APPENDIX E-II
CODE FORM FOR TEMP RAWINSONDE OBSERVATIONS
E-II.1 CODE FORM: TEMP | Parts A and B Up to and including the 100-hPa Surface and |
Parts C and D Above the 100-hPa Surface |
SECTION 1: Parts A, B, C, and D
MiMiMjMj | { |
D....D** YYGGId IIiii* or 99LaLaLa QcLoLoLoLo MMMULaULo*** h0h0h0h0im |
SECTION 2: Parts A and C
99P0P0P0 P1P1h1h1h1 ..... PnPnhnhnhn |
T0T0Ta0D0D0 T1T1Ta1DnDn ..... TnTnTanDnDn |
d0d0f0f0f0 d1d1f1f1f1 ..... dndnfnfnfn |
SECTION 3: Parts A and C
88PtPtPt or 88999 |
TtTtTarDtDt | dtdtftftft |
SECTION 4: Parts A and C
77PmPmPm or 66PmPmPm or 77999 |
} | dmdmfmfmfm (4vbvbvava) |
SECTION 5: Parts B and D
n0n0P0P0P0 T0T0Ta0D0D0
n1n1P1P1P1 T1T1Ta1D1D1
..... .....
nnnnPnPnPn TnTnTanDnDn
APPENDIX E-II.1 CODE FORM: | TEMP Parts A and B Up to and including the 100-hPa Surface and |
Parts C and D Above the 100-hPa Surface |
CODE FORM: | TEMP Parts A and B Up to and including the 100-hPa surface and |
Parts C and D above the 100-hPa surface |
SECTION 6: Part B
21212 | n0n0P0P0P0 n1n1P1P1P1 ..... nnnnPnPnPn |
d0d0f0f0f0 d1d1f1f1f1 ..... dndnfnfnfn |
SECTION 7: Part B
31313 | srrarasasa | 8GGgg | (9snTwTwTw) |
SECTION 8: Parts B and D
41414 | NhCLhCMCH |
SECTION 9: Parts B and D
51515 52525 ..... 59595 |
} | Code groups developed regionally |
SECTION 10: Parts B and D
61616 62626 ..... 69696 |
} | Code groups developed nationally |
APPENDIX E-II.2: TEMP Upper-level Pressure, Temperature, Humidity, and Wind Report Code Forms
CODE FORM: | Parts A and B Up to and including the 100-hPa surface |
Parts C and D above the 100-hPa surface |
E-II.2.1 SECTION 1 Identification and Position Data
MiMiMjMj | { | D....D** YYGGId IIiii* or 99LaLaLa QcLoLoLoLo MMMULaULo*** h0h0h0h0im |
NOTES: Relative to Id indicator |
Symbolic letters and definition |
(1) When wind data are missing for one or
more isobaric surfaces but are available for other isobaric surfaces below and
above, a group (or groups) of solidi shall be
included for the missing data. (2) The wind group shall
be omitted in the case of those isobaric surfaces for which no data are
available, provided wind data are not available for any still higher surface.
(3) Code figure Id = 0 shall
refer to the 1000-hPa level. (4) When wind data are not available for
any standard isobaric surfaces (either in Part A or in Part C), Id
shall be reported by means of a solidus (/). (5) When the wind group relating to the surface level shall be included in the report; when the corresponding wind data are not available, this group shall be coded /////. |
MiMi type of report MjMj part or report transmitted * Used in FM 35 only D....D ship or mobile land station call sign consisting of three or more alphanumeric characters--includes mobile land station observations or issuance of a radiological report on a routine basis and/ or in case of accident. It is recommended that this group be encoded in the form A1A2DDD, where A1A2 are the two-letter geographical designators related to countries or territories as specified in of the Manual on the Global Telecommunications System (Volume 1, Table C1, Part 1, Attachment II-5). DDD are location designators comprising the first three letters of the name of the town or commune where the mobile land station carries out upper-air reporting. |
APPENDIX E-II-2: TEMP Upper-level Pressure, Temperature, Humidity, and Wind Report Code Forms
CODE FORM: | Parts A and B Up to and including the 100-hPa surface |
Parts C and D above the 100-hPa surface (Continued) |
E-II.2.1 SECTION 1 Identification and position data
NOTES: (Continued) |
Symbolic letters and definitions (Continued) |
(6) If wind data are available up to and including the 250-hPa level, the wind group relating to the 200 hPa shall also be included in the report and codes as ///// except when the 250-hPa level is the highest standard isobaric surface reached by the sounding. The same rule shall apply to the 150-hPa level with regard to the 100-hPa level. |
IIiii WMO index number assigned to a fixed land station 99LaLaLa QcLoLoLoLo MMMULaULo replacement group for IIIiii of the report for a sea station, aircraft or a carrier balloon, or a mobile land station. 99 data on position to follow LaLaLa latitude in tenths of a degree Qc quadrant of the globe (Code Table 3333, WMO No. 306) LoLoLoLo longitude in tenths of a degree MMM Marsden square number in which station is located at observation time (Code Table 2590) ULa unit digit of reported latitude ULo unit digit of reported longitude h0h0h0h0im elevation of mobile land station, units of elevation, and elevation accuracy h0hoh0h0 elevation in meters or feet as indicated by im im indicator for units of elevation and confidence factor of accuracy (Code Table 1845) assigned or an identification group assigned for the duration of the activity which the station is supporting. If possible, the mobile station should maintain the same identification for the duration. YY Day of the month (UTC), (01 indicating the 1st day, 02 the 2nd day, etc.) on which the actual time of observation falls. YY shall also be used to indicate the unit of wind speed in addition to indicating the day of the month. When wind speeds are given in knots, 50 shall be added to YY. When the speed is given in meters per second, YY shall not be modified. GG Actual time of observation to the nearest whole hour UTC. In the case of upper-air observations, the actual time of observation is the time at which the balloon is actually released. Id Indicator used to specify the hundreds of hectopascals figure (in Part A of TEMP, TEMP SHIP, and TEMP MOBIL reports) or tens of hectopascals figure (in Part C of TEMP, TEMP SHIP, TEMP DROP and Temp MOBIL reports) of the pressure relative to the last standard isobaric surface for which the wind is reported |
APPENDIX E-II-2: TEMP Upper-level Pressure, Temperature, Humidity, and Wind Report Code Forms
CODE FORM: | Part A Up to and including the 100-hPa surface |
Part C above the 100-hPa surface (Continued) |
E-II.2.2 SECTION 2 Data for standard isobaric surfaces
99P0P0P0 P1P1h1h1h1 ..... PnPnhnhnhn |
T0T0Ta0D0D0 T1T1Ta1DnDn ..... TnTnTanDnDn |
d0d0f0f0f0 d1d1f1f1f1 ..... dndnfnfnfn |
Regulations: |
Symbolic letters and definitions |
The data groups for the surface level and the standard isobaric surfaces of 1000, 925, 850, 700, 500, 400, 300, 250, 200, and 100 hPa shall appear in Part A in ascending order with respect to altitude. For Part C the standard isobaric surfaces are 70, 50, 30, 20, 10, 7, 5, 2, and 1 hPa. When the geopotential of a standard isobaric surface is lower than the altitude of the reporting station, the air temperature-humidity group for that surface shall be included. Solidi (/////) shall be reported for these groups. The wind groups for these levels shall be included as specified by the value reported for symbol Id. When wind data are available for all levels, the wind group shall be included for each level as indicated in the symbolic code form. If wind data are not available for all levels, the procedures given below shall be followed: |
99P0P0P0 T0T0Ta0D0D0 d0d0f0f0f
|
E-II.2.2 SECTION 2 Data for standard isobaric surfaces (Continued)
Regulations: (Continued)
(a) When wind data are missing for one or more standard isobaric surfaces but are available for other standard isobaric surfaces below and above the level of missing wind data, the wind group(s), i.e. dndnfnfnfn, shall be coded by means of solidi (/////).
(b) When wind data are missing for a standard isobaric surface and are also missing for all succeeding standard isobaric surfaces up to the termination of the ascent, the wind group shall be omitted for all these levels and the symbol Id reported accordingly.
Whenever it is desired to extrapolate a sounding for the computation of the geopotential at a standard isobaric surface, the following rules shall apply:
(a) Extrapolation is permissible if, and only if, the pressure difference between the minimum pressure of the sounding and the isobaric surface for which the extrapolated value is being computed does not exceed one quarter of the pressure at which the extrapolated value is desired, provided the extrapolation does not extend through a pressure interval exceeding 25 hPa;
(b) For the purposes of geopotential calculation, and for this purpose only, the sounding will be extrapolated, using two points only of the sounding curve on a T-log p diagram, namely that at the minimum pressure reached by the sounding and that at the pressure given by the sum of this minimum pressure and the pressure differences, mentioned in (a) above.
APPENDIX E-II: TEMP Upper-level Pressure, Temperature, Humidity, and Wind Report Code Forms
CODE FORM: | Part A Up to and including the 100-hPa surface |
Part C above the 100-hPa surface (Continued) |
E-II.2.3 SECTION 3 Data for tropopause level(s)
88PtPtPt or 88999 |
TtTtTatDtDt | dtdtftftft |
Regulations: |
Symbolic letters and definitions |
When more than one tropopause is observed, each shall be reported by repeating Section 3. When no tropopause data are observed, the group 88999 shall be reported for Section 3. 88PtPtPt TtTtTatDtDt Data
for tropopause levels |
PtPtPt Pressure at the tropopause levels. The pressures of the level(s) greater than and including the 30 hPa surface shall be reported in whole hectopascals. TtTt Air temperature in whole degrees Celsius at the tropopause level. This temperature, measured in degrees and tenths, is not rounded off to the next whole degree; only the whole degrees are indicated by TtTt. The tenths of this temperature shall be indicated by means of Tat. Tat Approximate tenths value and sign (plus or minus) of the air temperature at the tropopause level (Code Table 3931). 88999 When no tropopause data are observed, 88999 shall be used for Section 3. |
CODE FORM: | Part A Up to and including the 100-hPa surface |
Part C above the 100-hPa surface (Continued) |
E-II.2.4 SECTION 4 Data for maximum wind level(s) and data for vertical wind shear
77PmPmPm or 66PmPmPm or 77999 |
} | dmdmfmfmfm (4vbvbvava) |
Regulations: |
Symbolic letters and definitions |
When more than one maximum wind level is observed, each
shall be reported by repeating Section 4. When no maximum wind level is observed, the group 77999
shall be reported by for Section 4. Indicator figures 77 shall be used when the
level(s) for which maximum wind data are reported does not coincide with the top
of the wind sounding corresponds to the highest wind speed observed throughout
the ascent. For the purpose of the above regulation, the "top of the wind
sounding" is to be understood as the highest altitude level for which wind
data are available. Group (4vbvbvava) shall be included only if data for vertical wind shear are computed and required. |
77 or 66 Indicator for maximum wind
level(s) and wind shear. Indicator figure 77 shall
be used when the level(s) for which maximum wind data are reported does (do) not
coincide with the top of the wind sounding. Indicator figures 66 shall
be used in the opposite case, i.e. whenever the top of the wind sounding
corresponds to the highest wind speed observed throughout the ascent. The top of
the wind sounding is to be understood as the highest level for which wind data
are available.
PmPmPm Pressure
at the maximum wind level. (1) The pressures from the surface including the
100-hPa surface shall be reported in whole hPas. For
a pressure level less than 100-hPa surface, pressure shall
be reported in tenths of a hectopascal. dmdm True
direction (rounded off to the nearest 5O), in tens of degrees, from
which maximum wind is blowing. fmfmfm Maximum
wind speed in meters per second or knots. (1) When encoding wind direction that
has been rounded off to the nearest 5O, the hundreds and tens
figures of this rounded direction shall be reported
by dd and the units figure shall be added to the
hundreds figure of the wind speed. (2) The day of the month (UTC) shall
be used to indicate the unit of wind speed in addition to indicating the day of
the month. When wind speeds are given in knots, 50 shall
be added to YY. When wind speed is given in meters per second, YY
shall not be modified. (4vbvbvava) Section
containing wind shear. vbvb Absolute
value of the vector difference between the maximum wind and the wind 1 km above
the level of maximum wind, in units indicated by YY. vava Absolute
value of the vector difference between the maximum wind and the wind 1 km above
the level of maximum wind, in units indicated by YY. 77999 When no maximum wind level is observed, the group 77999 shall be reported for Section 4. |
CODE FORM: | Part B Isobaric surfaces up to and including the |
100-hPa surface Part D above the 100-hPa surface (Continued) |
E-II.2.5 SECTION 5 Data for additional levels, with respect to temperature and/or relative humidity
n0n0P0P0P0 n1n1P1P1P1 ..... nnnnPnPnPn |
T0T0Ta0D0D0 T1T1Ta1D1D1 ..... TnTnTanDnDn |
Regulations: |
Symbolic letters and definitions |
If, in the determination of additional levels with respect to specified
criteria for changes in air temperature and/or relative humidity, the criteria
for either variable are satisfied at a particular point in altitude, data for
both variables (as available) shall be reported for
that level. Dew-point data shall be derived using the
function (or near equivalent) for the relationship between saturation vapor
pressure over water and air temperature (Appendix D, Section D.5.) Dew-point
data shall not be reported when the air temperature
is outside the range stated by WMO for the application of the function; a lesser
range may be used as a national practice. The highest level for which a dew point is reported shall
be one of the levels selected. The reported additional levels alone shall make it possible to reconstruct the air temperature and humidity profiles within the limits of the criteria specified. |
Data for significant levels, with respect to
temperature and/or relative humidity.
n0n0P0P0P0
T0T0Ta0D0D0
n0n0 Number
of level, starting with P0P0P0 Pressure
at specified levels. The T0T0 Tens
and units digits of air temperature Ta0 Approximate tenths
value and sign (plus |
APPENDIX E-II: TEMP Upper-level Pressure, Temperature, Humidity, and Wind Report Code Forms
CODE FORM: Part B Isobaric surfaces up to and including
the
100-hPa surface Part D above the 100-hPa surface (Continued)
E-II.2.5 SECTION 5 | Data for mandatory significant levels, with respect to |
temperature and/or relative humidity |
Regulations: (Continued) |
Symbolic letters and definitions (Continued) |
The following shall be included as "mandatory significant levels":
|
D0D0 Dew-point depression at
standard |
Note:
The inversion layers of (c) and (d) may be comprised of several thinner inversion layers separated by thin layers of temperature lapse. To allow for this situation, the tops of the inversion layers or (c) and (d) shall each be at a level such that no further inversion layers, whether thick or thin, shall occur for at least 20 hPa above the level.
The following shall be included as additional levels. They shall be selected in the order given, thereby giving priority to representing the temperature profile. As far as possible, these additional levels shall be the actual levels at which prominent changes in the lapse rate of air temperature occur:
(a) Levels which are necessary to ensure that the temperature obtained by linear interpolation (on a T-log P or essentially similar diagram) between adjacent levels shall not depart from the observed temperature by more than 1OC below the first level reported above the 300-hPa level or the first tropopause, whichever is the lower, or by more than 2OC thereafter;
(b) Levels which are necessary to ensure that the relative humidity obtained by linear interpolation between adjacent additional levels shall not depart by more than 15 percent from the observed values. (The criterion of 15 percent refers to an amount of relative humidity and not to the percentage of the observed value, e.g. if an observed value is 50 percent, the interpolated value shall lie between 35 percent and 65 percent.)
(c) Levels which are necessary to limit the interpolation error on diagrams other than T-log P. These levels shall be such that the pressure at one significant level divided by the pressure of the preceding significant level shall exceed 0.6 for levels up to the first tropopause and shall be determined by use of the method for selecting additional levels but with application of tighter criteria.
When an additional level (with respect to air temperature and/or relative humidity) and a standard isobaric surface coincide, data for that level shall be reported in Parts A and B (or C and D, as appropriate).
In Part B and D, a layer for which data are missing shall be indicated by reporting the boundary levels of the layer and a level of solidi (/////) to indicate the layer of missing data, provided that the layer is at least 20 hPa thick. The boundary levels are the levels closest to the bottom and top of the layer for which the observed data are missing. The boundary levels are not required to meet the additional level criteria. The boundary levels and the missing data level groups will be identified by appropriate nn numbers. For example:
33P3P3P3T3T3Ta3D3D3
44////////
55P5P5P5T5T5Ta5D5D5
where the levels 33 and 55 are the boundary levels and 44 indicates the layer for which data are missing.
APPENDIX E-II: TEMP Upper-level Pressure, Temperature, Humidity, and Wind Report Code Forms
CODE FORM: | Part B Isobaric surfaces up to and including the 100-hPa surface |
Part D above the 100-hPa surface |
E-II.2.6 SECTION 6 Data for additional levels, with respect to winds
21212 | n0n0P0P0P0 n1n1P1P1P1 ..... nnnnPnPnPn |
d0d0f0f0f0 d1d1f1f1f1 ..... dndnfnfnfn |
Regulation: |
Symbolic letters and definitions |
Additional levels shall be chosen so that the
data from them alone shall make it possible to
reconstruct the wind profile with sufficient accuracy for practical use. Note: Criteria for determining additional levels with respect to changes in wind speed and direction are given in Regulation 32.3.1. |
21212 n0n0P0P0P1 d0d0f0f0f0 n0n0 Number of level, starting with P0P0P0 Pressure at
specified levels. Pressure d0d0 True direction (rounded off to
the f0f0f0 Wind speed in
meters per second or (1) When encoding wind direction that has been rounded off
to the nearest 5O, the hundreds and tens figures of this rounded
direction shall be reported by dd and the units
figure shall be added to the hundreds figure of the
wind speed. |
E-II.2.7 SECTION 7 | Data on sea-surface temperature and sounding |
system |
31313 srrarasasa 8GGgg (9snTwTwTw)
Regulation: |
Symbolic letters and definitions |
Section 7 is a mandatory section and shall always be reported. The group srrarasasa and 8GGgg are mandatory for all TEMP, TEMP SHIP, and TEMP MOBIL. In TEMP SHIP reports, the group 9snTWTWTW shall also be included. |
31313 srrarasasa 8GGgg (9snTwTwTw)
|
APPENDIX E-ii: TEMP Upper-level Pressure, Temperature, Humidity, and Wind Report Code Forms
CODE FORM: | Part B Isobaric surfaces up to and including the 100-hPa surface |
Part D above the 100-hPa surface |
E-II.2.8 SECTION 8 Cloud data
41414 NhCLhCMCH
Regulation: |
Symbolic letters and definitions |
In TEMP, TEMP SHIP, and TEMP MOBIL reports, this section
shall be used to report cloud data. Nh,
h, CL, CM, and CH
shall be coded in accordance with the regulations in
FM 12 SYNOP. |
41414 NhCLhCMCH
Section 8 Cloud Data Nh Amount of all the CL present or,
if no CL is present, the amount of all the CM cloud
present. (WMO Code Table 2700) CL Clouds of the genera Stratocumulus, Stratus,
Cumulus and Cumulonimbus. (WMO Code Table 0513) h Height above surface of the base of the lowest cloud seen. (Code Table 1600) (1) the term "height above surface" shall be considered as being the height above the official aerodrome elevation or above station level at a non-aerodrome station, or above the surface of the water in reports from ships CM Clouds of the genera Altocumulus,
Altostratus, and Nimbostratus. (Code Table 0515) (1) The figure to be reported
for CM
shall be determined on the basis of the detailed
description of CM clouds and illustrations of them in the
International Cloud Atlas in conjunction with specifications in Code Table 0515.
CH Clouds of the genera Cirrus, Cirrocumulus and Cirrostratus. (Code Table 0509) (1) The figure to be reported for CH shall be determined on the basis of the detailed description of CH clouds and illustrations of them in the International Cloud Atlas in conjunction with specifications in Code Table 0509. (2) The figure CH = 9 shall be used when the predominant CH clouds are Cirrocumulus although small amounts of Cirrocumulus may be present in the CH cloud system reported under CH = 1 to 8. |
APPENDIX E-II: TEMP Upper-level Pressure, Temperature, Humidity, and Wind Report Code Forms
CODE FORM: | Part B Isobaric surfaces up to and including the |
100-hPa surface Part D above the 100-hPa surface (Continued) |
E-II.2.9 SECTION 9 Code groups developed regionally
|
Symbolic letters and definitions | |
51515 101AdfAdf |
AdfAdf Form of additional data reported (Code Table 421) 5 |
E-II.2.10 SECTION 10 Code groups
developed nationally |
Symbolic letters and definitions |
61616 |
Place holder for Section 10 |
Appendix E-I
Appendix E-III
Table of Contents
Publications List
Home