United Kingdom Meteorological Office (UKMO): References


[1]Cullen, M.J.P., 1993: The Unified Forecast/Climate Model. Meteor. Mag., 122, 81-94.

[2]Slingo, A. (ed.), 1985: Handbook of the Meteorological Office 11-layer atmospheric general circulation model. Vol. 1: Model description. DCTN 29, United Kingdom Meteorological Office, Bracknell, Berkshire RG12 2SZ, UK.

[3]Cullen, M.J.P., 1991: Positive definite advection scheme. Unified Model Documentation Paper No. 11, United Kingdom Meteorological Office, Bracknell, Berkshire RG12 2SZ, UK.

[4]Cullen, M.J.P., T. Davies, and M.H. Mawson, 1991: Conservative finite difference schemes for a Unified Forecast/Climate Model. Unified Model Documentation Paper No. 10, United Kingdom Meteorological Office, Bracknell, Berkshire RG12 2SZ, UK.

[5]Ingram, W.J., 1993: Radiation, version 1. Unified Model Documentation Paper No. 23, United Kingdom Meteorological Office, Bracknell, Berkshire RG12 2SZ, UK.

[6]Gregory, D., 1990: Convection scheme. Unified Model Documentation Paper No. 27, United Kingdom Meteorological Office, Bracknell, Berkshire RG12 2SZ, UK.

[7]Gregory, D., and R.N.B. Smith, 1990: Canopy, surface, and soil hydrology. Unified Model Documentation Paper No. 25, United Kingdom Meteorological Office, Bracknell, Berkshire RG12 2SZ, UK.

[8]Smith, R.N.B., 1993: Experience and developments with the layer cloud and boundary layer mixing schemes in the UK Meteorological Office Unified Model. In Proceedings of the ECMWF/GCSS Workshop on Parameterisation of the Cloud-Topped Boundary Layer, 8-11 June 1993, European Centre for Medium-Range Weather Forecasts, Reading, England.

[9]Smith, R.N.B., and D. Gregory, 1990: Large-scale precipitation. Unified Model Documentation Paper No. 26, United Kingdom Meteorological Office, Bracknell, Berkshire RG12 2SZ, UK.

[10]Wilson, C.A., 1989: Vertical diffusion. Unified Model Documentation Paper No. 21, United Kingdom Meteorological Office, Bracknell, Berkshire RG12 2SZ, UK.

[11]Wilson, C.A., and R. Swinbank, 1989: Gravity wave drag. Unified Model Documentation Paper No. 22, United Kingdom Meteorological Office, Bracknell, Berkshire RG12 2SZ, UK.

[12]Arakawa, A., and V.R. Lamb, 1977: Computational design of the basic dynamical processes of the UCLA general circulation model. In Methods in Computational Physics, 17, J. Chang (ed.), Academic Press, New York, 173-265.

[13]Bell, R.S., and A. Dickinson, 1987: The Meteorological Office operational numerical weather prediction system. Met. Office Sci. Paper No. 41, United Kingdom Meteorological Office, Bracknell, Berkshire RG12 2SZ, UK.

[14]Simmons, A.J., and R. Strüfing, 1981: An energy and angular-momentum conserving finite difference scheme, hybrid coordinates and medium-range weather prediction. ECMWF Tech. Report No. 28, European Centre for Medium-Range Weather Forecasts, Reading, England, 68 pp.

[15]White, A.A., and R.A. Bromley, 1988: A new set of dynamical equations for use in numerical weather prediction and global climate models. Met. Off. 13 Branch Memo., United Kingdom Meteorological Office, Bracknell, Berkshire RG12 2SZ, UK.

[16]Smith, R.N.B., 1990b: Subsurface, surface, and boundary layer processes. Unified Model Documentation Paper No. 24, United Kingdom Meteorological Office, Bracknell, Berkshire RG12 2SZ, UK.

[17]Palmer, T.N., G.J. Shutts, R. Swinbank, 1986: Alleviation of a systematic westerly bias in general circulation and numerical weather prediction models through an orographic gravity wave drag parameterization. Quart. J. Roy. Meteor. Soc., 112, 1001-1039.

[18]Keating, G.M., D.F. Young, and M.C. Pitts, 1987: Ozone reference models for CIRA. Adv. Space Res., 7, 105-115.

[19]McPeters, R.D., D.F. Heath, and P.K. Bhartia, 1984: Averaged ozone profiles for 1979 from the NIMBUS 7 SBUV instrument. J. Geophys. Res., 89, 5199-5214.

[20]Slingo, A., 1989: A GCM parameterization for the shortwave radiative properties of water clouds. J. Atmos. Sci., 46, 1419-1427.

[21]Slingo, A., and R.C. Wilderspin, 1986: Development of a revised longwave radiation scheme for an atmospheric general circulation model. Quart. J. Roy. Meteor. Soc., 112, 371-386.

[22]Roberts, R.E., J.A. Selby, and L.M. Biberman, 1976: Infrared continuum absorption by atmospheric water vapor in the 8-12 micron window. Appl. Optics, 15, 2085-2090.

[23]Geleyn, J.-F., and A. Hollingsworth, 1979: An economical analytical method for the computation of the interaction between scattering and line absorption of radiation. Beitr. Phys. Atmos., 52, 1-16.

[24]Zdunkowski, W.G., R.M. Welch, G. Korb, 1980: An investigation of the structure of typical two-stream methods for the calculation of solar fluxes and heating rates in clouds. Beitr. Phys. Atm., 53, 147-166.

[25]Yanai, M., S. Esbensen, and J.-H., Chu, 1973: Determination of bulk properties of tropical cloud clusters from large-scale heat and moisture budgets. J. Atmos. Sci., 30, 611-627.

[26]Gregory, D., and P.R.R. Rowntree, 1990: A mass flux convection scheme with representation of cloud ensemble characteristics and stability dependent closure. Mon. Wea. Rev., 118, 1483-1506.

[27]Smith, R.N.B., 1990a: A scheme for predicting layer clouds and their water content in a general circulation model. Quart. J. Roy. Meteor. Soc., 116, 435-460.

[28]Sundqvist, H., 1978: A parameterization scheme for non-convective condensation including prediction of cloud water content. Quart. J. Roy. Meteor. Soc., 104, 677-690.

[29]Sundqvist, H., 1981: Prediction of stratiform clouds: Results from a 5-day forecast with a global model. Tellus, 33, 242-253.

[30]Golding, B.W., 1986: Short range forecasting over the United Kingdom using a mesoscale forecasting system. Short- and Medium-Range Numerical Weather Prediction (Special Volume of J. Meteor. Soc. Japan), T. Matsuno (ed.), 563-572.

[31]Heymsfield, A.J., 1977: Precipitation development in stratiform ice clouds: A microphysical and dynamical study. J. Atmos. Sci., 34, 367-381.

[32]Kessler, E., 1969: On the distribution and continuity of water substance in atmospheric circulation. Meteorological Monographs, 10, American Meteorological Society, Boston, MA.

[33]Lin, Y.-L., R.D. Farley, and H.D. Orville, 1983: Bulk parameterization of the snowfield in a cloud model. J. Clim. Appl. Meteor., 22, 1065-1092.

[34]Dolman, A.J., and D. Gregory, 1992: The parameterization of rainfall interception in GCMs. Quart. J. Roy. Meteor. Soc.,118, 455-467.

[35]Joseph, D., 1980: Navy 10' global elevation values. National Center for Atmospheric Research notes on the FNWC terrain data set, National Center for Atmospheric Research, Boulder, CO, 3 pp.

[36]Semtner, A.J., 1976: A model for the thermodynamic growth of sea ice in numerical investigations of climate. J. Phys. Oceanogr., 6, 379-389.

[37]Wilson, M.F., and A. Henderson-Sellers, 1985: A global archive of land cover and soils data sets for use in general circulation models Int. J. Climatology, 5, 119-143.

[38]Buckley, E., and D.A. Warrilow, 1988: Derivation of land surface parameter datasets for use in the Met O 20 GCM. Met. O 20 Internal Note No. 81, United Kingdom Meteorological Office, Bracknell, Berkshire RG12 2SZ, UK.

[39]Charnock, H., 1955: Wind stress on a water surface. Quart. J. Roy. Meteor. Soc., 81, 639-640.

[40]Hansen, J., G. Russell, D. Rind, P. Stone, A. Lacis, S. Lebedeff, R. Reudy, and L. Travis, 1983: Efficient three-dimensional global models for climate studies: Models I and II. Mon. Wea. Rev., 111, 609-662.

[41]Warrilow, D.A., R.N.B. Smith, and F.E. Hewer, 1990: Snow processes in the 5th annual cycle integration. Met. Office Internal Note No. 93. United Kingdom Meteorological Office, Bracknell, Berkshire RG12 2SZ, UK.

[42]Louis, J.-F., 1979: A parametric model of vertical eddy fluxes in the atmosphere. Bound. Layer Meteor., 17, 187-202.

[43]Warrilow, D.A., A.B. Sangster, and A. Slingo, 1986: Modelling of land surface processes and their influence on European climate. DCTN 38, Dynamical Climatology Branch, United Kingdom Meteorological Office, Bracknell, Berkshire RG12 2SZ, UK.

[44]Shuttleworth, W.J., 1988: Macrohydrology: The new challenge for process hydrology. J. Hydrol., 100, 31-56.

[45]Eagleson, P.S., 1978: Climate, soil and vegetation. Water Resources Res., 14, 705-776.

[46]Monteith, J.L., 1965: Evaporation and environment. Symp. Soc. Exptl. Biol., 19, 205-234.

[47]Cox, P.M., C. Huntingford and R.J. Harding, 1998: A canopy conductance and photosynthesis model for use in a GCM land surface scheme. J. Hydrol., 212-213, 79-94.

[48]Cox, P.M., R.A. Betts, C.B. Bunton, R.L.H. Essery, P.R. Rowntree and J. Smith, 1999: The impact of new land surface physics on the GCM simulation of climate and climate sensitivity. Climate Dyn., 15, 183-203.

[49]Cusack, S., A. Slingo, J.M. Edwards,. and M. Wild, 1998: The radiative impact of a simple aerosol climatology on the Hadley Centre atmospheric GCM, Quart. J. Roy. Meteor. Soc., 124, 2517-2526.

[50]Edwards, J. M., and A. Slingo, 1996: Studies with a flexible new radiation code. I: Choosing a configuration for a large-scale model, Q. J. Roy. Meteorol. Soc., 122, 689-719.

[51]Gregory,  D., 1995: A consistent treatment of the evaporation of rain and snow for use in large scale models. Mon Wea. Rev., 123, 2716-2732.

[52]Gregory,  D.,  and D. Morris, 1996: The sensitivity of climate simulations to the spcification of mixed phase clouds. Climate Dyn., 12, 641-651.

[53]Gregory D, R. Kershaw, and P.M. Inness, 1997: Parameterization of momentum transport by convection. II: Tests in single-column and general circulation models. Quart. J. Roy. Meteor. Soc., 123, 1153-1183.

[54]Gregory, D., G.J. Shutts, and J.R. Mitchell,  1998, A new gravity-wave-drag scheme incorporating anisotropic orography and low-level wave breaking: Impact upon the climate of the UK Meteorological Office Unified Model. Quart. J. Roy. Meteor. Soc.,  124, 463-494.

[55]Mason, P., 1988: The formation of areally-averaged roughness lengths. Quart. J. Roy. Meteor. Soc., 114, 399-420.

[56]Milton, S. F., and C.A. Wilson, 1996: The impact of parametrized sub-grid-scale orographic forcing on systematic errors in a global NWP model. Mon. Wea. Rev. 124,  2023-2045.

[57]Pope, V. D., M.L. Gallani, P.R. Rowntree,  and R.A. Stratton,  2000: The impact of new physical parameterizations in the Hadley Centre climate model: HadAM3. Climate Dyn., 16, 123-146.

[58]Smith, R.N.B., J. Lean, and P.M. Cox, 1994: A surface flux scheme using a generalised Penman-Monteith approach. In Research Activities in Atmospheric Physics, WMO/TD-No. 592, 4.59-4.60.

[59]Wang, W.-C., X.-Z. Liang, M.P. Dudek, D. Pollard, and S.L. Thompson, 1995: Atmospheric ozone as a climate gas., Atm. Res.,37, 247-256.

[60]Cusack, S., J.M. Edwards, and J.M. Crowther, 1999: Investigating k-distribution methods for parameterizing gaseous absorption in the Hadley Centre climate model. J. Geophys. Res., 104, 2051-2057.

[61]Martin, G.M., D.W. Johnson, and A. Spice, 1994: The measurement and parameterization of effective radius in warm stratocumulus couds. J. Atm. Sci., 51, 1823-1842.

[62]Edwards, J.M., 1996: Efficient calculation of infra-red fluxes and cooling rates using the two-stream equations. J. Atm. Sci., 53, 1921-1932.

[63]Williams, P., and M. Smith, 1989: The Frozen Earth. Cambridge University Press, Cambridge, U.K.

[64]Black, P.B., and R.A. Tice, 1988: Comparison of soil freezing and soil water curve data for Windsor sandy loam. U.S. Army Cold Regions Research and Engineering Report 88:16.

[65]Farouki, O., 1981: The thermal properties of snow in cold regions. Cold Region Sci. Technol., 5, 67-75.

[66]Richards, L., 1931: Capillary condition of liquids through porous mediums. Physics, 1, 318-333.

[67]Clapp, R., and G.M. Hornberger, 1978: Empirical equations for some soil hydraulic properties. Water Resourses Res., 14, 601-604.

[68]Cosby, B.J., G.M. Hornberger, R.B. Clapp, and T.R. Ginn, 1984: A statistical exploration of the relationships of soil moisture characteristics to the physical properties of soils. Water Resources Res., 20, 682-690.

[69]Geleyn, J-F., 1988: Interpolation of wind, temperature, and humidity values from model levels to the height of measurement. Tellus, 40A, 347-351.

[70]Potter, G. L., J. M. Slingo, J.-J. Morcrette, and L. Corsetti, 1992: A modeling perspective on cloud radiative forcing. J. Geophys. Res, 97, 20,507-20,518.

[71]Anderson, S.R., and I. Roulstone, 1991: Derivation and calculation of Unified Model potential vorticity and the calculation of potential temperature on PV surfaces. Unified Model Documentation Paper No. 13, United Kingdom Meteorological Office, Bracknell, Berkshire RG12 2SZ, UK.

[72]Goddard, D.M., 1991: Interpolation techniques and grid transformation used in the Unified Model, Unified Model Documentation Paper No. S1, United Kingdom Meteorological Office, Bracknell, Berkshire RG12 2SZ, UK.

[73]Monteith, J.L., 1973: Principles of Environmental Physics. Edward Arnold Publishers, 236 pp.

[74]Senior, C.A., and J.F.B. Mitchell, 1993: Carbon dioxide and climate: The impact of cloud parameterizations. J. Climate, 6, 393-418.

[75]Rothman, L. S., R. R. Gamache, R. H. Tipping, C. P. Rinsland, M. A. H. Smith, D. C. Benner, V. Malathy Devi, J.-M. Flaud, C. Camy-Peyret, A. Perrin, A. Goldman, S. T. Massie, L. R. Brown and R. A. Toth, 1992: The HITRAN molecular database: Editions of 1991 and 1992, J. Quant. Spectrosc. Radiat. Transfer, 48, 469-507.

[76]Kneizys, F.X., E. P. Shettle, L. W. Abreu, J. H. Chetwynd, G. P. Anderson, W. O. Gallery, J. E. A. Selby and S. A. Clough, 1988: User's Guide to LOWTRAN7,  AFGL Report TR 88-0177, Air Force Geophysical Laboratory, Hanscomb Air Force Base, Bedford, Massachusetts.

[77]Clough, S. A., F. X. Kneizys and R. W. Davies, 1989: Line shape and the water vapor continuum, Atmos. Res., 23, 229-241.



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