CMN_SIZE" ! IIPAR ! Arguments INTEGER, INTENT(IN) :: J INTEGER, INTENT(OUT) :: SFC_TYP_OUT(IIPAR) ! Local variables INTEGER :: I !================================================================= ! SFC_TYP_GET begins here! !================================================================= DO I = 1, IIPAR SFC_TYP_OUT(I) = SFC_TYP(I,J) ENDDO ! Return to calling program END SUBROUTINE SFC_TYP_GET ! end sfc_typ_get() !------------------------------------------------------------------------------ SUBROUTINE TPT_GND_SOI_GET( J, TPT_GND_OUT, TPT_SOI_OUT ) 1,1 ! !****************************************************************************** ! Subroutine TPT_GND_SOI_GET returns a latitude slice of soil temperature and ! ground temperature to the calling program DST_MBL. (tdf, bmy, 3/30/04) ! ! Arguments as Input: ! ============================================================================ ! (1 ) J (INTEGER) : Grid box latitude index ! ! Arguments as Output: ! ============================================================================ ! (2 ) TPT_GND_OUT (REAL*8 ) : Ground temperature array slice [K] ! (3 ) tpt_soi_out (REAL*8 ) : Soil temperature array slice [K] ! ! NOTES ! (1 ) Updated comments & cosmetic changes (bmy, 3/30/04) !****************************************************************************** ! ! References to F90 modules USE DAO_MOD, ONLY : TS # include "CMN_SIZE" ! IIPAR ! Arguments INTEGER, INTENT(IN) :: J REAL*8, INTENT(OUT) :: TPT_GND_OUT(IIPAR) REAL*8, INTENT(OUT) :: TPT_SOI_OUT(IIPAR) ! Local variables INTEGER :: I !================================================================= ! TPT_GND_SOI_GET begins here! !================================================================= ! Use TS from GEOS-CHEM (tdf, 3/30/04) DO I = 1, IIPAR TPT_GND_OUT(I) = TS(I,J) TPT_SOI_OUT(I) = TS(I,J) ENDDO ! Return to calling program END SUBROUTINE TPT_GND_SOI_GET !------------------------------------------------------------------------------ SUBROUTINE VWC_SFC_GET( J, VWC_SFC_OUT ) 1,1 ! !****************************************************************************** ! Subroutine TPT_GND_SOI_GET returns a latitude slice of volumetric water ! content to the calling program DST_MBL. (tdf, bmy, 3/30/04) ! ! Arguments as Input: ! ============================================================================ ! (1 ) J (INTEGER) : Grid box latitude index ! ! Arguments as Output: ! ============================================================================ ! VWC_SFC_OUT (REAL*8 ) : Volumetric water content [m3/m3] ! ! NOTES ! (1 ) Updated comments & cosmetic changes (bmy, 3/30/04) !****************************************************************************** ! ! References to F90 modules USE DAO_MOD, ONLY : GWETTOP # include "CMN_SIZE" ! IIPAR ! Arguments INTEGER, INTENT(IN) :: J REAL*8, INTENT(OUT) :: VWC_SFC_OUT(IIPAR) ! Local variables INTEGER :: I !================================================================= ! VWC_SFC_GET begins here! !================================================================= DO I = 1, IIPAR VWC_SFC_OUT(I) = GWETTOP(I,J) ENDDO ! Return to calling program END SUBROUTINE VWC_SFC_GET !------------------------------------------------------------------------------ REAL*8 FUNCTION DSVPDT_H2O_LQD_PRK78_FST_SCL( TPT_CLS ) ! !****************************************************************************** ! Function DSVPDT_H2O_LQD_PRK78_FST_SCL returns the derivative of saturation ! vapor pressure [Pa] over planar liquid water (tdf, bmy, 3/30/04) ! ! Arguments as Input: ! ============================================================================ ! (1 ) TPT_CLS (REAL*8) : Temperature in Celsius [C] ! ! NOTES: ! (1 ) Updated comments, cosmetic changes. Also now force double-precision ! with "D" exponents. (bmy, 3/30/04) !****************************************************************************** ! ! Arguments REAL*8, INTENT(IN) :: TPT_CLS ! Local variables REAL*8, PARAMETER :: C0 = 4.438099984d-01 REAL*8, PARAMETER :: C1 = 2.857002636d-02 REAL*8, PARAMETER :: C2 = 7.938054040d-04 REAL*8, PARAMETER :: C3 = 1.215215065d-05 REAL*8, PARAMETER :: C4 = 1.036561403d-07 REAL*8, PARAMETER :: C5 = 3.532421810d-10 REAL*8, PARAMETER :: C6 =-7.090244804d-13 !================================================================= ! DSVPDT_H2O_LQD_PRK78_FST_SCL begins here! !================================================================= ! Return deriv. of saturation vapor pressure [Pa] DSVPDT_H2O_LQD_PRK78_FST_SCL = 100.0d0 * ( C0+TPT_CLS * & ( C1+TPT_CLS * & ( C2+TPT_CLS * & ( C3+TPT_CLS * & ( C4+TPT_CLS * & ( C5+TPT_CLS * C6 )))))) ! Return to calling program END FUNCTION DSVPDT_H2O_LQD_PRK78_FST_SCL !------------------------------------------------------------------------------ REAL*8 FUNCTION DSVPDT_H2O_ICE_PRK78_FST_SCL( TPT_CLS ) ! !****************************************************************************** ! Function DSVPDT_H2O_ICE_PRK78_FST_SCL returns the derivative of saturation ! vapor pressure [Pa] over planar ice water (tdf, bmy, 3/30/04) ! ! Arguments as Input: ! ============================================================================ ! (1 ) TPT_CLS (REAL*8) : Temperature in Celsius [C] ! ! NOTES: ! (1 ) Updated comments, cosmetic changes. Also now force double-precision ! with "D" exponents. (bmy, 3/30/04) !****************************************************************************** ! ! Arguments REAL*8, INTENT(IN) :: TPT_CLS ! Local variables REAL*8, PARAMETER :: D0 = 5.030305237d-01 REAL*8, PARAMETER :: D1 = 3.773255020d-02 REAL*8, PARAMETER :: D2 = 1.267995369d-03 REAL*8, PARAMETER :: D3 = 2.477563108d-05 REAL*8, PARAMETER :: D4 = 3.005693132d-07 REAL*8, PARAMETER :: D5 = 2.158542548d-09 REAL*8, PARAMETER :: D6 = 7.131097725d-12 !================================================================= ! DSVPDT_H2O_ICE_PRK78_FST_SCL begins here! !================================================================= ! Return deriv. of sat vapor pressure [Pa] DSVPDT_H2O_ICE_PRK78_FST_SCL = 100.0D0 * ( D0+TPT_CLS * & ( D1+TPT_CLS * & ( D2+TPT_CLS * & ( D3+TPT_CLS * & ( D4+TPT_CLS * & ( D5+TPT_CLS * D6 )))))) ! Return to calling program END FUNCTION DSVPDT_H2O_ICE_PRK78_FST_SCL !------------------------------------------------------------------------------ REAL*8 FUNCTION SVP_H2O_LQD_PRK78_FST_SCL( TPT_CLS ) ! !****************************************************************************** ! Function SVP_H2O_LQD_PRK78_FST_SCL returns the saturation vapor pressure ! over planer liquid water [Pa] See Lowe and Ficke (1974) as reported in ! PrK78 p. 625. Range of validity is -50 C < T < 50 C. (tdf, bmy, 3/30/04) ! ! Arguments as Input: ! ============================================================================ ! (1 ) TPT_CLS (REAL*8) : Temperature in Celsius [C] ! ! NOTES: ! (1 ) Updated comments, cosmetic changes. Also now force double-precision ! with "D" exponents. (bmy, 3/30/04) !****************************************************************************** ! ! Arguments REAL*8, INTENT(IN) :: TPT_CLS ! Local variables REAL*8, PARAMETER :: A0 = 6.107799961d0 REAL*8, PARAMETER :: A1 = 4.436518521d-01 REAL*8, PARAMETER :: A2 = 1.428945805d-02 REAL*8, PARAMETER :: A3 = 2.650648471d-04 REAL*8, PARAMETER :: A4 = 3.031240396d-06 REAL*8, PARAMETER :: A5 = 2.034080948d-08 REAL*8, PARAMETER :: A6 = 6.136820929d-11 !================================================================= ! SVP_H2O_LQD_PRK78_FST_SCL begins here! !================================================================= ! Return saturation vapor pressure over liquid water [Pa] SVP_H2O_LQD_PRK78_FST_SCL = 100.0D0 * ( A0+TPT_CLS * & ( A1+TPT_CLS * & ( A2+TPT_CLS * & ( A3+TPT_CLS * & ( A4+TPT_CLS * & ( A5+TPT_CLS * A6 )))))) ! Return to calling program END FUNCTION SVP_H2O_LQD_PRK78_FST_SCL !------------------------------------------------------------------------------ REAL*8 FUNCTION SVP_H2O_ICE_PRK78_FST_SCL( TPT_CLS ) ! !****************************************************************************** ! Function SVP_H2O_ICE_PRK78_FST_SCL returns the saturation vapor pressure ! [Pa] over planar ice water (tdf, bmy, 3/30/04) ! ! Arguments as Input: ! ============================================================================ ! (1 ) TPT_CLS (REAL*8) : Temperature in Celsius [C] ! ! NOTES: ! (1 ) Updated comments, cosmetic changes. Also now force double-precision ! with "D" exponents. (bmy, 3/30/04) !****************************************************************************** ! ! Arguments REAL*8, INTENT(IN) :: TPT_CLS ! Local variables REAL*8, PARAMETER :: B0 = 6.109177956d0 REAL*8, PARAMETER :: B1 = 5.034698970d-01 REAL*8, PARAMETER :: B2 = 1.886013408d-02 REAL*8, PARAMETER :: B3 = 4.176223716d-04 REAL*8, PARAMETER :: B4 = 5.824720280d-06 REAL*8, PARAMETER :: B5 = 4.838803174d-08 REAL*8, PARAMETER :: B6 = 1.838826904d-10 !================================================================= ! SVP_H2O_ICE_PRK78_FST_SCL begins here! !================================================================= ! Return saturation vapor pressure over ice [Pa] SVP_H2O_ICE_PRK78_FST_SCL = 100.0D0 * ( B0+TPT_CLS * & ( B1+TPT_CLS * & ( B2+TPT_CLS * & ( B3+TPT_CLS * & ( B4+TPT_CLS * & ( B5+TPT_CLS * B6 )))))) ! Return to calling program END FUNCTION SVP_H2O_ICE_PRK78_FST_SCL !------------------------------------------------------------------------------ REAL*8 FUNCTION TPT_BND_CLS_GET( TPT ) ! !****************************************************************************** ! Function TPT_BND_CLS_GET returns the bounded temperature in [C], ! (i.e., -50 < T [C] < 50 C), given the temperature in [K]. ! (tdf, bmy, 3/30/04) ! ! Arguments as Input: ! ============================================================================ ! (1 ) TPT (REAL*8) : Temperature in Kelvin [K] ! ! NOTES: !****************************************************************************** ! ! Arguments REAL*8, INTENT(IN) :: TPT ! Local variables REAL*8, PARAMETER :: TPT_FRZ_PNT=273.15 !================================================================= ! TPT_BND_CLS_GET begins here! !================================================================= TPT_BND_CLS_GET = MIN( 50.0D0, MAX( -50.0D0, ( TPT-TPT_FRZ_PNT)) ) ! Return to calling program END FUNCTION TPT_BND_CLS_GET !------------------------------------------------------------------------------ SUBROUTINE GET_ORO( OROGRAPHY ) 1,4 ! !****************************************************************************** ! Subroutine GET_ORO creates a 2D orography array, OROGRAPHY, from the ! GMAO LWI fields. Ocean= 0; Land=1; ice=2. (tdf, bmy, 3/30/04, 8/17/05) ! ! Arguments as Output: ! ============================================================================ ! (1 ) OROGRAPHY (INTEGER) : Array for orography flags ! ! NOTES: ! (1 ) Added parallel DO-loop (bmy, 4/14/04) ! (2 ) Now modified for GCAP and GEOS-5 met fields (swu, bmy, 6/9/05) ! (3 ) Now use IS_LAND, IS_WATER, IS_ICE functions from "dao_mod.f" ! (bmy, 8/17/05) !****************************************************************************** ! ! References to F90 modules USE DAO_MOD, ONLY : IS_LAND, IS_WATER, IS_ICE # include "CMN_SIZE" ! Arguments INTEGER, INTENT(OUT) :: OROGRAPHY(IIPAR,JJPAR) ! Local variables INTEGER :: I, J, TEMP !================================================================= ! GET_ORO begins here! !================================================================= !$OMP PARALLEL DO !$OMP+DEFAULT( SHARED ) !$OMP+PRIVATE( I, J ) DO J = 1, JJPAR DO I = 1, IIPAR ! Ocean IF ( IS_WATER( I, J ) ) OROGRAPHY(I,J) = 0 ! Land IF ( IS_LAND( I, J ) ) OROGRAPHY(I,J) = 1 ! Ice IF ( IS_ICE ( I, J ) ) OROGRAPHY(I,J) = 2 ENDDO ENDDO !$OMP END PARALLEL DO ! Return to calling program END SUBROUTINE GET_ORO !------------------------------------------------------------------------------ SUBROUTINE HYD_PRP_GET( FLG_MBL, MSS_FRC_CLY, MSS_FRC_SND, 1 & VWC_DRY, VWC_OPT, VWC_SAT ) ! !****************************************************************************** ! Subroutine HYD_PRP_GET determines hydrologic properties from soil texture. ! (tdf, bmy, 3/30/04) ! ! Arguments as Input: ! ============================================================================ ! (1 ) FLG_MBL (LOGICAL) : Mobilization candidate flag [unitless] ! (2 ) MSS_FRC_CLY (REAL*8 ) : Mass fraction clay [fraction] ! (3 ) MSS_FRC_SND (REAL*8 ) : Mass fraction sand [fraction] ! ! Arguments as Output: ! ============================================================================ ! (4 ) VWC_DRY (REAL*8 ) : Dry volumetric water content (no E-T) [m3/m3] ! (5 ) VWC_OPT (REAL*8 ) : E-T optimal volumetric water content [m3/m3] ! (6 ) VWC_SAT (REAL*8 ) : Saturated volumetric water content [m3/m3] ! ! NOTES: ! (1 ) All I/O for this routine is time-invariant, thus, the hydrologic ! properties could be computed once at initialization. However, ! FLG_MBL is time-dependent, so we should keep this as-is. ! (tdf, 10/27/03) !****************************************************************************** ! # include "CMN_SIZE" ! IIPAR ! Arguments LOGICAL, INTENT(IN) :: FLG_MBL(IIPAR) REAL*8, INTENT(IN) :: MSS_FRC_CLY(IIPAR) REAL*8, INTENT(IN) :: MSS_FRC_SND(IIPAR) REAL*8, INTENT(OUT) :: VWC_DRY(IIPAR) REAL*8, INTENT(OUT) :: VWC_OPT(IIPAR) REAL*8, INTENT(OUT) :: VWC_SAT(IIPAR) ! Local variables INTEGER :: LON_IDX ! [frc] Exponent "b" for smp (clay-dependent) REAL*8 :: SMP_XPN_B(IIPAR) ! [mm H2O] Saturated soil matric potential (sand-dependent) REAL*8 :: SMP_SAT(IIPAR) !================================================================= ! HYD_PRP_GET begins here !================================================================= ! Initialize output values VWC_DRY(:) = 0.0D0 VWC_OPT(:) = 0.0D0 VWC_SAT(:) = 0.0D0 ! Time-invariant soil hydraulic properties ! See Bon96 p. 98, implemented in CCM:lsm/lsmtci() DO LON_IDX = 1, IIPAR IF ( FLG_MBL(LON_IDX) ) THEN ! Exponent "b" for smp (clay-dependent) [fraction] SMP_XPN_B(LON_IDX) = & 2.91D0 +0.159D0 * MSS_FRC_CLY(LON_IDX) * 100.0D0 ! NB: Adopt convention that matric potential is positive definite ! Saturated soil matric potential (sand-dependent) [mm H2O] SMP_SAT(LON_IDX) = & 10.0D0 * (10.0D0**(1.88D0-0.0131D0 & * MSS_FRC_SND(LON_IDX)*100.0D0)) ! Saturated volumetric water content (sand-dependent) ! [m3 m-3] VWC_SAT(LON_IDX)= & 0.489D0 - 0.00126D0 * MSS_FRC_SND(LON_IDX)*100.0D0 ! [m3 m-3] VWC_DRY(LON_IDX) = ! Dry volumetric water content (no E-T) & VWC_SAT(LON_IDX)*(316230.0D0/SMP_SAT(LON_IDX)) & **(-1.0D0/SMP_XPN_B(LON_IDX)) ! E-T optimal volumetric water content! [m3 m-3] VWC_OPT(LON_IDX) = & VWC_SAT(LON_IDX)*(158490.0D0/SMP_SAT(LON_IDX)) & **(-1.0D0/SMP_XPN_B(LON_IDX)) ENDIF ENDDO ! Return to calling program END SUBROUTINE HYD_PRP_GET !------------------------------------------------------------------------------ SUBROUTINE CND_TRM_SOI_GET( CND_TRM_SOI, FLG_MBL, LVL_DLT, & MSS_FRC_CLY, MSS_FRC_SND, TPT_SOI, & VWC_DRY, VWC_OPT, VWC_SAT, & VWC_SFC ) ! !****************************************************************************** ! Subroutine CND_TRM_SOI_GET gets thermal properties of soil. Currently this ! routine is optimized for ground without snow-cover. Although snow ! thickness is read in, it is not currently used. (tdf, bmy, 3/30/04) ! ! Arguments as Input: ! ============================================================================ ! (3 ) lvl_dlt (REAL*8 ) : Soil layer thickness [m ] ! (4 ) mss_frc_cly (REAL*8 ) : Mass fraction clay [frac.] ! (5 ) mss_frc_snd (REAL*8 ) : Mass fraction sand [frac.] ! (6 ) tpt_soi (REAL*8 ) : Soil temperature [K ] ! (7 ) vwc_dry (REAL*8 ) : Dry volumetric water content (no E-T) [m3/m3] ! (8 ) vwc_opt (REAL*8 ) : E-T optimal volumetric water content [m3/m3] ! (9 ) vwc_sat (REAL*8 ) : Saturated volumetric water content [m3/m3] ! (10) vwc_sfc (REAL*8 ) : Volumetric water content [m3/m3] ! ! Arguments as Output: ! ============================================================================ ! (1 ) CND_TRM_SOI (REAL*8 ) : Soil thermal conductivity [W/m/K] ! (2 ) FLG_MBL (LOGICAL) : Mobilization candidate flag [flag ] ! ! NOTES: !****************************************************************************** ! # include "CMN_SIZE" ! IIPAR ! Arguments LOGICAL, INTENT(IN) :: FLG_MBL(IIPAR) REAL*8, INTENT(IN) :: MSS_FRC_CLY(IIPAR) REAL*8, INTENT(IN) :: MSS_FRC_SND(IIPAR) REAL*8, INTENT(IN) :: TPT_SOI(IIPAR) REAL*8, INTENT(IN) :: VWC_DRY(IIPAR) REAL*8, INTENT(IN) :: VWC_OPT(IIPAR) REAL*8, INTENT(IN) :: VWC_SAT(IIPAR) REAL*8, INTENT(IN) :: VWC_SFC(IIPAR) REAL*8, INTENT(OUT) :: CND_TRM_SOI(IIPAR) REAL*8, INTENT(OUT) :: LVL_DLT(IIPAR) !------------ ! Parameters !------------ ! Thermal conductivity of ice water [W m-1 K-1] REAL*8, PARAMETER :: CND_TRM_H2O_ICE = 2.2d0 ! Thermal conductivity of liquid water [W m-1 K-1] REAL*8, PARAMETER :: CND_TRM_H2O_LQD = 0.6d0 ! Thermal conductivity of snow Bon96 p. 77 [W m-1 K-1] REAL*8, PARAMETER :: CND_TRM_SNW = 0.34d0 ! Soil layer thickness, top layer! [m] REAL*8, PARAMETER :: LVL_DLT_SFC = 0.1d0 ! Temperature range of mixed phase soil [K] REAL*8, PARAMETER :: TPT_DLT = 0.5d0 ! Latent heat of fusion of H2O at 0 C, standard [J kg-1] REAL*8, PARAMETER :: LTN_HEAT_FSN_H2O_STD = 0.3336d06 ! Liquid water density [kg/m3] REAL*8, PARAMETER :: DNS_H2O_LQD_STD = 1000.0d0 ! Kelvin--Celsius scale offset Bol80 [K] REAL*8, PARAMETER :: TPT_FRZ_PNT = 273.15d0 !----------------- ! Local variables !----------------- ! Longitude index INTEGER :: LON_IDX ! Thermal conductivity of dry soil [W m-1 K-1] REAL*8 :: CND_TRM_SOI_DRY(IIPAR) ! Soil thermal conductivity, frozen [W m-1 K-1] REAL*8 :: CND_TRM_SOI_FRZ(IIPAR) ! Thermal conductivity of soil solids [W m-1 K-1] REAL*8 :: CND_TRM_SOI_SLD(IIPAR) ! Soil thermal conductivity, unfrozen [W m-1 K-1] REAL*8 :: CND_TRM_SOI_WRM(IIPAR) ! Volumetric latent heat of fusion [J m-3] REAL*8 :: LTN_HEAT_FSN_VLM(IIPAR) ! Bounded geometric bulk thickness of snow [m] REAL*8 :: SNW_HGT_BND !================================================================= ! CND_TRM_SOI_GET begins here! !================================================================= ! [m] Soil layer thickness LVL_DLT(:) = LVL_DLT_SFC ! [W m-1 K-1] Soil thermal conductivity CND_TRM_SOI(:) = 0.0D0 ! Loop over longitude DO LON_IDX = 1, IIPAR IF ( FLG_MBL(LON_IDX) ) THEN ! Volumetric latent heat of fusion [J m-3] LTN_HEAT_FSN_VLM(LON_IDX) = VWC_SFC(LON_IDX) & * LTN_HEAT_FSN_H2O_STD * DNS_H2O_LQD_STD !Thermal conductivity of soil solids Bon96 p. 77 [W/m/K] CND_TRM_SOI_SLD(LON_IDX) = & ( 8.80D0 *MSS_FRC_SND(LON_IDX) & + 2.92D0 *MSS_FRC_CLY(LON_IDX) ) & / (MSS_FRC_SND(LON_IDX) & + MSS_FRC_CLY(LON_IDX)) ! Thermal conductivity of dry soil Bon96 p. 77 [W/m/K] cnd_trm_soi_dry(lon_idx) = 0.15D0 ! Soil thermal conductivity, unfrozen [W/m/K] CND_TRM_SOI_WRM(LON_IDX) = & CND_TRM_SOI_DRY(LON_IDX) & + ( CND_TRM_SOI_SLD(LON_IDX) & ** (1.0D0-VWC_SAT(LON_IDX)) & * (CND_TRM_H2O_LQD ** VWC_SFC(LON_IDX) ) & - CND_TRM_SOI_DRY(LON_IDX) ) & * VWC_SFC(LON_IDX) / VWC_SAT(lon_idx) ! Soil thermal conductivity, frozen [W/m/K] CND_TRM_SOI_FRZ(LON_IDX) = & CND_TRM_SOI_DRY(LON_IDX) & + ( CND_TRM_SOI_SLD(LON_IDX) & ** (1.0D0-VWC_SAT(LON_IDX)) & * (CND_TRM_H2O_ICE ** VWC_SFC(LON_IDX) ) & - CND_TRM_SOI_DRY(LON_IDX) ) & * VWC_SFC(LON_IDX) / VWC_SAT(LON_IDX) IF (TPT_SOI(LON_IDX) < TPT_FRZ_PNT-TPT_DLT) THEN ! Soil thermal conductivity [W/m/K] CND_TRM_SOI(LON_IDX) = CND_TRM_SOI_FRZ(LON_IDX) ENDIF IF ( (TPT_SOI(LON_IDX) >= TPT_FRZ_PNT-TPT_DLT) & .AND. (TPT_SOI(LON_IDX) <= TPT_FRZ_PNT+TPT_DLT) ) & THEN ! Soil thermal conductivity [W/m/K] CND_TRM_SOI(LON_IDX) = & CND_TRM_SOI_FRZ(LON_IDX) & + (CND_TRM_SOI_FRZ(LON_IDX) & - CND_TRM_SOI_WRM(LON_IDX) ) & * (TPT_SOI(LON_IDX) & -TPT_FRZ_PNT+TPT_DLT) & / (2.0D0*TPT_DLT) ENDIF IF (TPT_SOI(LON_IDX) > TPT_FRZ_PNT+TPT_DLT) THEN ! Soil thermal conductivity[W/m/K] CND_TRM_SOI(LON_IDX)=CND_TRM_SOI_WRM(LON_IDX) ENDIF ! Implement this later(??) !cZ Blend snow into first soil layer !cZ Snow is not allowed to cover dust mobilization regions !cZ snw_hgt_bnd=min(snw_hgt(lon_idx),1.0D0) ! [m] Bounded geometric bulk thickness of snow !cZ lvl_dlt_snw(lon_idx)=lvl_dlt(lon_idx)+snw_hgt_bnd ! O [m] Soil layer thickness !cZ including snow Bon96 p. 77 ! !cZ cnd_trm_soi(lon_idx)= & ! [W m-1 K-1] Soil thermal conductivity Bon96 p. 77 !cZ cnd_trm_snw*cnd_trm_soi(lon_idx)*lvl_dlt_snw(lon_idx) & !cZ /(cnd_trm_snw*lvl_dlt(lon_idx)+cnd_trm_soi(lon_idx)*snw_hgt_bnd) ENDIF ENDDO END SUBROUTINE CND_TRM_SOI_GET !------------------------------------------------------------------------------ SUBROUTINE TRN_FSH_VPR_SOI_ATM_GET( FLG_MBL, & TPT_SOI, & TPT_SOI_FRZ, & TRN_FSH_VPR_SOI_ATM, & VWC_DRY, & VWC_OPT, & VWC_SFC ) ! !****************************************************************************** ! Subroutine TRN_FSH_VPR_SOI_ATM_GET computes the factor describing effects ! of soil texture and moisture on vapor transfer between soil and atmosphere. ! Taken from Bon96 p. 59, CCM:lsm/surphys. (tdf, bmy, 3/30/04) ! ! The TRN_FSH_VPR_SOI_ATM efficiency factor attempts to tie soil texture and ! moisture properties to the vapor conductance of the soil-atmosphere system. ! When the soil temperature is sub-freezing, the conductance describes the ! resistance to vapor sublimation (or deposition) and transport through the ! open soil pores to the atmosphere. ! ! For warm soils, vapor transfer is most efficient at the optimal VWC for E-T ! Thus when vwc_sfc = vwc_opt, soil vapor transfer is perfectly efficient ! (trn_fsh_vpr_soi_atm = 1.0) so the soil does not contribute any resistance ! to the surface vapor transfer. ! ! When vwc_sfc > vwc_opt, the soil has an excess of moisture and, again, ! vapor transfer is not limited by soil characteristics. ! In fact, according to Bon96 p. 98, vwc_dry is only slightly smaller than ! vwc_opt, so trn_fsh_vpr_soi_atm is usually either 0 or 1 and intermediate ! efficiencies occur over only a relatively small range of VWC. ! ! When vwc_sfc < vwc_dry, the soil matrix is subsaturated and acts as a ! one-way sink for vapor through osmotic and capillary potentials. ! In this case trn_fsh_vpr_soi_atm = 0, which would cause the surface ! resistance rss_vpr_sfc to blow up, but this is guarded against and ! rss_sfc_vpr is set to ~1.0e6*rss_aer_vpr instead. ! ! Note that this formulation does not seem to allow vapor transfer from ! the atmosphere to the soil when vwc_sfc < vwc_dry, even when ! e_atm > esat(Tg). ! ! Air at the apparent sink for moisture is has vapor pressure e_sfc ! e_atm = Vapor pressure of ambient air at z = hgt_mdp ! e_sfc = Vapor pressure at apparent sink for moisture at z = zpd + rgh_vpr ! e_gnd = Vapor pressure at air/ground interface temperature ! Air at the soil interface is assumed saturated, i.e., e_gnd = esat(Tg) ! ! Arguments as Input: ! ============================================================================ ! (1 ) FLG_MBL (LOGICAL) : Mobilization candidate flag [unitless] ! (2 ) TPT_SOI (REAL*8 ) : Soil temperature [K ] ! (3 ) TPT_SOI_FRZ (REAL*8 ) : Temperature of frozen soil [K ] ! (5 ) VWC_DRY (REAL*8 ) : Dry volumetric WC (no E-T) [m3/m3 ] ! (6 ) VWC_OPT (REAL*8 ) : E-T optimal volumetric WC [m3/m3 ] ! (7 ) VWC_SFC (REAL*8 ) : Volumetric water content [m3/m3 ] ! ! Arguments as Output: ! ============================================================================ ! (4 ) TRN_FSH_VPR_SOI_ATM (REAL*8 ) : Transfer efficiency of vapor from ! soil to atmosphere [fraction] ! ! NOTES: ! (1 ) Updated comments, cosmetic changes. Also force double-precision ! with "D" exponents. (tdf, bmy, 3/30/04) !****************************************************************************** ! # include "CMN_SIZE" ! IIPAR !---------------- ! Arguments !---------------- LOGICAL, INTENT(IN) :: FLG_MBL(IIPAR) REAL*8, INTENT(IN) :: TPT_SOI(IIPAR) REAL*8, INTENT(IN) :: TPT_SOI_FRZ REAL*8, INTENT(IN) :: VWC_DRY(IIPAR) REAL*8, INTENT(IN) :: VWC_OPT(IIPAR) REAL*8, INTENT(IN) :: VWC_SFC(IIPAR) REAL*8, INTENT(OUT) :: TRN_FSH_VPR_SOI_ATM(IIPAR) !---------------- ! Parameters !---------------- ! Transfer efficiency of vapor from frozen soil to ! atmosphere CCM:lsm/surphy() [fraction] REAL*8, PARAMETER :: TRN_FSH_VPR_SOI_ATM_FRZ = 0.01D0 !----------------- ! Local variables !----------------- INTEGER :: LON_IDX !================================================================= ! TRN_FSH_VPR_SOI_ATM_GET !================================================================= TRN_FSH_VPR_SOI_ATM(:) = 0.0D0 ! Loop over longitudes DO LON_IDX = 1, IIPAR ! If this is a mobilization candidate ... IF ( FLG_MBL(LON_IDX) ) THEN ! ... and if the soil is above freezing ... IF ( TPT_SOI(LON_IDX) > TPT_SOI_FRZ ) THEN ! Transfer efficiency of cvapor from soil to atmosphere [frac] ! CCM:lsm/surphys Bon96 p. 59 TRN_FSH_VPR_SOI_ATM(LON_IDX) = & MIN ( MAX(VWC_SFC(LON_IDX)-VWC_DRY(LON_IDX), 0.0D0) & /(VWC_OPT(LON_IDX)-VWC_DRY(LON_IDX)), 1.0D0) ELSE ! [frc] Bon96 p. 59 TRN_FSH_VPR_SOI_ATM(LON_IDX) = TRN_FSH_VPR_SOI_ATM_FRZ ENDIF ENDIF ENDDO ! Return to calling program END SUBROUTINE TRN_FSH_VPR_SOI_ATM_GET !------------------------------------------------------------------------------ SUBROUTINE BLM_MBL( FLG_MBL, RGH_MMN, WND_10M, MNO_LNG, WND_FRC ) 1,4 ! !****************************************************************************** ! Subroutine BLM_MBL computes the boundary-layer exchange properties, given ! the meteorology at the GEOS-CHEM layer midpoint. This routine is optimized ! for dust source regions: dry, bare, uncovered land. Theory and algorithms: ! Bonan (1996) CCM:lsm/surtem(). Stripped down version, based on adiabatic ! approximation to U*. (tdf, bmy, 3/30/04) ! ! Arguments as Input: ! ============================================================================ ! (1 ) FLG_MBL (LOGICAL) : Mobilization candidate flag [unitless] ! (2 ) RGH_MMN (REAL*8 ) : Roughness length momentum [m ] ! (3 ) WND_10M (REAL*8 ) : 10 m wind speed [m/s ] ! ! Arguments as Output: ! ============================================================================ ! (4 ) MNO_LNG (REAL*8 ) : Monin-Obukhov length [m ] ! (5 ) WND_FRC (REAL*8 ) : Surface friction velocity [m/s ] ! ! NOTES: ! (1 ) Updated comments, cosmetic changes. Also force double-precision with ! "D" exponents. (tdf, bmy, 3/30/04) !****************************************************************************** ! ! References to F90 modules USE DAO_MOD, ONLY : USTAR USE ERROR_MOD, ONLY : ERROR_STOP # include "CMN_SIZE" ! Size parameters !----------------- ! Arguments !----------------- LOGICAL, INTENT(IN) :: FLG_MBL(IIPAR) REAL*8, INTENT(IN) :: RGH_MMN(IIPAR) REAL*8, INTENT(IN) :: WND_10M(IIPAR) REAL*8, INTENT(OUT) :: MNO_LNG(IIPAR) REAL*8, INTENT(OUT) :: WND_FRC(IIPAR) !----------------- ! Parameters !----------------- ! Prevents division by zero [unitless] REAL*8, PARAMETER :: EPS_DBZ = 1.0d-6 ! Minimum windspeed used for mobilization [m/s] REAL*8, PARAMETER :: WND_MIN_MBL = 1.0d0 ! Roughness length momentum for erodible surfaces [m] ! MaB95 p. 16420, GMB98 p. 6205 REAL*8, PARAMETER :: RGH_MMN_MBL = 100.0d-6 ! Reference height for mobilization processes [m] REAL*8, PARAMETER :: HGT_RFR = 10.0d0 !----------------- ! Local variables !----------------- ! Counting index for lon INTEGER :: LON_IDX ! Denominator of Monin-Obukhov length Bon96 p. 49 REAL*8 :: MNO_DNM ! Surface layer mean wind speed [m/s] REAL*8 :: WND_MDP_BND(IIPAR) ! denominator for wind friction velocity REAL*8 :: WND_FRC_DENOM !================================================================= ! BLM_MBL begins here! !================================================================= ! Initialize MNO_LNG(:) = 0.0D0 WND_FRC(:) = 0.0D0 ! Loop over longitudes DO LON_IDX = 1, IIPAR ! Surface layer mean wind speed bounded [m/s] WND_MDP_BND(LON_IDX) = & MAX(WND_10M(LON_IDX), WND_MIN_MBL) ! Friction velocity (adiabatic approximation S&P equ. 16.57, ! tdf 10/27/2K3 -- Sanity check IF ( RGH_MMN(LON_IDX) <= 0.0 ) THEN CALL ERROR_STOP( 'RGH_MMN <= 0.0', & 'BLM_MBL ("dust_dead_mod.f")' ) ENDIF ! Distinguish between mobilisation candidates and noncandidates IF ( FLG_MBL(LON_IDX) ) THEN WND_FRC_DENOM = HGT_RFR / RGH_MMN_MBL ! z = 10 m ELSE WND_FRC_DENOM = HGT_RFR / RGH_MMN(LON_IDX) ! z = 10 m ENDIF ! Sanity check IF ( WND_FRC_DENOM <= 0.0 ) THEN CALL ERROR_STOP( 'wnd_frc_denom <= 0.0', & 'BLM_MBL ("dust_dead_mod.f")' ) ENDIF ! Take natural LOG of WND_FRC_DENOM WND_FRC_DENOM = LOG(WND_FRC_DENOM) ! Convert to [m/s] WND_FRC(LON_IDX) = WND_MDP_BND(LON_IDX) * CST_VON_KRM & / WND_FRC_DENOM ! Denominator of Monin-Obukhov length Bon96 p. 49 ! Set denominator of Monin-Obukhov length to minimum value MNO_DNM = EPS_DBZ ! Monin-Obukhov length Bon96 p. 49 [m] MNO_LNG(LON_IDX) = -1.0D0 * (WND_FRC(LON_IDX)**3.0D0) & /MNO_DNM ! Override for non mobilisation candidates IF ( .NOT. FLG_MBL(LON_IDX) ) THEN WND_FRC(LON_IDX) = 0.0D0 ENDIF ENDDO ! Return to calling program END SUBROUTINE BLM_MBL !------------------------------------------------------------------------------ LOGICAL FUNCTION ORO_IS_OCN( ORO_VAL ) 1 ! !****************************************************************************** ! Function ORO_IS_OCN returns TRUE if a grid box contains more than 50% ! ocean. (tdf, bmy, 3/30/04) ! ! Arguments as Input: ! ============================================================================ ! (1 ) ORO_VAL (REAL*8) : Orography at a grid box (0=ocean; 1=land; 2=ice) ! ! NOTES: !****************************************************************************** ! ! Arguments REAL*8, INTENT(IN) :: ORO_VAL !================================================================= ! ORO_IS_OCN begins here! !================================================================= ORO_IS_OCN = ( NINT( ORO_VAL ) == 0 ) ! Return to calling program END FUNCTION ORO_IS_OCN !------------------------------------------------------------------------------ LOGICAL FUNCTION ORO_IS_LND( ORO_VAL ) 2 ! !****************************************************************************** ! Function ORO_IS_LND returns TRUE if a grid box contains more than 50% ! land. (tdf, bmy, 3/30/04, 3/1/05) ! ! Arguments as Input: ! ============================================================================ ! (1 ) ORO_VAL (REAL*8) : Orography at a grid box (0=ocean; 1=land; 2=ice) ! ! NOTES: ! (1 ) Bug fix: Replaced ": :" with "::" in order to prevent compile error ! on Linux w/ PGI compiler. (bmy, 3/1/05) !****************************************************************************** ! ! Arguments REAL*8, INTENT(IN) :: ORO_VAL !================================================================= ! ORO_IS_OCN begins here! !================================================================= ORO_IS_LND = ( NINT( ORO_VAL ) == 1 ) ! Return to calling program END FUNCTION ORO_IS_LND !------------------------------------------------------------------------------ LOGICAL FUNCTION ORO_IS_ICE( ORO_VAL ) 1 ! !****************************************************************************** ! Function ORO_IS_LND returns TRUE if a grid box contains more than 50% ! ice. (tdf, bmy, 3/30/04) ! ! Arguments as Input: ! ============================================================================ ! (1 ) ORO_VAL (REAL*8) : Orography at a grid box (0=ocean; 1=land; 2=ice) ! ! NOTES: !****************************************************************************** ! ! Arguments REAL*8, INTENT(IN) :: ORO_VAL !================================================================= ! ORO_IS_ICE begins here! !================================================================= ORO_IS_ICE = ( NINT( ORO_VAL ) == 2 ) ! Return to calling program END FUNCTION ORO_IS_ICE !------------------------------------------------------------------------------ REAL*8 FUNCTION MNO_STB_CRC_HEAT_UNS_GET( SML_FNC_MMN_UNS_RCP ) ! !****************************************************************************** ! Function MNO_STB_CRC_HEAT_UNS_GET returns the stability correction factor ! for heat (usually called PSI), given the reciprocal of the Monin-Obukhov ! similarity function (usually called PHI) for momentum in an unstable ! atmosphere. (tdf, bmy, 3/30/04) ! ! Arguments as Input: ! ============================================================================ ! (1 ) sml_fnc_mmn_uns_rcp (REAL*8) : 1/(M-O similarity function) [fraction] ! ! References: ! ============================================================================ ! References are Ary88 p. 167, Bru82 p. 71, SeP97 p. 869, ! Bon96 p. 52, BKL97 p. F1, LaP81 p. 325, LaP82 p. 466 ! Currently this function is BFB with CCM:dom/flxoce() ! ! NOTES: ! (1 ) Updated comments, cosmetic changes (bmy, 3/30/04) !****************************************************************************** ! ! Arguments REAL*8, INTENT(IN) :: SML_FNC_MMN_UNS_RCP !================================================================= ! MNO_STB_CRC_HEAT_UNS_GET !================================================================= MNO_STB_CRC_HEAT_UNS_GET = 2.0D0 * & LOG( ( 1.0D0+SML_FNC_MMN_UNS_RCP * SML_FNC_MMN_UNS_RCP) / 2.0D0 ) ! Return to calling program END FUNCTION MNO_STB_CRC_HEAT_UNS_GET !------------------------------------------------------------------------------ REAL*8 FUNCTION MNO_STB_CRC_MMN_UNS_GET( SML_FNC_MMN_UNS_RCP ) ! !****************************************************************************** ! Function MNO_STB_CRC_MMN_UNS_GET returns the stability correction factor ! for momentum (usually called PSI), given the reciprocal of the ! Monin-Obukhov similarity function (usually called PHI), for momentum in ! an unstable atmosphere. (tdf, bmy, 3/30/04) ! ! Arguments as Input: ! ============================================================================ ! (1 ) SML_FNC_MMN_UNS_RCP (REAL*8) : 1/(M-O similarity function) [fraction] ! ! References: ! ============================================================================ ! References are Ary88 p. 167, Bru82 p. 71, SeP97 p. 869, ! Bon96 p. 52, BKL97 p. F1, LaP81 p. 325, LaP82 p. 466 ! Currently this function is BFB with CCM:dom/flxoce() ! ! NOTES: ! (1 ) Updated comments, cosmetic changes (bmy, 3/30/04) !****************************************************************************** ! ! Arguments REAL*8, INTENT(IN) :: SML_FNC_MMN_UNS_RCP !================================================================= ! MNO_STB_CRC_MMN_UNS_GET begins here! !================================================================= MNO_STB_CRC_MMN_UNS_GET = & LOG((1.0D0+SML_FNC_MMN_UNS_RCP*(2.0D0+SML_FNC_MMN_UNS_RCP)) & *(1.0D0+SML_FNC_MMN_UNS_RCP*SML_FNC_MMN_UNS_RCP)/8.0D0) & -2.0D0*ATAN(SML_FNC_MMN_UNS_RCP)+1.571D0 ! Return to calling program END FUNCTION MNO_STB_CRC_MMN_UNS_GET !------------------------------------------------------------------------------ REAL*8 FUNCTION XCH_CFF_MMN_OCN_NTR_GET( WND_10M_NTR ) 1 ! !****************************************************************************** ! Function XCH_CFF_MMN_OCN_NTR_GET returns the Neutral 10m drag coefficient ! over oceans. (tdf, bmy, 3/30/04) ! ! Arguments as Input: ! ============================================================================ ! (1 ) WIND_10M_NTR (REAL*8) : Wind speed @ 10 m[m/s] ! ! References: ! ============================================================================ ! LaP82 CCM:dom/flxoce(), NOS97 p. I2 ! ! NOTES: ! (1 ) Updated comments, cosmetic changes (bmy, 3/30/04) !****************************************************************************** ! ! Arguments REAL*8, INTENT(IN) :: WND_10M_NTR !================================================================= ! XCH_CFF_MMN_OCN_NTR_GET begins here! !================================================================= XCH_CFF_MMN_OCN_NTR_GET = 0.0027D0 / WND_10M_NTR + 0.000142D0 & + 0.0000764D0 * WND_10M_NTR ! REturn to calling program END FUNCTION XCH_CFF_MMN_OCN_NTR_GET !------------------------------------------------------------------------------ SUBROUTINE RGH_MMN_GET( ORO, RGH_MMN, SFC_TYP, SNW_FRC, WND_10M ) 1,6 ! !****************************************************************************** ! Subroutine RGH_MMN_GET sets the roughness length. (tdf, bmy, 3/30/04) ! ! Arguments as Input: ! ============================================================================ ! (1 ) ORO (INTEGER) : Orography (0=ocean; 1=land; 2=ice) [unitless] ! (3 ) SFC_TYP (REAL*8 ) : LSM surface type (0..28) [unitless] ! (4 ) SNW_FRC (REAL*8 ) : Fraction of surface covered by snow [fraction] ! (5 ) WND_10M (REAL*8 ) : 10 m wind speed [m/s ] ! ! Arguments as Output: ! ============================================================================ ! (2 ) RGH_MMN (REAL*8 ) : Roughness length momentu [m ] ! ! NOTES: ! (1 ) Updated comments, cosmetic changes. Also now force double-precision ! with "D" exponents (bmy, 3/30/04) !****************************************************************************** ! ! References to F90 modules USE ERROR_MOD, ONLY : ERROR_STOP # include "CMN_SIZE" ! Size parameters !----------------- ! Arguments !----------------- INTEGER, INTENT(IN) :: SFC_TYP(IIPAR) REAL*8, INTENT(IN) :: ORO(IIPAR) REAL*8, INTENT(IN) :: SNW_FRC(IIPAR) REAL*8, INTENT(IN) :: WND_10M(IIPAR) REAL*8, INTENT(OUT) :: RGH_MMN(IIPAR) !----------------- ! Parameters !----------------- ! Roughness length over frozen lakes Bon96 p. 59 [m] REAL*8, PARAMETER :: RGH_MMN_ICE_LAK = 0.04d0 ! Roughness length over ice, bare ground, wetlands Bon96 p. 59 [m] REAL*8, PARAMETER :: RGH_MMN_ICE_LND = 0.05d0 ! Roughness length over sea ice BKL97 p. F-3 [m] REAL*8, PARAMETER :: RGH_MMN_ICE_OCN = 0.0005d0 ! Roughness length over unfrozen lakes Bon96 p. 59 [m] REAL*8, PARAMETER :: RGH_MMN_LAK_WRM = 0.001d0 ! Roughness length over snow Bon96 p. 59 CCM:lsm/snoconi.F ! [m] REAL*8, PARAMETER :: RGH_MMN_SNW = 0.04d0 ! Minimum windspeed for momentum exchange REAL*8, PARAMETER :: WND_MIN_DPS = 1.0d0 !----------------- ! Local variables !----------------- ! [idx] Longitude index array (sea ice) INTEGER :: ICE_IDX(IIPAR) ! [nbr] Number of sea ice points INTEGER :: ICE_NBR ! [Idx] Counting index INTEGER :: IDX_IDX ! [idx] Longitude index array (land) INTEGER :: LND_IDX(IIPAR) ! [nbr] Number of land points INTEGER :: LND_NBR ! [idx] Counting index INTEGER :: LON_IDX ! [idx] Longitude index array (ocean) INTEGER :: OCN_IDX(IIPAR) ! [nbr] Number of ocean points INTEGER :: OCN_NBR ! [idx] Plant type index INTEGER :: PLN_TYP_IDX ! [idx] Surface type index INTEGER :: SFC_TYP_IDX ! [idx] Surface sub-gridscale index INTEGER :: SGS_IDX ! [m] Roughness length of current sub-gridscale REAL*8 :: RLM_CRR ! [m s-1] Bounded wind speed at 10 m REAL*8 :: WND_10M_BND ! [frc] Neutral 10 m drag coefficient over ocean REAL*8 :: XCH_CFF_MMN_OCN_NTR ! Momentum roughness length [m] REAL*8 :: Z0MVT(MVT) = (/ 0.94d0, 0.77d0, 2.62d0, 1.10d0, 0.99d0, & 0.06d0, 0.06d0, 0.06d0, 0.06d0, 0.06d0, & 0.06d0, 0.06d0, 0.06d0, 0.00d0 /) ! Displacement height (fn of plant type) REAL*8 :: ZPDVT(MVT) = (/ 11.39d0, 9.38d0, 23.45d0, 13.40d0, & 12.06d0, 0.34d0, 0.34d0, 0.34d0, & 0.34d0, 0.34d0, 0.34d0, 0.34d0, & 0.34d0, 0.00d0 /) !================================================================= ! RGH_MMN_SET begins here !================================================================= RGH_MMN(:) = 0.0D0 ! Count ocean grid boxes OCN_NBR = 0 DO LON_IDX = 1, IIPAR IF ( ORO_IS_OCN( ORO(LON_IDX) ) ) THEN OCN_NBR = OCN_NBR + 1 OCN_IDX(OCN_NBR) = LON_IDX ENDIF ENDDO ! Count ice grid boxes ICE_NBR = 0 DO LON_IDX = 1, IIPAR IF ( ORO_IS_ICE( ORO(LON_IDX) ) ) THEN ICE_NBR = ICE_NBR+1 ICE_IDX(ICE_NBR) = LON_IDX ENDIF ENDDO ! Count land grid boxes LND_NBR = 0 DO LON_IDX = 1, IIPAR IF ( ORO_IS_LND( ORO(LON_IDX) ) ) THEN LND_NBR = LND_NBR + 1 LND_IDX(LND_NBR) = LON_IDX ENDIF ENDDO !================================================================= ! Ocean points !================================================================= DO IDX_IDX = 1, OCN_NBR ! Longitude index of the ocean point LON_IDX = OCN_IDX(IDX_IDX) ! Convert wind speed to roughness length over ocean [m/s] WND_10M_BND = MAX( WND_MIN_DPS, WND_10M(LON_IDX) ) !Approximation: neutral 10 m wind speed unavailable, ! use 10 m wind speed [fraction] XCH_CFF_MMN_OCN_NTR = XCH_CFF_MMN_OCN_NTR_GET(WND_10M_BND) ! BKL97 p. F-4, LaP81 p. 327 (14) Ocean Points [m] RGH_MMN(LON_IDX)=10.0D0 & * EXP(-CST_VON_KRM / SQRT(XCH_CFF_MMN_OCN_NTR)) ENDDO !================================================================= ! Sea ice points !================================================================= DO IDX_IDX = 1, ICE_NBR LON_IDX = ICE_IDX(IDX_IDX) RGH_MMN(LON_IDX) = SNW_FRC(LON_IDX) * RGH_MMN_SNW & +(1.0D0-SNW_FRC(LON_IDX)) * RGH_MMN_ICE_OCN ! [m] Bon96 p. 59 ENDDO !================================================================= ! Land points !================================================================= DO IDX_IDX = 1, LND_NBR ! Longitude LON_IDX = LND_IDX(IDX_IDX) ! Store surface blend for current gridpoint, sfc_typ(lon_idx) SFC_TYP_IDX = SFC_TYP(LON_IDX) ! Inland lakes IF ( SFC_TYP_IDX == 0 ) THEN !fxm: Add temperature input and so ability to discriminate warm ! from frozen lakes here [m] Bon96 p. 59 RGH_MMN(LON_IDX) = RGH_MMN_LAK_WRM ! Land ice ELSE IF ( SFC_TYP_IDX == 1 ) THEN ! [m] Bon96 p. 59 RGH_MMN(LON_IDX) = SNW_FRC(LON_IDX)*RGH_MMN_SNW & + (1.0D0-SNW_FRC(LON_IDX))*RGH_MMN_ICE_LND ! Normal land ELSE DO SGS_IDX = 1, 3 ! Bare ground is pln_typ=14, ocean is pln_typ=0 PLN_TYP_IDX = PLN_TYP(SFC_TYP_IDX,SGS_IDX) ! Bare ground IF ( PLN_TYP_IDX == 14 ) THEN ! Bon96 p. 59 (glacial ice is same as bare ground) RLM_CRR = SNW_FRC(LON_IDX) * RGH_MMN_SNW & + (1.0D0-SNW_FRC(LON_IDX)) * RGH_MMN_ICE_LND ! [m] ! Regular plant type ELSE IF ( PLN_TYP_IDX > 0 ) THEN RLM_CRR = SNW_FRC(LON_IDX) * RGH_MMN_SNW & + (1.0D0-SNW_FRC(LON_IDX)) * Z0MVT(PLN_TYP_IDX) ! [m] Bon96 p. 59 ! Presumably ocean snuck through ELSE CALL ERROR_STOP( 'pln_typ_idx == 0', & 'RGH_MMN_GET ("dead_dust_mod.f")' ) ENDIF ! endif ! Roughness length for normal land RGH_MMN(LON_IDX) = RGH_MMN(LON_IDX) ! [m] & + PLN_FRC(SFC_TYP_IDX,SGS_IDX) ! [frc] & * RLM_CRR ! [m] ENDDO ENDIF ENDDO ! Return to calling program END SUBROUTINE RGH_MMN_GET !------------------------------------------------------------------------------ SUBROUTINE SNW_FRC_GET( SNW_HGT_LQD, SNW_FRC ) 1 ! !****************************************************************************** ! Subroutine SNW_FRC_GET converts equivalent liquid water snow depth to ! fractional snow cover. Uses the snow thickness -> fraction algorithm of ! Bon96. (tdf bmy, 3/30/04) ! ! Arguments as Input: ! =========================================================================== ! (1 ) snw_hgt_lqd (REAL*8) : Equivalent liquid water snow depth [m] ! ! Arguments as Output: ! =========================================================================== ! (2 ) snw_frc (REAL*8 ) : Fraction of surface covered by snow ! ! NOTES: ! (1 ) Updated comments, cosmetic changes. Also now force double-precision ! with "D" exponents. (bmy, 3/30/04) !****************************************************************************** ! # include "CMN_SIZE" !---------------- ! Arguments !---------------- REAL*8, INTENT(IN) :: SNW_HGT_LQD(IIPAR) REAL*8, INTENT(OUT) :: SNW_FRC(IIPAR) !---------------- ! Parameters !---------------- ! Note disparity in bulk snow density between CCM and LSM ! WiW80 p. 2724, 2725 has some discussion of bulk snow density ! ! Bulk density of snow [kg m-3] REAL*8, PARAMETER :: DNS_H2O_SNW_GND_LSM = 250.0D0 ! Standard bulk density of snow on ground [kg m-3] REAL*8, PARAMETER :: DNS_H2O_SNW_GND_STD = 100.0D0 ! Geometric snow thickness for 100% coverage ! [m] REAL*8, PARAMETER :: SNW_HGT_THR = 0.05D0 ! Liquid water density! [kg/m3] REAL*8, PARAMETER :: DNS_H2O_LQD_STD = 1000.0D0 !----------------- ! Local variables !----------------- ! [idx] Counting index for lon INTEGER :: LON_IDX ! [m] Geometric bulk thickness of snow REAL*8 :: SNW_HGT(IIPAR) ! Conversion factor from liquid water depth ! to geometric snow thickness [fraction] REAL*8 :: HGT_LQD_SNW_CNV !================================================================= ! SNW_FRC_GET begins here! !================================================================= ! Conversion factor from liquid water depth to ! geometric snow thickness [fraction] HGT_LQD_SNW_CNV = DNS_H2O_LQD_STD & / DNS_H2O_SNW_GND_STD ! Fractional snow cover DO LON_IDX = 1, IIPAR ! Snow height [m] SNW_HGT(LON_IDX) = SNW_HGT_LQD(LON_IDX) & * HGT_LQD_SNW_CNV ! Snow fraction ! NB: CCM and LSM seem to disagree on this SNW_FRC(LON_IDX) = MIN(SNW_HGT(LON_IDX)/SNW_HGT_THR, 1.0D0) ENDDO ! Return to calling program END SUBROUTINE SNW_FRC_GET !------------------------------------------------------------------------------ SUBROUTINE WND_RFR_GET( FLG_ORO, HGT_MDP, HGT_RFR, HGT_ZPD, & MNO_LNG, WND_FRC, WND_MDP, WND_MIN, & WND_RFR ) ! !****************************************************************************** ! Subroutine WND_RFR_GET interpolates wind speed at given height to wind ! speed at reference height. (tdf, bmy, 3/30/04) ! ! Arguments as Input: ! =========================================================================== ! (1 ) FLG_ORO (LOGICAL) : Orography flag (mobilization flag) [flag] ! (2 ) HGT_MDP (REAL*8 ) : Midpoint height above surface [m ] ! (3 ) HGT_RFR (REAL*8 ) : Reference height [m ] ! (4 ) HGT_ZPD (REAL*8 ) : Zero plane displacement [m ] ! (5 ) MNO_LNG (REAL*8 ) : Monin-Obukhov length [m ] ! (6 ) WND_FRC (REAL*8 ) : Surface friction velocity [m/s ] ! (7 ) WND_MDP (REAL*8 ) : Surface layer mean wind speed [m/s ] ! (8 ) WND_MIN (REAL*8 ) : Minimum windspeed [m/s ] ! ! Arguments as Output: ! =========================================================================== ! (9 ) WND_RFR (REAL*8 ) : Wind speed at reference height [m/s ] ! ! NOTES: ! (1 ) Updated comments, cosmetic changes. Also now force double-precision ! with "D" exponents. (bmy, 3/30/04) !****************************************************************************** ! # include "CMN_SIZE" ! IIPAR !------------------ ! Arguments !------------------ LOGICAL, INTENT(IN) :: FLG_ORO(IIPAR) REAL*8, INTENT(IN) :: HGT_MDP(IIPAR) REAL*8, INTENT(IN) :: HGT_RFR REAL*8, INTENT(IN) :: HGT_ZPD(IIPAR) REAL*8, INTENT(IN) :: MNO_LNG(IIPAR) REAL*8, INTENT(IN) :: WND_FRC(IIPAR) REAL*8, INTENT(IN) :: WND_MDP(IIPAR) REAL*8, INTENT(IN) :: WND_MIN REAL*8, INTENT(OUT) :: WND_RFR(IIPAR) !------------------ ! Parameters !------------------ ! Named index for lower (target) hght INTEGER, PARAMETER :: RFR_HGT_IDX=1 ! Named index for upper (known) hght INTEGER, PARAMETER :: GCM_HGT_IDX=2 !------------------ ! Local variables !------------------ ! [idx] Counting index INTEGER :: IDX_IDX ! [idx] Counting index for lon INTEGER :: LON_IDX ! Stability computation loop index INTEGER :: LVL_IDX ! Valid indices INTEGER :: VLD_IDX(IIPAR) ! [nbr] Number of valid indices INTEGER :: VLD_NBR ! [frc] Monin-Obukhov stability correction momentum REAL*8 :: MNO_STB_CRC_MMN(IIPAR,2) ! [frc] Monin-Obukhov stability parameter REAL*8 :: MNO_STB_PRM(IIPAR,2) ! [frc] Reciprocal of similarity function ! for momentum, unstable atmosphere REAL*8 :: SML_FNC_MMN_UNS_RCP ! Term in stability correction computation REAL*8 :: TMP2 ! Term in stability correction computation REAL*8 :: TMP3 ! Term in stability correction computation REAL*8 :: TMP4 ! [frc] Wind correction factor REAL*8 :: WND_CRC_FCT(IIPAR) ! [m-1] Reciprocal of reference height REAL*8 :: HGT_RFR_RCP !================================================================= ! WND_RFR_GET begins here! !================================================================= HGT_RFR_RCP = 1.0D0 / HGT_RFR ! [m-1] WND_RFR = WND_MIN ! [m s-1] ! Compute horizontal wind speed at reference height DO LON_IDX = 1, IIPAR IF (FLG_ORO(LON_IDX) .AND. HGT_ZPD(LON_IDX) < HGT_RFR) THEN ! Code uses notation of Bon96 p. 50, where lvl_idx=1 ! is 10 m ref. hgt, lvl_idx=2 is atm. hgt MNO_STB_PRM(LON_IDX,RFR_HGT_IDX) = & MIN((HGT_RFR-HGT_ZPD(LON_IDX)) & /MNO_LNG(LON_IDX),1.0D0) ! [frc] MNO_STB_PRM(LON_IDX,GCM_HGT_IDX) = & MIN((HGT_MDP(LON_IDX)-HGT_ZPD(LON_IDX)) & /MNO_LNG(LON_IDX),1.0D0) ! [frc] DO LVL_IDX = 1, 2 IF (MNO_STB_PRM(LON_IDX,LVL_IDX) < 0.0D0) THEN SML_FNC_MMN_UNS_RCP = (1.0D0 - 16.0D0 & * MNO_STB_PRM(LON_IDX,LVL_IDX))**0.25D0 TMP2 = LOG((1.0D0 + SML_FNC_MMN_UNS_RCP & * SML_FNC_MMN_UNS_RCP)/2.0D0) TMP3 = LOG((1.0D0 + SML_FNC_MMN_UNS_RCP)/2.0D0) MNO_STB_CRC_MMN(LON_IDX,LVL_IDX) = & 2.0D0 * TMP3 + TMP2 - 2.0D0 & * ATAN(SML_FNC_MMN_UNS_RCP) + 1.5707963 ELSE ! not stable MNO_STB_CRC_MMN(LON_IDX,LVL_IDX) = -5.0D0 & * MNO_STB_PRM(LON_IDX,LVL_IDX) ENDIF ! stable ENDDO ! end loop over lvl_idx TMP4 = LOG( (HGT_MDP(LON_IDX)-HGT_ZPD(LON_IDX)) & / (HGT_RFR-HGT_ZPD(LON_IDX)) ) ! Correct neutral stability assumption WND_CRC_FCT(LON_IDX) = TMP4 & - MNO_STB_CRC_MMN(LON_IDX,GCM_HGT_IDX) & + MNO_STB_CRC_MMN(LON_IDX,RFR_HGT_IDX) ! [frc] WND_RFR(LON_IDX) = WND_MDP(LON_IDX)-WND_FRC(LON_IDX) & * CST_VON_KRM_RCP * WND_CRC_FCT(LON_IDX) ! [m s-1] WND_RFR(LON_IDX) = MAX(WND_RFR(LON_IDX),WND_MIN) ! [m s-1] ENDIF ENDDO ! Return to calling program END SUBROUTINE WND_RFR_GET !------------------------------------------------------------------------------ SUBROUTINE WND_FRC_THR_SLT_GET( FLG_MBL, DNS_MDP, WND_FRC_THR_SLT) 1,2 ! !****************************************************************************** ! Subroutine WND_FRC_THR_SLT_GET ccmputes the dry threshold friction velocity ! for saltation -- See Zender et al. expression (1) (tdf, bmy, 3/30/04) ! ! Arguments as Input: ! =========================================================================== ! (1 ) FLG_MBL (LOGICAL) : mobilisation flag ! (2 ) DNS_MDP (REAL*8 ) : Midlayer density [kg/m3] ! ! Arguments as Output: ! =========================================================================== ! (3 ) WND_FRC_THR_SLT (REAL*8 ) : Threshold friction velocity ! for saltation [m/s] ! ! NOTES: ! (1 ) Updated comments, cosmetic changes. Also now force double-precision ! with "D" exponents. (bmy, 3/30/04) !****************************************************************************** ! ! References to F90 modules USE ERROR_MOD, ONLY : ERROR_STOP # include "CMN_SIZE" ! IIPAR !---------------- ! Arguments !---------------- LOGICAL, INTENT(IN) :: FLG_MBL(IIPAR) REAL*8, INTENT(IN) :: DNS_MDP(IIPAR) REAL*8, INTENT(OUT) :: WND_FRC_THR_SLT(IIPAR) !----------------- ! Parameters !----------------- ! [m] Optimal diameter for saltation, ! IvW82 p. 117 Fgr. 8, Pye87 p. 31, MBA97 p. 4388, SRL96 (2) REAL*8, PARAMETER :: DMT_SLT_OPT = 75.0d-6 ! [kg m-3] Density of optimal saltation particles, ! MBA97 p. 4388 friction velocity for saltation REAL*8, PARAMETER :: DNS_SLT = 2650.0d0 !----------------- ! Local variables !----------------- ! [idx] Longitude Counting Index INTEGER :: LON_IDX ! Threshold friction Reynolds number ! approximation for optimal size [frc] REAL*8 :: RYN_NBR ! Density ratio factor for saltation calculation REAL*8 :: DNS_FCT ! Interparticle cohesive forces factor for saltation calculation REAL*8 :: ALPHA, BETA, GAMMA, TMP1 !================================================================= ! WND_FRC_THR_SLT_GET begins here! !================================================================= ! Initialize some variables ! MaB95 pzn. for Re*t(D_opt) circumvents iterative solution ! [frc] "B" MaB95 p. 16417 (5) ! [m/s] Threshold velocity WND_FRC_THR_SLT(:) = 0.0D0 ! Threshold friction Reynolds number approximation for optimal size RYN_NBR = 0.38D0 + 1331.0D0 & * (100.0D0*DMT_SLT_OPT)**1.56D0 ! tdf NB conversion of Dp to [cm] ! Given Re*t(D_opt), compute time independent factors contributing ! to u*t. IvW82 p. 115 (6) MaB95 p. 16417 (4) Interparticle cohesive ! forces. see Zender et al., Equ. (1). ! tdf introduced beta [fraction] BETA = 1.0D0+6.0D-07 / (DNS_SLT*GRV_SFC*(DMT_SLT_OPT**2.5D0)) ! IvW82 p. 115 (6) MaB95 p. 16417 (4) DNS_FCT = DNS_SLT * GRV_SFC * DMT_SLT_OPT ! Error check IF ( RYN_NBR < 0.03D0 ) THEN CALL ERROR_STOP( 'RYN_NBR < 0.03', & 'WND_FRC_THR_SLT_GET ("dust_dead_mod.f")' ) ELSE IF ( RYN_NBR < 10.0D0 ) THEN ! IvW82 p. 114 (3), MaB95 p. 16417 (6) ! tdf introduced gamma [fraction] GAMMA = -1.0D0 + 1.928D0 * (RYN_NBR**0.0922D0) TMP1 = 0.129D0*0.129D0 * BETA / GAMMA ELSE ! ryn_nbr > 10.0D0 ! IvW82 p. 114 (3), MaB95 p. 16417 (7) ! tdf introduced gamma [fraction] GAMMA = 1.0D0-0.0858D0 * EXP(-0.0617D0*(RYN_NBR-10.0D0)) TMP1 = 0.12D0*0.12D0 * BETA * GAMMA * GAMMA ENDIF DO LON_IDX = 1, IIPAR ! Threshold friction velocity for saltation dry ground ! tdf introduced alpha ALPHA = DNS_FCT / DNS_MDP(LON_IDX) ! Added mobilisation constraint IF ( FLG_MBL(LON_IDX) ) THEN WND_FRC_THR_SLT(LON_IDX) = SQRT(TMP1) * SQRT(ALPHA) ! [m s-1] ENDIF ENDDO ! Return to calling program END SUBROUTINE WND_FRC_THR_SLT_GET !------------------------------------------------------------------------------ SUBROUTINE WND_RFR_THR_SLT_GET( WND_FRC, WND_FRC_THR_SLT, & WND_MDP, WND_RFR, & WND_RFR_THR_SLT ) ! !****************************************************************************** ! Subroutine WND_RFR_THR_SLT_GET computes the threshold horizontal wind ! speed at reference height for saltation. (tdf, bmy, 3/30/04) ! ! Arguments as Input: ! ============================================================================ ! (1 ) wnd_frc (REAL*8) : Surface friction velocity [m/s] ! (2 ) wnd_frc_thr_slt (REAL*8) : Threshold friction vel. for saltation [m/s] ! (3 ) wnd_mdp (REAL*8) : Surface layer mean wind speed [m/s] ! (4 ) wnd_rfr (REAL*8) : Wind speed at reference height [m/s] ! ! Arguments as Output: ! ============================================================================ ! (5 ) wnd_rfr_thr_slt (REAL*8) : Threshold 10m wind speed for saltation [m/s] ! ! NOTES: ! (1 ) Updated comments, cosmetic changes. !****************************************************************************** ! # include "CMN_SIZE" ! Size parameters ! Arguments REAL*8, INTENT(IN) :: WND_FRC(IIPAR) REAL*8, INTENT(IN) :: WND_FRC_THR_SLT(IIPAR) REAL*8, INTENT(IN) :: WND_MDP(IIPAR) REAL*8, INTENT(IN) :: WND_RFR(IIPAR) REAL*8, INTENT(OUT) :: WND_RFR_THR_SLT(IIPAR) ! Local variables INTEGER :: I !================================================================= ! WND_RFR_THR_SLT_GET begins here !================================================================= DO I = 1, IIPAR ! A more complicated procedure would recompute mno_lng for ! wnd_frc_thr, and then integrate vertically from rgh_mmn+hgt_zpd ! to hgt_rfr. ! ! wnd_crc_fct is (1/k)*[ln(z-D)/z0 - psi(zeta2) + psi(zeta1)] WND_RFR_THR_SLT(I) = WND_FRC_THR_SLT(I) & * WND_RFR(I) / WND_FRC(I) ENDDO ! Return to calling program END SUBROUTINE WND_RFR_THR_SLT_GET !------------------------------------------------------------------------------ SUBROUTINE VWC2GWC( FLG_MBL, GWC_SFC, VWC_SAT, VWC_SFC ) 1 ! !****************************************************************************** ! Subroutine VWC2GWC converts volumetric water content to gravimetric water ! content -- assigned only for mobilisation candidates. (tdf, bmy, 3/30/04) ! ! Arguments as Input: ! =========================================================================== ! (1 ) FLG_MBL (LOGICAL) : Mobilization candidate flag [flag] ! (3 ) VWC_SAT (REAL*8 ) : Saturated VWC (sand-dependent) [m3/m3] ! (4 ) VWC_SFC (REAL*8 ) : Volumetric water content! [m3/m3 ! ! Arguments as Output: ! =========================================================================== ! (2 ) gwc_sfc (REAL*8 ) : Gravimetric water content [kg/kg] ! ! NOTES: ! (1 ) Updated comments, cosmetic changes. Also now forces double-precision ! with "D" exponents. (tdf, bmy, 3/30/04) !****************************************************************************** ! # include "CMN_SIZE" !---------------- ! Arguments !---------------- LOGICAL, INTENT(IN) :: FLG_MBL(IIPAR) REAL*8, INTENT(IN) :: VWC_SAT(IIPAR) REAL*8, INTENT(IN) :: VWC_SFC(IIPAR) REAL*8, INTENT(OUT) :: GWC_SFC(IIPAR) !---------------- ! Parameters !---------------- ! Dry density of soil ! particles (excluding pores) [kg/m3] REAL*8, PARAMETER :: DNS_PRT_SFC = 2650.0d0 ! liq. H2O density [kg/m3] REAL*8, PARAMETER :: DNS_H2O_LQD_STD = 1000.0d0 !----------------- ! Local variables !----------------- ! Longitude index INTEGER :: LON_IDX ! [kg m-3] Bulk density of dry surface soil REAL*8 :: DNS_BLK_DRY(IIPAR) !================================================================= ! VWC2GWC begins here! !================================================================= GWC_SFC(:) = 0.0D0 DNS_BLK_DRY(:) = 0.0D0 ! Loop over longitudes DO LON_IDX = 1, IIPAR ! If this is a mobilization candidate then... IF ( FLG_MBL(LON_IDX) ) THEN ! Assume volume of air pores when dry equals saturated VWC ! This implies air pores are completely filled by water in ! saturated soil ! Bulk density of dry surface soil [kg m-3] DNS_BLK_DRY(LON_IDX) = DNS_PRT_SFC & * ( 1.0d0 - VWC_SAT(LON_IDX) ) ! Gravimetric water content [ kg kg-1] GWC_SFC(LON_IDX) = VWC_SFC(LON_IDX) & * DNS_H2O_LQD_STD & / DNS_BLK_DRY(LON_IDX) ENDIF ENDDO ! Return to calling program END SUBROUTINE VWC2GWC !------------------------------------------------------------------------------ SUBROUTINE FRC_THR_NCR_WTR_GET( FLG_MBL, FRC_THR_NCR_WTR, 1 & MSS_FRC_CLY, GWC_SFC ) ! !****************************************************************************** ! Subroutine FRC_THR_NCR_WTR_GET computes the factor by which soil moisture ! increases threshold friction velocity. This parameterization is based on ! FMB99. Zender et al., exp. (5). (tdf, bmy, 4/5/04) ! ! Arguments as Input: ! =========================================================================== ! (1 ) FLG_MBL (LOGICAL) : Mobilization candidate flag [flags ] ! (3 ) MSS_FRC_CLY (REAL*8 ) : Mass fraction of clay [fraction] ! (4 ) GWC_SFC (REAL*8 ) : Gravimetric water content [kg/kg ] ! ! Arguments as Output: ! =========================================================================== ! (2 ) FRC_THR_NCR_WTR (REAL*8 ) : Factor by which moisture increases ! threshold friction velocity [fraction] ! ! NOTES: ! (1 ) Updated comments, cosmetic changes. Also now forces double-precision ! with "D" exponents. (tdf, bmy, 4/5/04) !****************************************************************************** ! # include "CMN_SIZE" ! Arguments LOGICAL, INTENT(IN) :: FLG_MBL(IIPAR) REAL*8, INTENT(IN) :: MSS_FRC_CLY(IIPAR) REAL*8, INTENT(IN) :: GWC_SFC(IIPAR) REAL*8, INTENT(OUT) :: FRC_THR_NCR_WTR(IIPAR) ! local variables INTEGER :: LON_IDX ! [idx] Counting index REAL*8 :: GWC_THR(IIPAR) ! [kg/kg] Threshold GWC !================================================================= ! FRC_THR_NCR_WTR_GET begins here! !================================================================= ! Initialize frc_thr_ncr_wtr(:) = 1.0D0 gwc_thr(:) = 0.0D0 ! Loop over longitudes DO LON_IDX = 1, IIPAR ! If this is a candidate for mobilization... IF ( FLG_MBL(LON_IDX) ) THEN !=========================================================== ! Adjust threshold velocity for inhibition by moisture ! frc_thr_ncr_wtr(lon_idx)=exp(22.7D0*vwc_sfc(lon_idx)) ! [frc] SRL96 ! ! Compute threshold soil moisture based on clay content ! GWC_THR=MSS_FRC_CLY*(0.17D0+0.14D0*MSS_FRC_CLY) [m3/m3] ! FMB99 p. 155 (14) ! ! 19991105 remove factor of mss_frc_cly from gwc_thr to ! improve large scale behavior. !=========================================================== ! [m3 m-3] GWC_THR(LON_IDX) = 0.17D0 + 0.14D0 * MSS_FRC_CLY(LON_IDX) IF ( GWC_SFC(LON_IDX) > GWC_THR(LON_IDX) ) & FRC_THR_NCR_WTR(LON_IDX) = SQRT(1.0D0+1.21D0 & * (100.0D0 * (GWC_SFC(LON_IDX)-GWC_THR(LON_IDX))) & ** 0.68D0) ! [frc] FMB99 p. 155 (15) ENDIF ENDDO ! Return to calling program END SUBROUTINE FRC_THR_NCR_WTR_GET !------------------------------------------------------------------------------ SUBROUTINE FRC_THR_NCR_DRG_GET( FRC_THR_NCR_DRG, FLG_MBL,,2 & Z0M, ZS0M ) ! !****************************************************************************** ! Subroutine FRC_THR_NCR_DRG_GET computes factor by which surface roughness ! increases threshold friction velocity. Zender et al., expression (3) ! This parameterization is based on MaB95 and GMB98. (tdf, bmy, 4/5/04) ! ! Arguments as Input: ! =========================================================================== ! (2 ) FLG_MBL (LOGICAL) : Mobilization candidate flag ! (3 ) Z0M (REAL*8 ) : Roughness length momentum ! : for erodible surfaces [m] ! (4 ) ZS0M (REAL*8 ) : Smooth roughness length [m] ! ! Arguments as Output: ! =========================================================================== ! (1 ) FRC_THR_NCR_DRG (REAL*8 ) : Factor by which surface roughness ! increases threshold fric. velocity [frac] ! ! NOTES: ! (1 ) Updated comments, cosmetic changes. Also now forces double-precision ! with "D" exponents. (tdf, bmy, 4/5/04) !****************************************************************************** ! ! References to F90 modules USE ERROR_MOD, ONLY : ERROR_STOP # include "CMN_SIZE" ! Size parameters !----------------- ! Arguments !----------------- LOGICAL, INTENT(IN) :: FLG_MBL(IIPAR) REAL*8, INTENT(IN) :: Z0M REAL*8, INTENT(IN) :: ZS0M REAL*8, INTENT(OUT) :: FRC_THR_NCR_DRG(IIPAR) !----------------- ! Local variables !----------------- ! [idx] Counting index integer lon_idx ! [frc] Efficient fraction of wind friction real*8 Feff ! [frc] Reciprocal of Feff real*8 Feff_rcp !================================================================= ! FRC_THR_NCR_DRG_GET begins here! !================================================================= FRC_THR_NCR_DRG(:) = 1.0D0 ! Adjust threshold velocity for inhibition by roughness elements ! Zender et al. Equ. (3), fd. ! [frc] MaB95 p. 16420, GMB98 p. 6207 FEFF = 1.0D0 - LOG( Z0M /ZS0M ) & / LOG( 0.35D0*( (0.1D0/ZS0M)**0.8D0) ) ! Error check if ( FEFF <= 0.0D0 .OR. FEFF > 1.0D0 ) THEN CALL ERROR_STOP( 'Feff out of range!', & 'FRC_THR_NCR_DRG_GET ("dust_dead_mod.f")' ) ENDIF ! Reciprocal of FEFF [fraction] FEFF_RCP = 1.0D0 / FEFF ! Loop over longitudes DO LON_IDX = 1, IIPAR ! If this is a mobilization candidate... IF ( FLG_MBL(LON_IDX) ) THEN ! Save into FRC_THR_NCR_DRG FRC_THR_NCR_DRG(LON_IDX) = FEFF_RCP ! fxm: 19991012 ! Set frc_thr_ncr_drg=1.0, equivalent to assuming mobilization ! takes place at smooth roughness length FRC_THR_NCR_DRG(LON_IDX) = 1.0D0 ENDIF ENDDO ! Return to calling program END SUBROUTINE FRC_THR_NCR_DRG_GET !------------------------------------------------------------------------------ SUBROUTINE WND_FRC_SLT_GET( FLG_MBL, WND_FRC, WND_FRC_SLT, 1 & WND_RFR, WND_RFR_THR_SLT ) ! !****************************************************************************** ! Subroutine WND_FRC_SLT_GET computes the saltating friction velocity. ! Saltation increases friction speed by roughening surface, AKA "Owen's ! effect". This acts as a positive feedback to the friction speed. GMB98 ! parameterized this feedback in terms of 10 m windspeeds, Zender et al. ! equ. (4). (tdf, bmy, 4/5/04, 1/25/07) ! ! Arguments as Input: ! =========================================================================== ! (1 ) FLG_MBL (LOGICAL) : Mobilization candidate flag ! (2 ) WND_FRC (REAL*8 ) : Surface friction velocity [m/s] ! (4 ) WND_RFR (REAL*8 ) : Wind speed at reference height [m/s] ! (5 ) WND_RFR_THR_SLT (REAL*8 ) : Thresh. 10m wind speed for saltation [m/s] ! ! Arguments as Output: ! =========================================================================== ! (3 ) WND_FRC_SLT (REAL*8 ) : Saltating friction velocity [m/s] ! ! NOTES: ! (1 ) Updated comments, cosmetic changes. Also now forces double-precision ! with "D" exponents. (tdf, bmy, 4/5/04) ! (2 ) Now eliminate Owen effect (tdf, bmy, 1/25/07) !****************************************************************************** ! # include "CMN_SIZE" ! Size parameters !------------------- ! Arguments !------------------- LOGICAL, INTENT(IN) :: FLG_MBL(IIPAR) REAL*8, INTENT(IN) :: WND_FRC(IIPAR) REAL*8, INTENT(IN) :: WND_RFR(IIPAR) REAL*8, INTENT(IN) :: WND_RFR_THR_SLT(IIPAR) REAL*8, INTENT(OUT) :: WND_FRC_SLT(IIPAR) !------------------- ! Local variables !------------------- ! [idx] Counting index INTEGER :: LON_IDX !--------------------------------------------------------------------- ! Prior to 1/25/07: ! Eliminate Owen effect, so comment out this code (tdf, bmy, 1/25/07) ! ! %%%%% DO NOT DELETE -- LEAVE THIS CODE COMMENTED OUT %%%%% ! !! [m/s] Reference windspeed excess over threshold !REAL*8 :: WND_RFR_DLT ! !! [m/s] Friction velocity increase from saltation !REAL*8 :: WND_FRC_SLT_DLT !--------------------------------------------------------------------- !================================================================= ! WND_FRC_SLT_GET begins here! !================================================================= ! [m/s] Saltating friction velocity WND_FRC_SLT(:) = WND_FRC(:) !------------------------------------------------------------------------------ ! Prior to 1/25/07: ! Eliminate the Owen effect. Note that the more computationally ! efficient way to do this is to just comment out the entire IF block. ! (tdf, bmy, 1/25/07) ! ! %%%%% DO NOT DELETE -- LEAVE THIS CODE COMMENTED OUT %%%%% ! ! ! Loop over longitudes ! DO LON_IDX = 1, IIPAR ! ! ! If this is a mobilization candidate, then only ! ! only apply Owen effect only when Uref > Ureft (tdf 4/5/04) ! IF ( FLG_MBL(LON_IDX) .AND. ! & WND_RFR(LON_IDX) >= WND_RFR_THR_SLT(LON_IDX) ) THEN ! ! !================================================================== ! ! Saltation roughens the boundary layer, AKA "Owen's effect" ! ! GMB98 p. 6206 Fig. 1 shows observed/computed u* dependence ! ! on observed U(1 m). GMB98 p. 6209 (12) has u* in cm s-1 and ! ! U, Ut in m s-1, personal communication, D. Gillette, 19990529 ! ! With everything in MKS, the 0.3 coefficient in GMB98 (12) ! ! becomes 0.003. Increase in friction velocity due to saltation ! ! varies as square of difference between reference wind speed ! ! and reference threshold speed. ! !================================================================== ! WND_RFR_DLT = WND_RFR(LON_IDX) - WND_RFR_THR_SLT(LON_IDX) ! ! ! Friction velocity increase from saltation GMB98 p. 6209 [m/s] ! wnd_frc_slt_dlt = 0.003D0 * wnd_rfr_dlt * wnd_rfr_dlt ! ! ! Saltation friction velocity, U*,s, Zender et al. Equ. (4). ! WND_FRC_SLT(LON_IDX) = WND_FRC(LON_IDX) ! & + WND_FRC_SLT_DLT ! [m s-1] ! ! ! !ctdf Eliminate Owen effect tdf 01/13/2K5 ! wnd_frc_slt(:) = wnd_frc(:) ! ! ENDIF ! ENDDO !------------------------------------------------------------------------------ ! Return to calling program END SUBROUTINE WND_FRC_SLT_GET !------------------------------------------------------------------------------ SUBROUTINE FLX_MSS_CACO3_MSK( DMT_VWR, FLG_MBL, 1,3 & FLX_MSS_VRT_DST_CACO3,MSS_FRC_CACO3, & MSS_FRC_CLY, MSS_FRC_SND ) ! !****************************************************************************** ! Subroutine FLX_MSS_CACO3_MSK masks dust mass flux by CaCO3 mass fraction at ! source. Theory: Uses soil CaCO3 mass fraction from Global Soil Data Task, ! 1999 (Sch99). Uses size dependent apportionment of CaCO3 from Claquin et ! al, 1999 (CSB99). (tdf, bmy, 4/5/04) ! ! Arguments as Input: ! =========================================================================== ! (1 ) DMT_VWR (REAL*8 ) : Mass weighted diameter resolved [m] ! (2 ) FLG_MBL (LOGICAL) : Mobilization candidate flag ! (3 ) FLX_MSS_VRT_DST_CACO3 (REAL*8 ) : Vert. mass flux of dust [kg/m2/s ] ! (4 ) MSS_FRC_CACO3 (REAL*8 ) : Mass fraction of CaCO3 [fraction] ! (5 ) MSS_FRC_CLY (REAL*8 ) : Mass fraction of clay [fraction] ! (6 ) MSS_FRC_SND (REAL*8 ) : Mass fraction of sand [fraction] ! ! Arguments as Output: ! =========================================================================== ! (3 ) FLX_MSS_VRT_DST_CACO3 (REAL*8 ) : Vertical mass flux of CaCO3 [kg/m2/s] ! ! NOTES: ! (1 ) Updated comments, cosmetic changes. Also now forces double-precision ! with "D" exponents. (tdf, bmy, 4/5/04) !****************************************************************************** ! ! References to F90 modules USE ERROR_MOD, ONLY : ERROR_STOP # include "CMN_SIZE" ! Size parameters !------------------ ! Arguments !------------------ LOGICAL, INTENT(IN) :: FLG_MBL(IIPAR) REAL*8, INTENT(IN) :: DMT_VWR(NDSTBIN) REAL*8, INTENT(IN) :: MSS_FRC_CACO3(IIPAR) REAL*8, INTENT(IN) :: MSS_FRC_CLY(IIPAR) REAL*8, INTENT(IN) :: MSS_FRC_SND(IIPAR) REAL*8, INTENT(INOUT) :: FLX_MSS_VRT_DST_CACO3(IIPAR,NDSTBIN) !------------------ ! Parameters !------------------ ! Maximum diameter of Clay soil texture CSB99 p. 22250 [m] REAL*8, PARAMETER :: DMT_CLY_MAX = 2.0d-6 ! Maximum diameter of Silt soil texture CSB99 p. 22250 [m] REAL*8, PARAMETER :: DMT_SLT_MAX = 50.0d-6 ! Density of CaCO3 http://www.ssc.on.ca/mandm/calcit.htm [kg/m3] REAL*8, PARAMETER :: DNS_CACO3 = 2950.0d0 !------------------ ! Local variables !------------------ ! [idx] Counting index INTEGER :: M ! [idx] Counting index for lon INTEGER :: LON_IDX ! [frc] Mass fraction of silt REAL*8 :: MSS_FRC_SLT(IIPAR) ! [frc] Fraction of soil CaCO3 in size bin REAL*8 :: MSS_FRC_CACO3_SZ_CRR ! [frc] Fraction of CaCO3 in clay REAL*8 :: MSS_FRC_CACO3_CLY ! [frc] Fraction of CaCO3 in silt REAL*8 :: MSS_FRC_CACO3_SLT ! [frc] Fraction of CaCO3 in sand REAL*8 :: MSS_FRC_CACO3_SND !================================================================= ! FLX_MSS_CACO3_MSK !================================================================= ! INITIALIZE MSS_FRC_SLT(:) = 0.0D0 ! Loop over dust bins DO M = 1, NDSTBIN ! Loop over longitudes DO LON_IDX = 1, IIPAR !=========================================================== ! Simple technique is to mask dust mass by tracer mass ! fraction. The model transports (hence conserves) CaCO3 ! rather than total dust itself. The method assumes source, ! transport, and removal processes are linear with tracer ! mass !=========================================================== ! If this is a mobilization candidate, then... IF ( FLG_MBL(LON_IDX) ) THEN ! 20000320: Currently this is only process in ! dust model requiring mss_frc_slt ! [frc] Mass fraction of silt MSS_FRC_SLT(LON_IDX) = & MAX(0.0D0, 1.0D0 -MSS_FRC_CLY(LON_IDX) & -MSS_FRC_SND(LON_IDX)) ! CSB99 showed that CaCO3 is not uniformly distributed ! across sizes. There is more CaCO3 per unit mass of ! silt than per unit mass of clay. ! Fraction of CaCO3 in clay CSB99 p. 22249 Figure 1b MSS_FRC_CACO3_CLY = MAX(0.0D0,-0.045D0+0.5D0 & * MIN(0.5D0,MSS_FRC_CLY(LON_IDX))) ! Fraction of CaCO3 in silt CSB99 p. 22249 Figure 1a MSS_FRC_CACO3_SLT = MAX(0.0D0,-0.175D0+1.4D0 & * MIN(0.5D0,MSS_FRC_SLT(LON_IDX))) ! Fraction of CaCO3 in sand CSB99 p. 22249 Figure 1a MSS_FRC_CACO3_SND = 1.0D0 - MSS_FRC_CACO3_CLY & - MSS_FRC_CACO3_SND ! Set CaCO3 fraction of total CaCO3 for each transport bin IF ( DMT_VWR(M) < DMT_CLY_MAX ) THEN ! Transport bin carries Clay ! Fraction of soil CaCO3 in size bin MSS_FRC_CACO3_SZ_CRR = MSS_FRC_CACO3_CLY ELSE IF ( DMT_VWR(M) < DMT_SLT_MAX ) THEN ! Transport bin carries Silt ! Fraction of soil CaCO3 in size bin MSS_FRC_CACO3_SZ_CRR = MSS_FRC_CACO3_SLT ELSE ! Transport bin carries Sand ! Fraction of soil CaCO3 in size bin MSS_FRC_CACO3_SZ_CRR = MSS_FRC_CACO3_SND ENDIF ! Error checks IF ( MSS_FRC_CACO3_SZ_CRR < 0.0D0 .OR. & MSS_FRC_CACO3_SZ_CRR > 1.0D0 ) THEN CALL ERROR_STOP( & 'mss_frc_CaC_s < 0.0.or.mss_frc_CaC_s > 1.0!', & 'FLX_MSS_CACO3_MSK ("dust_dead_mod.f")' ) ENDIF IF ( MSS_FRC_CACO3(LON_IDX) < 0.0D0 .OR. & MSS_FRC_CACO3(LON_IDX) > 1.0D0 ) THEN CALL ERROR_STOP( & 'mss_frc_CaCO3_s < 0.0.or.mss_frc_CaCO3 > 1.0!', & ' FLX_MSS_CACO3_MSK ("dust_dead_mod.f")' ) ENDIF ! Convert dust flux to CaCO3 flux FLX_MSS_VRT_DST_CACO3(LON_IDX,M) = & FLX_MSS_VRT_DST_CACO3(LON_IDX,M) ! [KG m-2 s-1] & * MSS_FRC_CACO3(LON_IDX) ! [frc] Mass fraction of ! CaCO3 (at this location) ! 20020925 fxm: Remove size dependence of CaCO3 & * 1.0D0 ENDIF ENDDO ENDDO ! Return to calling program END SUBROUTINE FLX_MSS_CACO3_MSK !------------------------------------------------------------------------------ SUBROUTINE FLX_MSS_HRZ_SLT_TTL_WHI79_GET( DNS_MDP, FLG_MBL, 1 & QS_TTL, U_S, U_ST ) ! !****************************************************************************** ! Subroutine FLX_MSS_HRZ_SLT_TTL_WHI79_GET computes vertically integrated ! streamwise mass flux of particles. Theory: Uses method proposed by White ! (1979). See Zender et al., expr (10). fxm: use surface air density not ! midlayer density (tdf, bmy, 4/5/04) ! ! Arguments as Input: ! ============================================================================ ! (1 ) DNS_MDP (REAL*8 ) : Midlayer density [g/m3 ] ! (2 ) FLG_MBL (LOGICAL) : Mobilization candidate flag [flag ] ! (4 ) U_S (REAL*8 ) : Surface friction velocity [m/s ] ! (5 ) U_ST (REAL*8 ) : Threshold friction spd for saltation [m/s ] ! ! Arguments as Output: ! ============================================================================ ! (3 ) QS_TTL (REAL*8 ) : Vertically integrated streamwise mass flux [kg/m/s] ! ! NOTES: ! (1 ) Updated comments, cosmetic changes. Also now forces double-precision ! with "D" exponents. (tdf, bmy, 4/5/04) !****************************************************************************** ! # include "CMN_SIZE" !------------------ ! Arguments !------------------ LOGICAL, INTENT(IN) :: FLG_MBL(IIPAR) REAL*8, INTENT(IN) :: DNS_MDP(IIPAR) REAL*8, INTENT(IN) :: U_S(IIPAR) REAL*8, INTENT(IN) :: U_ST(IIPAR) REAL*8, INTENT(OUT) :: QS_TTL(IIPAR) !------------------ ! Parameters !------------------ ! [frc] Saltation constant Whi79 p. 4648, MaB97 p. 16422 REAL*8, PARAMETER :: CST_SLT = 2.61d0 !------------------ ! Local variables !------------------ ! [frc] Ratio of wind friction threshold to wind friction real*8 :: U_S_rat ! [idx] Counting index for lon integer :: lon_idx !================================================================= ! FLX_MSS_HRZ_SLT_TTL_WHI79_GET begins here! !================================================================= ! Initialize QS_TTL(:) = 0.0D0 ! Loop over longitudes DO LON_IDX = 1, IIPAR ! If this is a mobilization candidate and the friction ! velocity is above the threshold for saltation... IF ( FLG_MBL(LON_IDX) .AND. & U_S(LON_IDX) > U_ST(LON_IDX) ) THEN ! Ratio of wind friction threshold to wind friction U_S_RAT = U_ST(LON_IDX) / U_S(LON_IDX) ! Whi79 p. 4648 (19), MaB97 p. 16422 (28) QS_TTL(LON_IDX) = ! [kg m-1 s-1] & CST_SLT * DNS_MDP(LON_IDX) * (U_S(LON_IDX)**3.0D0) & * (1.0D0-U_S_RAT) * (1.0D0+U_S_RAT) & * (1.0D0+U_S_RAT) / GRV_SFC ENDIF ENDDO ! Return to calling program END SUBROUTINE FLX_MSS_HRZ_SLT_TTL_WHI79_GET !------------------------------------------------------------------------------ SUBROUTINE FLX_MSS_VRT_DST_TTL_MAB95_GET( DST_SLT_FLX_RAT_TTL, 1 & FLG_MBL, & FLX_MSS_HRZ_SLT_TTL, & FLX_MSS_VRT_DST_TTL, & MSS_FRC_CLY ) ! !****************************************************************************** ! Subroutine FLX_MSS_VRT_DST_TTL_MAB95_GET diagnoses total vertical mass flux ! of dust from vertically integrated streamwise mass flux, Zender et al., ! expr. (11). (tdf, bmy, 4/5/04) ! ! Theory: Uses clay-based method proposed by Marticorena & Bergametti (1995) ! Their parameterization is based only on data for mss_frc_cly < 0.20 ! For clayier soils, dst_slt_flx_rat_ttl may behave dramatically differently ! Whether this behavior changes when mss_frc_cly > 0.20 is unknown ! Anecdotal evidence suggests vertical flux decreases for mss_frc_cly > 0.20 ! Thus we use min[mss_frc_cly,0.20] in MaB95 parameterization ! ! Arguments as Input: ! ============================================================================ ! (2 ) FLG_MBL (LOGICAL) : Mobilization candidate flag ! (3 ) FLX_MSS_HRZ_SLT_TTL (REAL*8 ) : Vertically integrated streamwise ! mass flux [kg/m/s] ! (5 ) MSS_FRC_CLY (REAL*8 ) : Mass fraction clay [fraction] ! ! Arguments as Output: ! ============================================================================ ! (1 ) DST_SLT_FLX_RAT_TTL (REAL*8 ) : Ratio of vertical dust flux t ! to streamwise mass flux [1/m] ! (4 ) FX_MSS_VRT_DST_TTL (REAL*8 ) : Total vert. mass flux of dust [kg/m2/s] ! ! NOTES: ! (1 ) Updated comments, cosmetic changes. Also now forces double-precision ! with "D" exponents. (tdf, bmy, 4/5/04) !****************************************************************************** ! # include "CMN_SIZE" ! Size parameters !----------------- ! Arguments !----------------- LOGICAL, INTENT(IN) :: FLG_MBL(IIPAR) REAL*8, INTENT(IN) :: FLX_MSS_HRZ_SLT_TTL(IIPAR) REAL*8, INTENT(IN) :: MSS_FRC_CLY(IIPAR) REAL*8, INTENT(OUT) :: DST_SLT_FLX_RAT_TTL(IIPAR) REAL*8, INTENT(OUT) :: FLX_MSS_VRT_DST_TTL(IIPAR) !----------------- ! Local variables !----------------- ! [idx] Counting index for lon INTEGER :: LON_IDX ! [frc] Mass fraction clay limited to 0.20 REAL*8 :: MSS_FRC_CLY_VLD ! [frc] Natural log of 10 REAL*8 :: LN10 !================================================================= ! FLX_MSS_VRT_DST_TTL_MAB95_GET !================================================================= ! Initialize LN10 = LOG(10.0D0) DST_SLT_FLX_RAT_TTL(:) = 0.0D0 FLX_MSS_VRT_DST_TTL(:) = 0.0D0 ! Loop over longitudes DO LON_IDX = 1, IIPAR ! If this is a mobilization candidate... IF ( FLG_MBL(LON_IDX) ) then ! 19990603: fxm: Dust production is EXTREMELY sensitive to ! this parameter, which changes flux by 3 orders of magnitude ! in 0.0 < mss_frc_cly < 0.20 MSS_FRC_CLY_VLD = MIN(MSS_FRC_CLY(LON_IDX),0.2D0) ! [frc] DST_SLT_FLX_RAT_TTL(LON_IDX) = ! [m-1] & 100.0D0 * EXP(LN10*(13.4D0*MSS_FRC_CLY_VLD-6.0D0)) ! MaB95 p. 16423 (47) FLX_MSS_VRT_DST_TTL(LON_IDX) = ! [kg M-1 s-1] & FLX_MSS_HRZ_SLT_TTL(LON_IDX) & * DST_SLT_FLX_RAT_TTL(LON_IDX) ENDIF ENDDO ! Return to calling program END SUBROUTINE FLX_MSS_VRT_DST_TTL_MAB95_GET !------------------------------------------------------------------------------ SUBROUTINE DST_PSD_MSS( OVR_SRC_SNK_FRC, MSS_FRC_SRC, 1 & OVR_SRC_SNK_MSS, NDSTBIN, DST_SRC_NBR ) ! !****************************************************************************** ! Subroutine DST_PSD_MSS computes OVR_SRC_SNK_MSS from OVR_SRC_SNK_FRC ! and MSS_FRC_SRC. (tdf, bmy, 4/5/04) ! ! Multiply ovr_src_snk_frc(src_idx,*) by mss_frc(src_idx) to obtain ! absolute mass fraction mapping from source dists. to sink bins ! ! Arguments as Input: ! ============================================================================ ! (1 ) OVR_SRC_SNK_FRC (REAL*8 ) : Mass overlap, Mij, Zender p. 5, Equ. 12 ! (2 ) MSS_FRC_SRC (REAL*8 ) : Mass fraction in each mode (Table 1, M) ! (4 ) NDSTBIN (INTEGER) : Number of GEOS_CHEM dust bins ! (5 ) DST_SRC_NBR (INTEGER) : Number of source modes ! ! Arguments as Output: ! ============================================================================ ! (3 ) OVR_SRC_SNK_MSS (REAL*8 ) : Mass of stuff ??? ! ! NOTES: ! (1 ) Updated comments, cosmetic changes. Also now forces double-precision ! with "D" exponents. (tdf, bmy, 4/5/04) !****************************************************************************** ! !----------------- ! Arguments !----------------- INTEGER, INTENT(IN) :: DST_SRC_NBR, NDSTBIN REAL*8, INTENT(IN) :: OVR_SRC_SNK_FRC(DST_SRC_NBR,NDSTBIN) REAL*8, INTENT(IN) :: MSS_FRC_SRC(DST_SRC_NBR) REAL*8, INTENT(OUT) :: OVR_SRC_SNK_MSS(DST_SRC_NBR,NDSTBIN) !----------------- ! Local variables !----------------- INTEGER :: SRC_IDX, SNK_IDX REAL*8 :: MSS_FRC_TRN_DST_SRC(NDSTBIN) REAL*8 :: OVR_SRC_SNK_MSS_TTL !================================================================= ! DST_PSD_MSS begins here! !================================================================= ! Fraction of vertical dust flux which is transported OVR_SRC_SNK_MSS_TTL = 0.0D0 ! Fraction of transported dust mass at source DO SNK_IDX = 1, NDSTBIN MSS_FRC_TRN_DST_SRC(SNK_IDX) = 0.0D0 ENDDO DO SNK_IDX = 1, NDSTBIN DO SRC_IDX = 1, DST_SRC_NBR OVR_SRC_SNK_MSS (SRC_IDX,SNK_IDX) = ! [frc] & OVR_SRC_SNK_FRC (SRC_IDX,SNK_IDX) & * MSS_FRC_SRC (SRC_IDX) ! [frc] ENDDO ENDDO ! Split double do loop into 2 parts tdf 10/22/2K3 DO SNK_IDX = 1, NDSTBIN DO SRC_IDX = 1, DST_SRC_NBR ! [frc] Fraction of transported dust mass at source MSS_FRC_TRN_DST_SRC(SNK_IDX) = & MSS_FRC_TRN_DST_SRC(SNK_IDX) & + OVR_SRC_SNK_MSS(SRC_IDX,SNK_IDX) ! [frc] Compute total transported mass fraction of dust flux OVR_SRC_SNK_MSS_TTL = OVR_SRC_SNK_MSS_TTL & + OVR_SRC_SNK_MSS (SRC_IDX,snk_idx) ENDDO ENDDO ! Convert fraction of mobilized mass to fraction of transported mass DO SNK_IDX = 1, NDSTBIN MSS_FRC_TRN_DST_SRC (SNK_IDX) = & MSS_FRC_TRN_DST_SRC (SNK_IDX) / OVR_SRC_SNK_MSS_TTL ENDDO ! Return to calling program END SUBROUTINE DST_PSD_MSS !------------------------------------------------------------------------------ SUBROUTINE FLX_MSS_VRT_DST_PRT( FLG_MBL, 1 & FLX_MSS_VRT_DST, & FLX_MSS_VRT_DST_TTL ) ! !****************************************************************************** ! Subroutine FLX_MSS_VRT_DST_PRT partitions total vertical mass flux of dust ! into transport bins. Assumes a trimodal lognormal probability density ! function (see Zender et al., p. 5). (tdf, bmy, 4/5/04) ! ! DST_SRC_NBR = 3 - trimodal size distribution in source c regions (p. 5) ! OVR_SRC_SNK_MSS [frc] computed in dst_psd_mss, called from dust_mod.f ! ! Arguments as Input: ! ============================================================================ ! (1 ) FLG_MBL (LOGICAL) : Mobilization candidate flag ! (3 ) FLX_MSS_VRT_DST_TTL (REAL*8 ) : Total vert. mass flux of dust [kg/m2/s] ! ! Arguments as Output: ! ============================================================================ ! (2 ) FLX_MSS_VRT_DST (REAL*8 ) : Vertical mass flux of dust [kg/m2/s] ! ! NOTES: ! (1 ) Updated comments, cosmetic changes. Also now forces double-precision ! with "D" exponents. (tdf, bmy, 4/5/04) !****************************************************************************** ! # include "CMN_SIZE" ! Size parameters ! Arguments LOGICAL, INTENT(IN) :: FLG_MBL(IIPAR) REAL*8, INTENT(IN) :: FLX_MSS_VRT_DST_TTL(IIPAR) REAL*8, INTENT(OUT) :: FLX_MSS_VRT_DST(IIPAR,NDSTBIN) ! Local variables INTEGER :: LON_IDX ! [idx] Counting index for lon INTEGER :: SRC_IDX ! [idx] Counting index for src INTEGER :: SNK_IDX ! [idx] Counting index for snk INTEGER :: SNK_NBR ! [nbr] Dimension size !================================================================= ! FLX_MSS_VRT_DST_PRT begins here! !================================================================= ! Initialize FLX_MSS_VRT_DST(:,:) = 0.0D0 ! [frc] ! Loop over longitudes (NB: Inefficient loop order) DO LON_IDX = 1, IIPAR ! If this is a mobilization candidate... IF ( FLG_MBL(LON_IDX) ) THEN ! Loop over source & sink indices DO SNK_IDX = 1, NDSTBIN DO SRC_IDX = 1, DST_SRC_NBR FLX_MSS_VRT_DST(LON_IDX,SNK_IDX) = ! [kg m-2 s-1] & FLX_MSS_VRT_DST(LON_IDX,SNK_IDX) & + OVR_SRC_SNK_MSS(SRC_IDX,SNK_IDX) & * FLX_MSS_VRT_DST_TTL(LON_IDX) ENDDO ENDDO ENDIF ENDDO ! Return to calling program END SUBROUTINE FLX_MSS_VRT_DST_PRT !------------------------------------------------------------------------------ SUBROUTINE TM_2_IDX_WGT() ! routine eliminated: see original code END SUBROUTINE TM_2_IDX_WGT !------------------------------------------------------------------------------ SUBROUTINE LND_FRC_MBL_GET( DOY, FLG_MBL, LAT_RDN, 1,5 & LND_FRC_DRY, LND_FRC_MBL, MBL_NBR, & ORO, SFC_TYP, SNW_FRC, & TPT_SOI, TPT_SOI_FRZ, VAI_DST ) ! !****************************************************************************** ! Subroutine LND_FRC_MBL_GET returns the fraction of each GEOS-CHEM grid ! box which is suitable for dust mobilization. This routine is called ! by DST_MBL. (tdf, bmy, 4/5/04, 1/25/07) ! ! The DATE is used to obtain the time-varying vegetation cover. ! Routine currently uses latitude slice of VAI from time-dependent surface ! boundary dataset (tdf, 10/27/03). LAI/VAI algorithm is from CCM:lsm/phenol ! () Bon96. The LSM data are mid-month values, i.e., valid on the 15th of ! ! the month.! ! ! Criterion for mobilisation candidate (tdf, 4/5/04): ! (1) first, must be a land point, not ocean, not ice ! (2) second, it cannot be an inland lake, wetland or ice ! (3) modulated by vegetation type ! (4) modulated by subgridscale wetness ! (5) cannot be snow covered ! ! Arguments as Input: ! ============================================================================ ! (1 ) DOY (REAL*8 ) : Day of year [1.0-366.0] ! (3 ) LAT_RDN (REAL*8 ) : Latitude [radians ] ! (4 ) LND_FRC_DRY (REAL*8 ) : Dry land fraction [fraction ] ! (7 ) ORO (REAL*8 ) : Orography: land/ocean/ice [flags ] ! (8 ) SFC_TYP (INTEGER) : LSM surface type (0..28) [unitless ] ! (9 ) SNW_FRC (REAL*8 ) : Fraction of surface covered by snow [fraction ] ! (10) TPT_SOI (REAL*8 ) : Soil temperature [K ] ! (11) TPT_SOI_FRZ (REAL*8 ) : Temperature of frozen soil [K ] ! (12) VAI_DST (REAL*8 ) : Vegetation area index, one-sided [m2/m2 ] ! ! Arguments as Output: ! ============================================================================ ! (2 ) FLG_MBL (LOGICAL) : Mobilization candidate flag [flag ] ! (5 ) LND_FRC_MBL (REAL*8 ) : Bare ground fraction [fraction ] ! (6 ) MBL_NBR (INTEGER) : Number of mobilization candidates [unitless ] ! ! NOTES: ! (1 ) Updated comments, cosmetic changes. Also now forces double-precision ! with "D" exponents. (tdf, bmy, 4/5/04) ! (2 ) For the GOCART source function, we don't use VAI, so set FLG_VAI_TVBDS ! = .FALSE. and disable calls to ERROR_STOP (tdf, bmy, 1/25/07) !****************************************************************************** ! ! References to F90 modules USE ERROR_MOD, ONLY : ERROR_STOP # include "CMN_SIZE" ! Size parameters # include "CMN_GCTM" ! PI !------------------ ! Arguments !------------------ INTEGER, INTENT(IN) :: SFC_TYP(IIPAR) REAL*8, INTENT(IN) :: DOY REAL*8, INTENT(IN) :: LAT_RDN REAL*8, INTENT(IN) :: LND_FRC_DRY(IIPAR) REAL*8, INTENT(IN) :: ORO(IIPAR) REAL*8, INTENT(IN) :: SNW_FRC(IIPAR) REAL*8, INTENT(IN) :: TPT_SOI(IIPAR) REAL*8, INTENT(IN) :: TPT_SOI_FRZ REAL*8, INTENT(IN) :: VAI_DST(IIPAR) INTEGER, INTENT(OUT) :: MBL_NBR LOGICAL, INTENT(OUT) :: FLG_MBL(IIPAR) REAL*8, INTENT(OUT) :: LND_FRC_MBL(IIPAR) !------------------ ! Parameters !------------------ ! VAI threshold quench [m2/m2] REAL*8, PARAMETER :: VAI_MBL_THR = 0.30D0 !------------------ ! Local variables !------------------ ! [idx] Counting index INTEGER :: IDX_IDX ! [idx] Interpolation month, future INTEGER :: IDX_MTH_GLB ! [idx] Interpolation month, past INTEGER :: IDX_MTH_LUB ! [idx] Longitude index array (land) INTEGER :: LND_IDX(IIPAR) ! [nbr] Number of land points INTEGER :: LND_NBR ! [idx] Counting index for longitude INTEGER :: LON_IDX ! [idx] Surface type index INTEGER :: SFC_TYP_IDX ! [idx] Surface sub-gridscale index INTEGER :: SGS_IDX !------------------------------------------------------------------- ! Prior to 1/25/07: ! For GOCART source function, we don't use VAI (tdf, bmy, 1/25/07) ! ! %%%%% DO NOT DELETE -- LEAVE THIS CODE COMMENTED OUT %%%%% ! !! [flg] Use VAI data from time-varying boundary dataset ! LOGICAL :: FLG_VAI_TVBDS = .TRUE. !------------------------------------------------------------------- ! For GOCART source function, we do not use VAI (tdf, bmy, 1/25/07) LOGICAL :: FLG_VAI_TVBDS = .FALSE. ! [flg] Add 182 days in southern hemisphere LOGICAL :: FLG_SH_ADJ = .TRUE. ! [dgr] Latitude REAL*8 :: LAT_DGR ! [m2 m-2] Leaf + stem area index, one-sided REAL*8 :: VAI_SGS !================================================================= ! LND_FRC_MBL_GET begins here! !================================================================= ! Error check IF ( VAI_MBL_THR <= 0.0d0 ) THEN CALL ERROR_STOP( 'VAI_MBL_THR <= 0.0!', & 'LND_FRC_MBL_GET ("dust_dead_mod.f")' ) ENDIF ! Latitude (degrees) LAT_DGR = 180.0D0 * LAT_RDN/PI ! Initialize outputs MBL_NBR = 0 DO LON_IDX = 1, IIPAR FLG_MBL(LON_IDX) = .FALSE. ENDDO LND_FRC_MBL(:) = 0.0D0 !================================================================= ! For dust mobilisation, we need to have land! tdf 10/27/2K3 ! Set up lnd_idx to hold the longitude indices for land ! Land ahoy! !================================================================= LND_NBR = 0 DO LON_IDX = 1, IIPAR IF ( ORO_IS_LND( ORO(LON_IDX)) ) THEN LND_NBR = LND_NBR + 1 LND_IDX(LND_NBR) = LON_IDX ENDIF ENDDO ! Much ado about nothing (no land points) IF ( LND_NBR == 0 ) RETURN !----------------------------------------------------------------------------- ! Prior to 1/25/07: ! When GOCART source function is used, VAI flag is NOT used, so ! we need to disable the ERROR_STOP call (tdf, bmy, 1/25/07) ! ! %%%%% DO NOT DELETE -- LEAVE THIS CODE COMMENTED OUT %%%%% ! ! ! Introduce error message for flg_vai_tvbds=F (VAI not used!) ! IF ( .not. FLG_VAI_TVBDS ) THEN !c print *,' FLG_VAI_TVBDS is false: GOCART source function used' ! CALL ERROR_STOP( 'FLG_VAI_TVBDS=F', ! & 'LND_FRC_MBL_GET ("dust_dead_mod.f")' ) ! ENDIF !----------------------------------------------------------------------------- !================================================================= ! Only land points are possible candidates for dust mobilization !================================================================= ! Loop over land points DO IDX_IDX = 1, LND_NBR LON_IDX = LND_IDX(IDX_IDX) ! Store surface blend of current gridpoint SFC_TYP_IDX = SFC_TYP(LON_IDX) ! Check for wet or frozen conditions - no mobilisation allowed ! Surface type 1 = inland lakes & land ice ! Surface type 27 = wetlands IF ( SFC_TYP_IDX <= 1 .OR. SFC_TYP_IDX >= 27 .OR. & TPT_SOI(LON_IDX) < TPT_SOI_FRZ ) THEN ! SET bare ground fraction to zero LND_FRC_MBL(LON_IDX) = 0.0D0 ELSE !------------------------- ! If we are using VAI... !------------------------- IF ( FLG_VAI_TVBDS ) THEN ! "bare ground" fraction of current gridcell decreases ! linearly from 1.0 to 0.0 as VAI increases from 0.0 to ! vai_mbl_thr. NOTE: vai_mbl_thr set to 0.3 (tdf, 4/5/04) LND_FRC_MBL(LON_IDX) = & 1.0D0 - MIN(1.0D0, MIN(VAI_DST(LON_IDX), & VAI_MBL_THR) / VAI_MBL_THR) !--------------------------- ! If we're not using VAI... !--------------------------- ELSE !----------------------------------------------------------------------------- ! Prior to 1/25/07: ! When GOCART source function is used, VAI flag is NOT used, so ! we need to disable the ERROR_STOP call. (tdf, bmy, 1/25/07) ! ! %%%%% DO NOT DELETE -- LEAVE THIS CODE COMMENTED OUT %%%%% ! ! CALL ERROR_STOP( 'FLG_VAI_TVBDS=F', ! & 'LND_FRC_MBL_GET ("dust_dead_mod.f")' ) !----------------------------------------------------------------------------- ! For GOCART source function, set the bare ! ground fraction to 1 (tdf, bmy, 1/25/07) LND_FRC_MBL(LON_IDX) = 1.0D0 ENDIF ENDIF ! endif normal land !============================================================== ! We have now filled "lnd_frc_mbl" the land fraction suitable ! for mobilisation. Adjust for factors which constrain entire ! gridcell LND_FRC_MBL modulated by LND_FRC_DRY and SNW_FRC. ! (tdf, 4/5/04) !============================================================== ! Take the bare ground fraction, multiply by the fraction ! that is dry and that is NOT covered by snow LND_FRC_MBL(LON_IDX) = LND_FRC_MBL(LON_IDX) & * LND_FRC_DRY(LON_IDX) & * ( 1.0D0 - SNW_FRC(LON_IDX) ) ! Error check IF ( LND_FRC_MBL(lon_idx) > 1.0D0 ) THEN CALL ERROR_STOP( 'LND_FRC_MBL > 1!', & 'LND_FRC_MBL_GET ("dust_dead_mod.f")' ) ENDIF IF ( LND_FRC_MBL(LON_IDX) < 0.0D0 ) then CALL ERROR_STOP( 'LND_FRC_MBL < 0!', & 'LND_FRC_MBL_GET ("dust_dead_mod.f")' ) ENDIF ! If there is dry land in this longitude if ( LND_FRC_MBL(LON_IDX) > 0.0D0 ) then ! Set flag, we have a candidate! FLG_MBL(LON_IDX) = .TRUE. ! Increment # of candidates MBL_NBR = MBL_NBR + 1 ENDIF ENDDO ! Return to calling program END SUBROUTINE LND_FRC_MBL_GET !------------------------------------------------------------------------------ SUBROUTINE DST_ADD_LON( Q, Q_TTL ) ! !****************************************************************************** ! Subroutine DST_ADD_LON dst_add_lon() computes and returns the total ! property (e.g., mixing ratio, flux), obtained by simply adding along the ! (dust) constituent dimension, when given an 3-D array of an additive ! property (e.g., mixing ratio, flux). (tdf, bmy, 4/5/04) ! ! Arguments as Input: ! ============================================================================ ! (1 ) q (REAL*8) : Total property ! ! Arguments as Output: ! ============================================================================ ! (2 ) q_ttl (REAL*8) : Property for each size class ! ! NOTES: ! (1 ) Updated comments, cosmetic changes. Also now forces double-precision ! with "D" exponents. (tdf, bmy, 4/5/04) !****************************************************************************** ! # include "CMN_SIZE" ! Size parameters ! Arguments REAL*8, INTENT(IN) :: Q(IIPAR,NDSTBIN) REAL*8, INTENT(OUT) :: Q_TTL(IIPAR) ! Local variables INTEGER :: I, M !================================================================= ! DST_ADD_LON begins here! !================================================================= ! Initialize Q_TTL = 0d0 ! Loop over dust bins DO M = 1, NDSTBIN ! Loop over longitudes DO I = 1, IIPAR ! Integrate! Q_TTL(I) = Q_TTL(I) + Q(I,M) ENDDO ENDDO ! Return to calling program END SUBROUTINE DST_ADD_LON !------------------------------------------------------------------------------ SUBROUTINE DST_TVBDS_GET( LAT_IDX, VAI_DST_OUT ) 1 ! !****************************************************************************** ! Subroutine DST_TVBDS_GET returns a specifed latitude slice of VAI data. ! (tdf, bmy, 4/5/04) ! ! Arguments as Input: ! ============================================================================ ! (1 ) LAT_IDX (INTEGER) : Latitude index ! ! Arguments as Output: ! ============================================================================ ! (2 ) VAI_DST_OUT (REAL*8 ) : Vegetation area index, 1-sided, current [m2/m2] ! ! NOTES: ! (1 ) Updated comments, cosmetic changes. Also now forces double-precision ! with "D" exponents. (tdf, bmy, 4/5/04) !****************************************************************************** ! # include "CMN_SIZE" ! Size parameters ! Arguments INTEGER, INTENT(IN) :: LAT_IDX REAL*8, INTENT(OUT) :: VAI_DST_OUT(:) ! Local variables INTEGER :: LON_IDX !================================================================= ! DST_TVBDS_GET begins here! !================================================================= ! Return lat slice of VAI [m2/m2] DO LON_IDX = 1, IIPAR VAI_DST_OUT(LON_IDX) = VAI_DST(LON_IDX,LAT_IDX) ENDDO ! Return to calling program END SUBROUTINE DST_TVBDS_GET !------------------------------------------------------------------------------ SUBROUTINE OVR_SRC_SNK_FRC_GET( SRC_NBR, MDN_SRC, 1,9 & GSD_SRC, SNK_NBR, & DMT_MIN_SNK, DMT_MAX_SNK, & OVR_SRC_SNK_FRC ) ! !****************************************************************************** ! Subroutine OVR_SRC_SNK_FRC_GET, given one set (the "source") of lognormal ! distributions, and one set of bin boundaries (the "sink"), computes and ! returns the overlap factors between the source distributions and the sink ! bins. (tdf, bmy, 4/5/04) ! ! The output is a matrix, Mij, OVR_SRC_SNK_FRC(SRC_NBR,SNK_NBR) ! Element ovr_src_snk_frc(i,j) is the fraction of size distribution i ! in group src that overlaps sink bin j ! ! Arguments as Input: ! ============================================================================ ! (1 ) SRC_NBR (INTEGER) : Dimension size [unitless] ! (2 ) MDN_SRC (REAL*8 ) : Mass median particle size [m ] ! (3 ) GSD_SRC (REAL*8 ) : Geometric standard deviation [fraction] ! (4 ) SNK_NBR (INTEGER) : Dimension size [unitless] ! (5 ) DMT_MIN_SNK (REAL*8 ) : Minimum diameter in bin [m ] ! (6 ) DMT_MAX_SNK (REAL*8 ) : Maximum diameter in bin [m ] ! ! Arguments as Output: ! ============================================================================ ! (7 ) OVR_SRC_SNK_FRC (REAL*8 ) : Fractional overlap of src with snk, Mij. ! ! NOTES ! (1 ) Updated comments, cosmetic changes. Also now forces double-precision ! with "D" exponents. (tdf, bmy, 4/5/04) !****************************************************************************** ! ! References to F90 modules USE ERROR_MOD, ONLY : GEOS_CHEM_STOP ! Arguments INTEGER, INTENT(IN) :: SRC_NBR REAL*8, INTENT(IN) :: MDN_SRC(SRC_NBR) REAL*8, INTENT(IN) :: GSD_SRC(SRC_NBR) INTEGER, INTENT(IN) :: SNK_NBR REAL*8, INTENT(IN) :: DMT_MIN_SNK(SNK_NBR) REAL*8, INTENT(IN) :: DMT_MAX_SNK(SNK_NBR) REAL*8, INTENT(OUT) :: OVR_SRC_SNK_FRC(SRC_NBR,SNK_NBR) ! Local LOGICAL :: FIRST = .TRUE. INTEGER :: SRC_IDX ! [idx] Counting index for src INTEGER :: SNK_IDX ! [idx] Counting index for snk REAL*8 :: LN_GSD ! [frc] ln(gsd) REAL*8 :: SQRT2LNGSDI ! [frc] Factor in erf() argument REAL*8 :: LNDMAXJOVRDMDNI ! [frc] Factor in erf() argument REAL*8 :: LNDMINJOVRDMDNI ! [frc] Factor in erf() argument !================================================================= ! OVR_SRC_SNK_FRC_GET begins here !================================================================= IF ( FIRST ) THEN ! Test if ERF is implemented OK on this platform ! 19990913: erf() in SGI /usr/lib64/mips4/libftn.so is bogus IF ( ABS( 0.8427d0 - ERF(1.0d0) ) / 0.8427d0 > 0.001d0 ) THEN WRITE(6,'(a,f12.10)' ) 'erf(1.0D0) = ',ERF(1.0D0) WRITE( 6, '(a)' ) 'ERF error in OVR_SRC_SNK_FRC_GET!' CALL GEOS_CHEM_STOP ENDIF ! Another ERF check IF ( ERF( 0.0D0 ) /= 0.0D0 ) THEN WRITE (6,'(a,f12.10)') 'erf(0.0D0) = ',ERF(0.0D0) WRITE( 6, '(a)' ) 'ERF error in OVR_SRC_SNK_FRC_GET!' CALL GEOS_CHEM_STOP ENDIF ! Reset first-time flag FIRST = .FALSE. ENDIF ! Loop over source index (cf Zender et al eq 12) DO SRC_IDX = 1, SRC_NBR ! Fraction SQRT2LNGSDI = SQRT(2.0D0) * LOG( GSD_SRC(SRC_IDX) ) ! Loop over sink index DO SNK_IDX = 1, SNK_NBR ! [fraction] LNDMAXJOVRDMDNI = LOG(DMT_MAX_SNK(SNK_IDX)/MDN_SRC(SRC_IDX)) ! [fraction] LNDMINJOVRDMDNI = LOG(DMT_MIN_SNK(SNK_IDX)/MDN_SRC(SRC_IDX)) ! [fraction] OVR_SRC_SNK_FRC (SRC_IDX,SNK_IDX)= ! [frc] & 0.5D0 * (ERF(LNDMAXJOVRDMDNI/SQRT2LNGSDI) & - ERF(LNDMINJOVRDMDNI/SQRT2LNGSDI) ) ENDDO ENDDO ! Return to calling program END SUBROUTINE OVR_SRC_SNK_FRC_GET !------------------------------------------------------------------------------ FUNCTION ERF( X ) RESULT( ERF_VAL ) 6,1 ! !****************************************************************************** ! Function ERF returns the error function erf(x). See comments heading ! routine CALERF below. Author/Date: W. J. Cody, January 8, 1985 ! (tdf, bmy, 4/5/04) ! ! Arguments as Input: ! ============================================================================ ! (1 ) X (REAL*8) : Argument to erf(x) ! ! NOTES: ! (1 ) Updated comments (bmy, 4/5/04) !****************************************************************************** ! IMPLICIT NONE ! Arguments REAL*8, INTENT(IN) :: X ! Local variables INTEGER :: JINT REAL*8 :: RESULT, ERF_VAL !================================================================ ! ERF begins here! !================================================================ JINT = 0 CALL CALERF( X, RESULT, JINT ) ERF_VAL = RESULT ! Return to calling program END FUNCTION ERF !------------------------------------------------------------------------------ SUBROUTINE CALERF( ARG, RESULT, JINT ) 1 ! !****************************************************************************** ! This packet evaluates erf(x), erfc(x), and exp(x*x)*erfc(x) ! for a real argument x. It contains three function type ! subprograms: erf, erfc, and erfcx (or derf, derfc, and derfcx), ! and one subroutine type subprogram, calerf. The calling ! statements for the primary entries are: ! ! y=erf(x) (or y=derf(x)), ! y=erfc(x) (or y=derfc(x)), ! and ! y=erfcx(x) (or y=derfcx(x)). ! ! The routine calerf is intended for internal packet use only, ! all computations within the packet being concentrated in this ! routine. The function subprograms invoke calerf with the ! statement ! call calerf(arg,result,jint) ! where the parameter usage is as follows ! ! Function Parameters for calerf ! Call Arg Result Jint ! ! erf(arg) any real argument erf(arg) 0 ! erfc(arg) abs(arg) < xbig erfc(arg) 1 ! erfcx(arg) xneg < arg < xmax erfcx(arg) 2 ! ! The main computation evaluates near-minimax approximations: ! from "Rational Chebyshev Approximations for the Error Function" ! by W. J. Cody, Math. Comp., 1969, pp. 631-638. This ! transportable program uses rational functions that theoretically ! approximate erf(x) and erfc(x) to at least 18 significant ! decimal digits. The accuracy achieved depends on the arithmetic ! system, the compiler, the intrinsic functions, and proper ! selection of the machine-dependent constants. ! ! Explanation of machine-dependent constants: ! xmin = The smallest positive floating-point number. ! xinf = The largest positive finite floating-point number. ! xneg = The largest negative argument acceptable to erfcx; ! the negative of the solution to the equation ! 2*exp(x*x) = xinf. ! xsmall = Argument below which erf(x) may be represented by ! 2*x/sqrt(pi) and above which x*x will not underflow. ! A conservative value is the largest machine number x ! such that 1.0 + x = 1.0 to machine precision. ! xbig = Largest argument acceptable to erfc; solution to ! the equation: w(x)* (1-0.5/x**2) = xmin, where ! w(x) = exp(-x*x)/[x*sqrt(pi)]. ! xhuge = Argument above which 1.0 - 1/(2*x*x) = 1.0 to ! machine precision. a conservative value is ! 1/[2*sqrt(xsmall)] ! xmax = Largest acceptable argument to erfcx; the minimum ! of xinf and 1/[sqrt(pi)*xmin]. ! ! Approximate values for some important machines are: ! xmin xinf xneg xsmall ! CDC 7600 (s.p.) 3.13e-294 1.26e+322 -27.220 7.11e-15 ! Cray-1 (s.p.) 4.58e-2467 5.45e+2465 -75.345 7.11e-15 ! IEEE (IBM/XT, ! Sun, etc.) (s.p.) 1.18e-38 3.40e+38 -9.382 5.96e-8 ! IEEE (IBM/XT, ! Sun, etc.) (d.p.) 2.23d-308 1.79d+308 -26.628 1.11d-16 ! IBM 195 (d.p.) 5.40d-79 7.23e+75 -13.190 1.39d-17 ! Univac 1108 (d.p.) 2.78d-309 8.98d+307 -26.615 1.73d-18 ! Vax d-format (d.p.) 2.94d-39 1.70d+38 -9.345 1.39d-17 ! Vax g-format (d.p.) 5.56d-309 8.98d+307 -26.615 1.11d-16 ! ! xbig xhuge xmax ! CDC 7600 (s.p.) 25.922 8.39e+6 1.80x+293 ! Cray-1 (s.p.) 75.326 8.39e+6 5.45e+2465 ! IEEE (IBM/XT, ! Sun, etc.) (s.p.) 9.194 2.90e+3 4.79e+37 ! IEEE (IBM/XT, ! Sun, etc.) (d.p.) 26.543 6.71d+7 2.53d+307 ! IBM 195 (d.p.) 13.306 1.90d+8 7.23e+75 ! Univac 1108 (d.p.) 26.582 5.37d+8 8.98d+307 ! Vax d-format (d.p.) 9.269 1.90d+8 1.70d+38 ! Vax g-format (d.p.) 26.569 6.71d+7 8.98d+307 ! ! Error returns: ! The program returns erfc = 0 for arg >= xbig; ! erfcx = xinf for arg < xneg; ! and ! erfcx = 0 for arg >= xmax. ! ! Intrinsic functions required are: ! abs, aint, exp ! ! Author: W. J. Cody ! Mathematics And Computer Science Division ! Argonne National Laboratory ! Argonne, IL 60439 ! Latest modification: March 19, 1990 ! ! NOTES: ! (1 ) Now force double-precision w/ "D" exponents (bmy, 4/5/04) !****************************************************************************** ! IMPLICIT NONE INTEGER I,JINT REAL*8 A,ARG,B,C,D,DEL,FOUR,HALF,P,ONE,Q,RESULT,SIXTEN,SQRPI, & TWO,THRESH,X,XBIG,XDEN,XHUGE,XINF,XMAX,XNEG,XNUM,XSMALL, & Y,YSQ,ZERO DIMENSION A(5),B(4),C(9),D(8),P(6),Q(5) ! Mathematical constants data four,one,half,two,zero/4.0d0,1.0d0,0.5d0,2.0d0,0.0d0/, & sqrpi/5.6418958354775628695d-1/,thresh/0.46875d0/, & sixten/16.0d0/ ! Machine-dependent constants data xinf,xneg,xsmall/3.40d+38,-9.382d0,5.96d-8/, & xbig,xhuge,xmax/9.194d0,2.90d3,4.79d37/ ! Coefficients for approximation to erf in first interval data a /3.16112374387056560d00,1.13864154151050156d02, & 3.77485237685302021d02,3.20937758913846947d03, & 1.85777706184603153d-1/ data b /2.36012909523441209d01,2.44024637934444173d02, & 1.28261652607737228d03,2.84423683343917062d03/ ! Coefficients for approximation to erfc in second interval data c /5.64188496988670089d-1,8.88314979438837594d0, & 6.61191906371416295d01,2.98635138197400131d02, & 8.81952221241769090d02,1.71204761263407058d03, & 2.05107837782607147d03,1.23033935479799725d03, & 2.15311535474403846d-8/ data d /1.57449261107098347d01,1.17693950891312499d02, & 5.37181101862009858d02,1.62138957456669019d03, & 3.29079923573345963d03,4.36261909014324716d03, & 3.43936767414372164d03,1.23033935480374942d03/ ! Coefficients for approximation to erfc in third interval data p /3.05326634961232344d-1,3.60344899949804439d-1, & 1.25781726111229246d-1,1.60837851487422766d-2, & 6.58749161529837803d-4,1.63153871373020978d-2/ data q /2.56852019228982242d00,1.87295284992346047d00, & 5.27905102951428412d-1,6.05183413124413191d-2, & 2.33520497626869185d-3/ c Main Code x=arg y=abs(x) if (y <= thresh) then c Evaluate erf for |x| <= 0.46875 ysq=zero if (y > xsmall) ysq=y*y xnum=a(5)*ysq xden=ysq do i=1,3 xnum=(xnum+a(i))*ysq xden=(xden+b(i))*ysq end do result=x*(xnum+a(4))/(xden+b(4)) if (jint /= 0) result=one-result if (jint == 2) result=exp(ysq)*result go to 800 c Evaluate erfc for 0.46875 <= |x| <= 4.0 else if (y <= four) then xnum=c(9)*y xden=y do i=1,7 xnum=(xnum+c(i))*y xden=(xden+d(i))*y end do result=(xnum+c(8))/(xden+d(8)) if (jint /= 2) then ysq=aint(y*sixten)/sixten del=(y-ysq)*(y+ysq) result=exp(-ysq*ysq)*exp(-del)*result end if c Evaluate erfc for |x| > 4.0 else result=zero if (y >= xbig) then if ((jint /= 2).or.(y >= xmax)) go to 300 if (y >= xhuge) then result=sqrpi/y go to 300 end if end if ysq=one/(y*y) xnum=p(6)*ysq xden=ysq do i=1,4 xnum=(xnum+p(i))*ysq xden=(xden+q(i))*ysq end do result=ysq*(xnum+p(5))/(xden+q(5)) result=(sqrpi-result)/y if (jint /= 2) then ysq=aint(y*sixten)/sixten del=(y-ysq)*(y+ysq) result=exp(-ysq*ysq)*exp(-del)*result end if end if c Fix up for negative argument, erf, etc. 300 if (jint == 0) then result=(half-result)+half if (x < zero) result=-result else if (jint == 1) then if (x < zero) result=two-result else if (x < zero) then if (x < xneg) then result=xinf else ysq=aint(x*sixten)/sixten del=(x-ysq)*(x+ysq) y=exp(ysq*ysq)*exp(del) result=(y+y)-result end if end if end if 800 return ! Return to calling program END SUBROUTINE CALERF !------------------------------------------------------------------------------ SUBROUTINE PLN_TYP_GET( PLN_TYP, PLN_FRC, TAI ) 1 ! !****************************************************************************** ! Subroutine PLN_TYPE_GET returns LSM information needed by the DEAD ! dust parameterization. (tdf, bmy, 4/5/04) ! ! Arguments as Output: ! ============================================================================ ! (1 ) PLN_TYP (INTEGER) : LSM plant type index (1..14) ! (2 ) PLN_TYP (REAL*8 ) : Weight of corresponding plant type (sums to 1.0) ! (3 ) TAI (REAL*8 ) : Leaf-area index (one sided) [index] ! ! NOTES: ! (1 ) Updated comments. Now force double-precision w/ "D" exponents. ! (bmy, 4/5/04) !****************************************************************************** ! ! Arguments INTEGER, INTENT(OUT) :: PLN_TYP(0:28,3) REAL*8, INTENT(OUT) :: PLN_FRC(0:28,3) REAL*8, INTENT(OUT) :: TAI(14,12) ! Local variables INTEGER :: I, J !================================================================= ! There are 29 land surface types: 0 = ocean, 1 to 28 = land. ! Each land point has up to three vegetation types, ranging in ! value from 1 to 14. PLN_TYPE contains the vegetation type of ! the 3 subgrid points for each surface type. PLN_FRC contains ! the fractional area of the 3 subgrid points for each surface ! type. !================================================================= PLN_TYP(0:28,1) = (/ 0, & 14, 14, 1, 2, 4, 1 , 1, & 4, 1, 3, 5, 13, 1, 2, & 11, 11, 6, 13, 9, 7, 8, & 8, 12, 11, 12, 11, 3, 14/) PLN_FRC(0:28,1) = (/ 0.00d0, & 1.00d0, 1.00d0, 0.75d0, 0.50d0, & 0.75d0, 0.37d0, 0.75d0, & 0.75d0, 0.37d0, 0.95d0, 0.75d0, & 0.70d0, 0.25d0, 0.25d0, & 0.40d0, 0.40d0, 0.60d0, 0.60d0, & 0.30d0, 0.80d0, 0.80d0, & 0.10d0, 0.85d0, 0.85d0, 0.85d0, & 0.85d0, 0.80d0, 1.00d0/) PLN_TYP(0:28,2) = (/ 0, & 14, 14, 14, 14, 14, 4 ,14, & 14, 4, 14, 14, 5, 10, 10, & 4, 4, 13, 6, 10, 14, 14, & 14, 14, 14, 14, 14, 14, 14/) PLN_FRC(0:28,2) = (/ 0.00d0, & 0.00d0, 0.00d0, 0.25d0, 0.50d0, & 0.25d0, 0.37d0, 0.25d0, & 0.25d0, 0.37d0, 0.05d0, 0.25d0, & 0.30d0, 0.25d0, 0.25d0, & 0.30d0, 0.30d0, 0.20d0, 0.20d0, & 0.30d0, 0.20d0, 0.20d0, & 0.90d0, 0.15d0, 0.15d0, 0.15d0, & 0.15d0, 0.20d0, 0.00d0/) PLN_TYP(0:28,3) = (/ 0, & 14, 14, 14, 14, 14, 14, 14, & 14, 14, 14, 14, 14, 14, 14, & 1, 1, 14, 14, 14, 14, 14, & 14, 14, 14, 14, 14, 14, 14/) PLN_FRC(0:28,3) = (/ 0.00d0, & 0.00d0, 0.00d0, 0.00d0, 0.00d0, & 0.00d0, 0.26d0, 0.00d0, & 0.00d0, 0.26d0, 0.00d0, 0.00d0, & 0.00d0, 0.50d0, 0.50d0, & 0.30d0, 0.30d0, 0.20d0, 0.20d0, & 0.40d0, 0.00d0, 0.00d0, & 0.00d0, 0.00d0, 0.00d0, 0.00d0, & 0.00d0, 0.00d0, 0.00d0/) !================================================================= ! ---------------------------------------------------------------- ! description of the 29 surface types ! ---------------------------------------------------------------- ! ! no vegetation ! ------------- ! 0 ocean ! 1 land ice (glacier) ! 2 desert ! ! forest vegetation ! ----------------- ! 3 cool needleleaf evergreen tree ! 4 cool needleleaf deciduous tree ! 5 cool broadleaf deciduous tree ! 6 cool mixed needleleaf evergreen and broadleaf deciduous tree ! 7 warm needleleaf evergreen tree ! 8 warm broadleaf deciduous tree ! 9 warm mixed needleleaf evergreen and broadleaf deciduous tree ! 10 tropical broadleaf evergreen tree ! 11 tropical seasonal deciduous tree ! ! interrupted woods ! ---------------- ! 12 savanna ! 13 evergreen forest tundra ! 14 deciduous forest tundra ! 15 cool forest crop ! 16 warm forest crop ! ! non-woods ! --------- ! 17 cool grassland ! 18 warm grassland ! 19 tundra ! 20 evergreen shrub ! 21 deciduous shrub ! 22 semi-desert ! 23 cool irrigated crop ! 24 cool non-irrigated crop ! 25 warm irrigated crop ! 26 warm non-irrigated crop ! ! wetlands ! -------- ! 27 forest (mangrove) ! 28 non-forest ! ! ---------------------------------------------------------------- ! description of the 14 plant types. see vegconi.F for ! parameters that depend on vegetation type ! ---------------------------------------------------------------- ! ! 1 = needleleaf evergreen tree ! 2 = needleleaf deciduous tree ! 3 = broadleaf evergreen tree ! 4 = broadleaf deciduous tree ! 5 = tropical seasonal tree ! 6 = cool grass (c3) ! 7 = evergreen shrub ! 8 = deciduous shrub ! 9 = arctic deciduous shrub ! 10 = arctic grass ! 11 = crop ! 12 = irrigated crop ! 13 = warm grass (c4) ! 14 = not vegetated !================================================================= ! TAI = monthly leaf area index + stem area index, one-sided TAI(1,1:12) = (/ 4.5d0, 4.7d0, 5.0d0, 5.1d0, 5.3d0, 5.5d0, & 5.3d0, 5.3d0, 5.2d0, 4.9d0, 4.6d0, 4.5d0 /) TAI(2,1:12) = (/ 0.3d0, 0.3d0, 0.3d0, 1.0d0, 1.6d0, 2.4d0, & 4.3d0, 2.9d0, 2.0d0, 1.3d0, 0.8d0, 0.5d0 /) TAI(3,1:12) = (/ 5.0d0, 5.0d0, 5.0d0, 5.0d0, 5.0d0, 5.0d0, & 5.0d0, 5.0d0, 5.0d0, 5.0d0, 5.0d0, 5.0d0 /) TAI(4,1:12) = (/ 0.4d0, 0.4d0, 0.7d0, 1.6d0, 3.5d0, 5.1d0, & 5.4d0, 4.8d0, 3.8d0, 1.7d0, 0.6d0, 0.4d0 /) TAI(5,1:12) = (/ 1.2d0, 1.0d0, 0.9d0, 0.8d0, 0.8d0, 1.0d0, & 2.0d0, 3.7d0, 3.2d0, 2.7d0, 1.9d0, 1.2d0 /) TAI(6,1:12) = (/ 0.7d0, 0.8d0, 0.9d0, 1.0d0, 1.5d0, 3.4d0, & 4.3d0, 3.8d0, 1.8d0, 1.0d0, 0.9d0, 0.8d0 /) TAI(7,1:12) = (/ 1.3d0, 1.3d0, 1.3d0, 1.3d0, 1.3d0, 1.3d0, & 1.3d0, 1.3d0, 1.3d0, 1.3d0, 1.3d0, 1.3d0 /) TAI(8,1:12) = (/ 1.0d0, 1.0d0, 0.8d0, 0.3d0, 0.6d0, 0.0d0, & 0.1d0, 0.3d0, 0.5d0, 0.6d0, 0.7d0, 0.9d0 /) TAI(9,1:12) = (/ 0.1d0, 0.1d0, 0.1d0, 0.1d0, 0.1d0, 0.3d0, & 1.5d0, 1.7d0, 1.4d0, 0.1d0, 0.1d0, 0.1d0 /) TAI(10,1:12) = (/ 0.7d0, 0.8d0, 0.9d0, 1.0d0, 1.5d0, 3.4d0, & 4.3d0, 3.8d0, 1.8d0, 1.0d0, 0.9d0, 0.8d0 /) TAI(11,1:12) = (/ 0.0d0, 0.0d0, 0.0d0, 0.0d0, 1.0d0, 2.0d0, & 3.0d0, 3.0d0, 1.5d0, 0.0d0, 0.0d0, 0.0d0 /) TAI(12,1:12) = (/ 0.0d0, 0.0d0, 0.0d0, 0.0d0, 1.0d0, 2.0d0, & 3.0d0, 3.0d0, 1.5d0, 0.0d0, 0.0d0, 0.0d0 /) TAI(13,1:12) = (/ 0.7d0, 0.8d0, 0.9d0, 1.0d0, 1.5d0, 3.4d0, & 4.3d0, 3.8d0, 1.8d0, 1.0d0, 0.9d0, 0.8d0 /) TAI(14,1:12) = (/ 0.0d0, 0.0d0, 0.0d0, 0.0d0, 0.0d0, 0.0d0, & 0.0d0, 0.0d0, 0.0d0, 0.0d0, 0.0d0, 0.0d0 /) ! Return to calling program END SUBROUTINE PLN_TYP_GET !------------------------------------------------------------------------------ SUBROUTINE GET_TIME_INVARIANT_DATA 1,32 ! !****************************************************************************** ! Subroutine GET_TIME_INVARIANT_DATA gets data for the DEAD model which ! does not vary w/ time. This routine is called from SRC_DUST_DEAD in ! "dust_mod.f" only on the first timestep. (bmy, 4/5/04, 1/25/07) ! ! NOTES: ! (1 ) Now reference DATA_DIR from "directory_mod.f" (bmy, 7/20/04) ! (2 ) Now can read data for both GEOS & GCAP grids (bmy, 8/16/05) ! (3 ) Now make sure all USE statements are USE, ONLY (bmy, 10/3/05) ! (4 ) Now references "file_mod.f", "transfer_mod.f". Also now read from ! dust_200605 directory. Now reads GOCART source function from a ! separate file. (tdf, bmy, 1/25/07) !****************************************************************************** ! ! References to F90 modules USE BPCH2_MOD, ONLY : GET_NAME_EXT_2D, GET_RES_EXT USE BPCH2_MOD, ONLY : GET_TAU0, READ_BPCH2 USE DIRECTORY_MOD, ONLY : DATA_DIR USE FILE_MOD, ONLY : IOERROR USE TRANSFER_MOD, ONLY : TRANSFER_2D # include "CMN_SIZE" ! Size parameters ! Local variables INTEGER :: I, IOS REAL*4 :: ARRAY(IGLOB,JGLOB,1) REAL*8 :: XTAU CHARACTER(LEN=255) :: FILENAME !================================================================= ! GET_TIME_INVARIANT_DATA begins here! !================================================================= ! Initialize data arrays CALL INIT_DUST_DEAD !================================================================= ! Compute mass overlaps, Mij, between "source" PDFs ! and size bins (Zender et al., 2K3, Equ. 12, and Table 1) !================================================================= CALL OVR_SRC_SNK_FRC_GET( DST_SRC_NBR, DMT_VMA_SRC, & GSD_ANL_SRC, NDSTBIN, & DMT_MIN, DMT_MAX, & OVR_SRC_SNK_FRC ) !================================================================= ! Compute OVR_SRC_SNK_MSS, the fraction of dust transported, given ! the mass overlap, OVR_SRC_SNK_FRC, and the mass fraction ! MSS_FRC_SRC. OVR_SRC_SNK_MSS is used in routine ! FLX_MSS_VRT_DST_PRT which partitions the total vertical ! dust flux into transport !============================================================== CALL DST_PSD_MSS( OVR_SRC_SNK_FRC, MSS_FRC_SRC, & OVR_SRC_SNK_MSS, NDSTBIN, DST_SRC_NBR ) !================================================================= ! Get plant type, cover, and Leaf area index from land sfc model !================================================================= CALL PLN_TYP_GET( PLN_TYP, PLN_FRC, TAI ) !================================================================= ! Need also to provide surface boundary information here ! read time-invariant boundary fields data set (labelled 1,1,1985) ! ! The following time-invariant fields are read in ! ERD_FCT_GEO ; geomorphic erodibility: IIPAR JJPAR ! ERD_FCT_HYDRO ; hydrologic erodibility: IIPAR JJPAR ! ERD_FCT_TOPO ; topog. erodibility (Ginoux): IIPAR JJPAR ! ERD_FCT_UNITY ; uniform erodibility: IIPAR JJPAR ! MBL_BSN_FCT ; overall erodibility factor : IIPAR JJPAR ! ! Erodibility field should be copied onto mbl_bsn_fct ! which is the one used by the DEAD code Duncan 8/1/2003 ! ! LND_FRC_DRY ; dry land fraction: IIPAR JJPAR ! MSS_FRC_CACO3 ; mass fraction of soil CaCO3: IIPAR JJPAR ! MSS_FRC_CLY ; mass fraction of clay: IIPAR JJPAR ! MSS_FRC_SND ; mass fraction of sand: IIPAR JJPAR ! SFC_TYP ; surface type: IIPAR JJPAR !================================================================= ! Filename FILENAME = TRIM( DATA_DIR ) // & 'dust_200605/dst_tibds.' // GET_NAME_EXT_2D() // & '.' // GET_RES_EXT() ! TAU value for reading the bpch files XTAU = GET_TAU0( 1, 1, 1985 ) ! Echo info WRITE( 6, 100 ) TRIM( FILENAME ) 100 FORMAT( ' - GET_TIME_INVARIANT_DATA: Reading ', a ) !----------------- ! ERD_FCT_GEO !----------------- CALL READ_BPCH2( FILENAME, 'DEAD-2D', 1, & XTAU, IGLOB, JGLOB, & 1, ARRAY, QUIET=.TRUE. ) CALL TRANSFER_2D( ARRAY(:,:,1), ERD_FCT_GEO ) !----------------- ! ERD_FCT_HYDRO !----------------- CALL READ_BPCH2( FILENAME, 'DEAD-2D', 2, & XTAU, IGLOB, JGLOB, & 1, ARRAY, QUIET=.TRUE. ) CALL TRANSFER_2D( ARRAY(:,:,1), ERD_FCT_HYDRO ) !----------------- ! ERD_FCT_TOPO !----------------- CALL READ_BPCH2( FILENAME, 'DEAD-2D', 3, & XTAU, IGLOB, JGLOB, & 1, ARRAY, QUIET=.TRUE. ) CALL TRANSFER_2D( ARRAY(:,:,1), ERD_FCT_TOPO ) !----------------- ! ERD_FCT_UNITY !----------------- CALL READ_BPCH2( FILENAME, 'DEAD-2D', 4, & XTAU, IGLOB, JGLOB, & 1, ARRAY, QUIET=.TRUE. ) CALL TRANSFER_2D( ARRAY(:,:,1), ERD_FCT_UNITY ) !----------------- ! MBL_BSN_FCT !----------------- !----------------------------------------------------------------------------- ! To read MBL_BSN_FCT, uncomment these lines: ! CALL READ_BPCH2( FILENAME, 'DEAD-2D', 5, ! & XTAU, IGLOB, JGLOB, ! & 1, ARRAY, QUIET=.TRUE. ) ! ! CALL TRANSFER_2D( ARRAY(:,:,1), MBL_BSN_FCT ) !----------------------------------------------------------------------------- ! ??? Is this correct (bmy, 4/9/04) ! ! Set erodibility to a global uniform value of 5.707 ! as recommended by Zender et al 2003 (tdf, 4/9/04) MBL_BSN_FCT(:,:) = 1.0d0 !----------------- ! LND_FRC_DRY !----------------- CALL READ_BPCH2( FILENAME, 'DEAD-2D', 6, & XTAU, IGLOB, JGLOB, & 1, ARRAY, QUIET=.TRUE. ) CALL TRANSFER_2D( ARRAY(:,:,1), LND_FRC_DRY ) !----------------- ! MSS_FRC_CACO3 !----------------- CALL READ_BPCH2( FILENAME, 'DEAD-2D', 7, & XTAU, IGLOB, JGLOB, & 1, ARRAY, QUIET=.TRUE. ) CALL TRANSFER_2D( ARRAY(:,:,1), MSS_FRC_CACO3 ) !----------------- ! MSS_FRC_CLY !----------------- CALL READ_BPCH2( FILENAME, 'DEAD-2D', 8, & XTAU, IGLOB, JGLOB, & 1, ARRAY, QUIET=.TRUE. ) CALL TRANSFER_2D( ARRAY(:,:,1), MSS_FRC_CLY ) !----------------- ! MSS_FRC_SND !----------------- CALL READ_BPCH2( FILENAME, 'DEAD-2D', 9, & XTAU, IGLOB, JGLOB, & 1, ARRAY, QUIET=.TRUE. ) CALL TRANSFER_2D( ARRAY(:,:,1), MSS_FRC_SND ) !----------------- ! SFC_TYP !----------------- CALL READ_BPCH2( FILENAME, 'DEAD-2D', 10, & XTAU, IGLOB, JGLOB, & 1, ARRAY, QUIET=.TRUE. ) ! NINT is not defined for REAL*8 !CALL TRANSFER_2D( ARRAY(:,:,1), SFC_TYP ) ! Also round off SFC_TYP = NINT( ARRAY(:,:,1) ) !------------------------ ! GOCART source function ! (tdf, bmy, 1/25/07) !------------------------ ! File name FILENAME = TRIM( DATA_DIR ) // & 'dust_200605/GOCART_src_fn.' // GET_NAME_EXT_2D() // & '.' // GET_RES_EXT() ! Echo info WRITE( 6, 100 ) TRIM( FILENAME ) ! Read data CALL READ_BPCH2( FILENAME, 'DEAD-2D', 14, & XTAU, IGLOB, JGLOB, & 1, ARRAY, QUIET=.TRUE. ) ! Cast to REAL*8 CALL TRANSFER_2D( ARRAY(:,:,1), SRCE_FUNC ) ! Return to calling program END SUBROUTINE GET_TIME_INVARIANT_DATA !------------------------------------------------------------------------------ SUBROUTINE GET_MONTHLY_DATA 1,10 ! !****************************************************************************** ! Subroutine GET_MONTHLY_DATA gets data for the DEAD model which varies by ! month. This routine is called from SRC_DUST_DEAD in "dust_mod.f". ! (tdf, bmy, 4/5/04, 1/25/07) ! ! NOTES: ! (1 ) Now reference DATA_DIR from "directory_mod.f" (bmy, 7/20/04) ! (2 ) Now can read data for both GEOS & GCAP grids (bmy, 8/16/05) ! (3 ) Now make sure all USE statements are USE, ONLY (bmy, 10/3/05) ! (4 ) Now read from dust_200605 directory (tdf, bmy, 1/25/07) !****************************************************************************** ! ! References to F90 modules USE BPCH2_MOD, ONLY : GET_NAME_EXT_2D, GET_RES_EXT USE BPCH2_MOD, ONLY : GET_TAU0, READ_BPCH2 USE DIRECTORY_MOD, ONLY : DATA_DIR USE TIME_MOD, ONLY : GET_MONTH, ITS_A_NEW_MONTH USE TRANSFER_MOD, ONLY : TRANSFER_2D # include "CMN_SIZE" ! Size parameters ! Local variables INTEGER :: THISMONTH REAL*4 :: ARRAY(IGLOB,JGLOB,1) REAL*8 :: XTAU CHARACTER(LEN=255) :: FILENAME !================================================================= ! GET_MONTHLY_DATA begins here! !================================================================= ! Filename and time FILENAME = TRIM( DATA_DIR ) // & 'dust_200605/dst_tvbds.' // GET_NAME_EXT_2D() // & '.' // GET_RES_EXT() ! TAU for reading the bpch files THISMONTH = GET_MONTH() XTAU = GET_TAU0( THISMONTH, 1, 1985 ) ! Echo info WRITE( 6, 100 ) TRIM( FILENAME ) 100 FORMAT( ' - GET_MONTHLY_DATA: Reading ', a ) !----------------------- ! Veg. Area Index (VAI) !----------------------- CALL READ_BPCH2( FILENAME, 'DEAD-2D', 13, & XTAU, IGLOB, JGLOB, & 1, ARRAY, QUIET=.TRUE. ) ! Cast to REAL*8 and resize CALL TRANSFER_2D( ARRAY(:,:,1), VAI_DST ) ! Return to calling program END SUBROUTINE GET_MONTHLY_DATA !------------------------------------------------------------------------------ SUBROUTINE INIT_DUST_DEAD 1,32 ! !****************************************************************************** ! Subroutine INIT_DUST_DEAD initializes all allocatable module arrays. ! (tdf, bmy, 3/30/04, 1/25/07) ! ! NOTES: ! (1 ) Now allocate SRCE_FUNC (tdf, bmy, 1/25/07) !****************************************************************************** ! ! References to F90 modules USE ERROR_MOD, ONLY : ALLOC_ERR # include "CMN_SIZE" ! Local variables INTEGER :: AS !================================================================= ! INIT_DUST_DEAD begins here! !================================================================= ALLOCATE( ERD_FCT_GEO( IIPAR, JJPAR ), STAT=AS ) IF ( AS /= 0 ) CALL ALLOC_ERR( 'ERD_FCT_GEO' ) ERD_FCT_GEO = 0d0 ALLOCATE( ERD_FCT_HYDRO( IIPAR, JJPAR ), STAT=AS ) IF ( AS /= 0 ) CALL ALLOC_ERR( 'ERD_FCT_HYDRO' ) ERD_FCT_HYDRO = 0d0 ALLOCATE( ERD_FCT_TOPO( IIPAR, JJPAR ), STAT=AS ) IF ( AS /= 0 ) CALL ALLOC_ERR( 'ERD_FCT_TOPO' ) ERD_FCT_TOPO = 0d0 ALLOCATE( ERD_FCT_UNITY( IIPAR, JJPAR ), STAT=AS ) IF ( AS /= 0 ) CALL ALLOC_ERR( 'ERD_FCT_UNITY' ) ERD_FCT_UNITY = 0d0 ALLOCATE( MBL_BSN_FCT( IIPAR, JJPAR), STAT=AS ) IF ( AS /= 0 ) CALL ALLOC_ERR( 'MBL_BSN_FCT' ) MBL_BSN_FCT = 0d0 ALLOCATE( LND_FRC_DRY( IIPAR, JJPAR ), STAT=AS ) IF ( AS /= 0 ) CALL ALLOC_ERR( 'LND_FRC_DRY' ) LND_FRC_DRY = 0d0 ALLOCATE( MSS_FRC_CACO3( IIPAR, JJPAR ), STAT=AS ) IF ( AS /= 0 ) CALL ALLOC_ERR( 'MSS_FRC_CACO3' ) MSS_FRC_CACO3 = 0d0 ALLOCATE( MSS_FRC_CLY( IIPAR, JJPAR ), STAT=AS ) IF ( AS /= 0 ) CALL ALLOC_ERR( 'MSS_FRC_CLY' ) MSS_FRC_CLY = 0d0 ALLOCATE( MSS_FRC_SND( IIPAR, JJPAR ), STAT=AS ) IF ( AS /= 0 ) CALL ALLOC_ERR( 'MSS_FRC_SND' ) MSS_FRC_SND = 0d0 ALLOCATE( SFC_TYP( IIPAR, JJPAR ), STAT=AS ) IF ( AS /= 0 ) CALL ALLOC_ERR( 'SFC_TYP' ) SFC_TYP = 0d0 ALLOCATE( FLX_LW_DWN_SFC( IIPAR, JJPAR ), STAT=AS ) IF ( AS /= 0 ) CALL ALLOC_ERR( 'FLX_LW_DWN_SFC' ) FLX_LW_DWN_SFC = 0d0 ALLOCATE( FLX_SW_ABS_SFC( IIPAR, JJPAR ), STAT=AS ) IF ( AS /= 0 ) CALL ALLOC_ERR( 'FLX_SW_ABS_SFC' ) FLX_SW_ABS_SFC = 0d0 ALLOCATE( TPT_GND( IIPAR, JJPAR ), STAT=AS ) IF ( AS /= 0 ) CALL ALLOC_ERR( 'TPT_GND' ) TPT_GND = 0d0 ALLOCATE( TPT_SOI( IIPAR, JJPAR ), STAT=AS ) IF ( AS /= 0 ) CALL ALLOC_ERR( 'TPT_SOI' ) TPT_SOI = 0d0 ALLOCATE( VWC_SFC( IIPAR, JJPAR ), STAT=AS ) IF ( AS /= 0 ) CALL ALLOC_ERR( 'VWC_SFC' ) VWC_SFC = 0d0 ALLOCATE( VAI_DST( IIPAR, JJPAR ), STAT=AS ) IF ( AS /= 0 ) CALL ALLOC_ERR( 'VAI_DST' ) VAI_DST = 0d0 ALLOCATE( SRC_STR( IIPAR, JJPAR ), STAT=AS ) IF ( AS /= 0 ) CALL ALLOC_ERR( 'SRC_STR' ) SRC_STR = 0d0 ! (tdf, bmy, 1/25/07) ALLOCATE( SRCE_FUNC( IIPAR, JJPAR ), STAT=AS ) IF ( AS /= 0 ) CALL ALLOC_ERR( 'SRCE_FUNC' ) SRCE_FUNC = 0d0 ALLOCATE( PLN_TYP( 0:28, 3 ), STAT=AS ) IF ( AS /= 0 ) CALL ALLOC_ERR( 'PLN_TYP' ) PLN_TYP = 0 ALLOCATE( PLN_FRC( 0:28, 3 ), STAT=AS ) IF ( AS /= 0 ) CALL ALLOC_ERR( 'PLN_FRC' ) PLN_FRC = 0d0 ALLOCATE( TAI( MVT, 12 ), STAT=AS ) IF ( AS /= 0 ) CALL ALLOC_ERR( 'TAI' ) TAI = 0d0 ALLOCATE( DMT_VWR( NDSTBIN ), STAT=AS ) IF ( AS /= 0 ) CALL ALLOC_ERR( 'DMT_VWR' ) DMT_VWR = 0d0 ALLOCATE( DNS_AER( NDSTBIN ), STAT=AS ) IF ( AS /= 0 ) CALL ALLOC_ERR( 'DNS_AER' ) DNS_AER = 0d0 ALLOCATE( OVR_SRC_SNK_FRC( DST_SRC_NBR, NDSTBIN ), STAT=AS ) IF ( AS /= 0 ) CALL ALLOC_ERR( 'OVR_SRC_SNK_FRC' ) OVR_SRC_SNK_FRC = 0d0 ALLOCATE( OVR_SRC_SNK_MSS( DST_SRC_NBR, NDSTBIN ), STAT=AS ) IF ( AS /= 0 ) CALL ALLOC_ERR( 'OVR_SRC_SNK_MSS' ) OVR_SRC_SNK_MSS = 0d0 ALLOCATE( OROGRAPHY( IIPAR, JJPAR ), STAT=AS ) IF ( AS /= 0 ) CALL ALLOC_ERR( 'OROGRAPHY' ) OROGRAPHY = 0 ! Bin size min diameter [m] ALLOCATE( DMT_MIN( NDSTBIN ), STAT=AS ) IF ( AS /= 0 ) CALL ALLOC_ERR( 'DMT_MIN' ) DMT_MIN(1) = 0.2d-6 DMT_MIN(2) = 2.0d-6 DMT_MIN(3) = 3.6d-6 DMT_MIN(4) = 6.0d-6 ! Bin size max diameter [m] ALLOCATE( DMT_MAX( NDSTBIN ), STAT=AS ) IF ( AS /= 0 ) CALL ALLOC_ERR( 'DMT_MAX' ) DMT_MAX(1) = 2.0d-6 DMT_MAX(2) = 3.6d-6 DMT_MAX(3) = 6.0d-6 DMT_MAX(4) = 1.2d-5 ! DMT_VMA_SRC: D'Almeida's (1987) "Background" modes ! as default [m] (Zender et al. p.5 Table 1) ! These modes also summarized in BSM96 p. 73 Table 2 ! Mass median diameter BSM96 p. 73 Table 2 ALLOCATE( DMT_VMA_SRC( DST_SRC_NBR ), STAT=AS ) IF ( AS /= 0 ) CALL ALLOC_ERR( 'DMT_VMA_SRC' ) DMT_VMA_SRC(1) = 0.832d-6 DMT_VMA_SRC(2) = 4.82d-6 DMT_VMA_SRC(3) = 19.38d-6 ! GSD_ANL_SRC: Geometric standard deviation [fraction] ! BSM96 p. 73 Table 2 ALLOCATE( GSD_ANL_SRC( DST_SRC_NBR ), STAT=AS ) IF ( AS /= 0 ) CALL ALLOC_ERR( 'GSD_ANL_SRC' ) GSD_ANL_SRC(1) = 2.10d0 GSD_ANL_SRC(2) = 1.90d0 GSD_ANL_SRC(3) = 1.60d0 ! MSS_FRC_SRC: Mass fraction BSM96 p. 73 Table 2 ALLOCATE( MSS_FRC_SRC( DST_SRC_NBR ), STAT=AS ) IF ( AS /= 0 ) CALL ALLOC_ERR( 'MSS_FRC_SRC' ) MSS_FRC_SRC(1) = 0.036d0 MSS_FRC_SRC(2) = 0.957d0 MSS_FRC_SRC(3) = 0.007d0 ! Return to calling program END SUBROUTINE INIT_DUST_DEAD !------------------------------------------------------------------------------ SUBROUTINE CLEANUP_DUST_DEAD 1 ! !****************************************************************************** ! Subroutine CLEANUP_DUST_DEAD deallocates all module variables. ! (tdf, bmy, 3/30/04, 1/25/07) ! ! NOTES: ! (1 ) Now deallocate SRCE_FUNC (tdf, bmy, 1/25/07) !****************************************************************************** ! !================================================================= ! CLEANUP_DUST_DEAD begins here! !================================================================= IF ( ALLOCATED( ERD_FCT_GEO ) ) DEALLOCATE( ERD_FCT_GEO ) IF ( ALLOCATED( ERD_FCT_HYDRO ) ) DEALLOCATE( ERD_FCT_HYDRO ) IF ( ALLOCATED( ERD_FCT_TOPO ) ) DEALLOCATE( ERD_FCT_TOPO ) IF ( ALLOCATED( ERD_FCT_UNITY ) ) DEALLOCATE( ERD_FCT_UNITY ) IF ( ALLOCATED( MBL_BSN_FCT ) ) DEALLOCATE( MBL_BSN_FCT ) IF ( ALLOCATED( LND_FRC_DRY ) ) DEALLOCATE( LND_FRC_DRY ) IF ( ALLOCATED( MSS_FRC_CACO3 ) ) DEALLOCATE( MSS_FRC_CACO3 ) IF ( ALLOCATED( MSS_FRC_CLY ) ) DEALLOCATE( MSS_FRC_CLY ) IF ( ALLOCATED( MSS_FRC_SND ) ) DEALLOCATE( MSS_FRC_SND ) IF ( ALLOCATED( SFC_TYP ) ) DEALLOCATE( SFC_TYP ) IF ( ALLOCATED( FLX_LW_DWN_SFC ) ) DEALLOCATE( FLX_LW_DWN_SFC ) IF ( ALLOCATED( FLX_SW_ABS_SFC ) ) DEALLOCATE( FLX_SW_ABS_SFC ) IF ( ALLOCATED( TPT_GND ) ) DEALLOCATE( TPT_GND ) IF ( ALLOCATED( TPT_SOI ) ) DEALLOCATE( TPT_SOI ) IF ( ALLOCATED( VWC_SFC ) ) DEALLOCATE( VWC_SFC ) IF ( ALLOCATED( VAI_DST ) ) DEALLOCATE( VAI_DST ) IF ( ALLOCATED( SRC_STR ) ) DEALLOCATE( SRC_STR ) IF ( ALLOCATED( PLN_TYP ) ) DEALLOCATE( PLN_TYP ) IF ( ALLOCATED( PLN_FRC ) ) DEALLOCATE( PLN_FRC ) IF ( ALLOCATED( TAI ) ) DEALLOCATE( TAI ) IF ( ALLOCATED( DMT_VWR ) ) DEALLOCATE( DMT_VWR ) IF ( ALLOCATED( DNS_AER ) ) DEALLOCATE( DNS_AER ) IF ( ALLOCATED( OVR_SRC_SNK_FRC ) ) DEALLOCATE( OVR_SRC_SNK_FRC ) IF ( ALLOCATED( OVR_SRC_SNK_MSS ) ) DEALLOCATE( OVR_SRC_SNK_MSS ) IF ( ALLOCATED( OROGRAPHY ) ) DEALLOCATE( OROGRAPHY ) IF ( ALLOCATED( DMT_MIN ) ) DEALLOCATE( DMT_MIN ) IF ( ALLOCATED( DMT_MAX ) ) DEALLOCATE( DMT_MAX ) IF ( ALLOCATED( DMT_VMA_SRC ) ) DEALLOCATE( DMT_VMA_SRC ) IF ( ALLOCATED( GSD_ANL_SRC ) ) DEALLOCATE( GSD_ANL_SRC ) IF ( ALLOCATED( MSS_FRC_SRC ) ) DEALLOCATE( MSS_FRC_SRC ) IF ( ALLOCATED( SRCE_FUNC ) ) DEALLOCATE( SRCE_FUNC ) ! Return to calling program END SUBROUTINE CLEANUP_DUST_DEAD !------------------------------------------------------------------------------ END MODULE DUST_DEAD_MOD