Parameters 2: Indicator of parameter
Code tables
Id | Name | Units |
0 | Reserved | |
1 | Pressure | Pa |
2 | Pressure reduced to MSL | Pa |
3 | Pressure tendency | Pa s1 |
4 | Potential vorticity | K m2 kg1 s1 |
5 | ICAO Standard Atmosphere reference height | m |
6 | Geopotential | m2 s2 |
7 | Geopotential height | gpm |
8 | Geometrical height | m |
9 | Standard deviation of height | m |
10 | Total ozone | Dobson |
11 | Temperature | K |
12 | Virtual temperature | K |
13 | Potential temperature | K |
14 | Pseudo-adiabatic potential temperature | K |
15 | Maximum temperature | K |
16 | Minimum temperature | K |
17 | Dew-point temperature | K |
18 | Dew-point depression (or deficit) | K |
19 | Lapse rate | K m1 |
20 | Visibility | m |
21 | Radar spectra (1) | |
22 | Radar spectra (2) | |
23 | Radar spectra (3) | |
24 | Parcel lifted index (to 500 hPa) | K |
25 | Temperature anomaly | K |
26 | Pressure anomaly | Pa |
27 | Geopotential height anomaly | gpm |
28 | Wave spectra (1) | |
29 | Wave spectra (2) | |
30 | Wave spectra (3) | |
31 | Wind direction | Degree true |
32 | Wind speed | m s1 |
33 | u-component of wind | m s1 |
34 | v-component of wind | m s1 |
35 | Stream function | m2 s1 |
36 | Velocity potential | m2 s1 |
37 | Montgomery stream function | m2 s2 |
38 | Sigma coordinate vertical velocity | s1 |
39 | Vertical velocity | Pa s1 |
40 | Vertical velocity | m s1 |
41 | Absolute vorticity | s1 |
42 | Absolute divergence | s1 |
43 | Relative vorticity | s1 |
44 | Relative divergence | s1 |
45 | Vertical u-component shear | s1 |
46 | Vertical v-component shear | s1 |
47 | Direction of current | Degree true |
48 | Speed of current | m s1 |
49 | u-component of current | m s1 |
50 | v-component of current | m s1 |
51 | Specific humidity | kg kg1 |
52 | Relative humidity | % |
53 | Humidity mixing ratio | kg kg1 |
54 | Precipitable water | kg m2 |
55 | Vapour pressure | Pa |
56 | Saturation deficit | Pa |
57 | Evaporation | kg m2 |
58 | Cloud ice | kg m2 |
59 | Precipitation rate | kg m2 s1 |
60 | Thunderstorm probability | % |
61 | Total precipitation | kg m2 |
62 | Large scale precipitation | kg m2 |
63 | Convective precipitation | kg m2 |
64 | Snowfall rate water equivalent | kg m2 s1 |
65 | Water equivalent of accumulated snow depth | kg m2 |
66 | Snow depth | m |
67 | Mixed layer depth | m |
68 | Transient thermocline depth | m |
69 | Main thermocline depth | m |
70 | Main thermocline anomaly | m |
71 | Total cloud cover | % |
72 | Convective cloud cover | % |
73 | Low cloud cover | % |
74 | Medium cloud cover | % |
75 | High cloud cover | % |
76 | Cloud water | kg m2 |
77 | Best lifted index (to 500 hPa) | K |
78 | Convective snow | kg m2 |
79 | Large scale snow | kg m2 |
80 | Water temperature | K |
81 | Land cover (1 = land, 0 = sea) | Proportion |
82 | Deviation of sea level from mean | m |
83 | Surface roughness | m |
84 | Albedo | % |
85 | Soil temperature | K |
86 | Soil moisture content | kg m2 |
87 | Vegetation | % |
88 | Salinity | kg kg1 |
89 | Density | kg m3 |
90 | Water run-off | kg m2 |
91 | Ice cover (1 = ice, 0 = no ice) | Proportion |
92 | Ice thickness | m |
93 | Direction of ice drift | Degree true |
94 | Speed of ice drift | m s1 |
95 | u-component of ice drift | m s1 |
96 | v-component of ice drift | m s1 |
97 | Ice growth rate | m s1 |
98 | Ice divergence | s1 |
99 | Snow melt | kg m2 |
100 | Significant height of combined wind waves and swell | m |
101 | Direction of wind waves | Degree true |
102 | Significant height of wind waves | m |
103 | Mean period of wind waves | s |
104 | Direction of swell waves | Degree true |
105 | Significant height of swell waves | m |
106 | Mean period of swell waves | s |
107 | Primary wave direction | Degree true |
108 | Primary wave mean period | s |
109 | Secondary wave direction | Degree true |
110 | Secondary wave mean period | s |
111 | Net short-wave radiation flux (surface) | W m2 |
112 | Net long-wave radiation flux (surface) | W m2 |
113 | Net short-wave radiation flux (top of atmosphere) | W m2 |
114 | Net long-wave radiation flux (top of atmosphere) | W m2 |
115 | Long-wave radiation flux | W m2 |
116 | Short-wave radiation flux | W m2 |
117 | Global radiation flux | W m2 |
118 | Brightness temperature | K |
119 | Radiance (with respect to wave number) | W m1 sr1 |
120 | Radiance (with respect to wave length) | W m3 sr1 |
121 | Latent heat flux | W m2 |
122 | Sensible heat flux | W m2 |
123 | Boundary layer dissipation | W m2 |
124 | Momentum flux, u-component | N m2 |
125 | Momentum flux, v-component | N m2 |
126 | Wind mixing energy | J |
127 | Image data | |
128 | Reserved for originating centre use | |
255 | Missing value |
( 1) SI units only are used for GRIB; the accuracy or precision with which the data are represented is a function of the range of the values, the decimal and/or binary scaling, and the number of bits used; GRIB enables suitable scaling factors to be selected to obviate the need to define parameters in non-SI units.
( 2) The code figures 0 to 127 are used to represent parameters which are exchanged between a number of centres; since the products generated by centres can be extremely diverse, code figures 128 to 254 are reserved for definition by the originating centre and may differ from centre to centre.
( 3) By convention, downward fluxes of radiation or other quantities shall be assigned negative values; upward fluxes of radiation or other quantities shall be assigned positive values.
( 4) Latitude and longitude are in millidegrees (thousandths of a degree).
( 5) Provision is made for three types of spectra:
-1- direction and frequency
-2- direction and radial number;
-3- radial number and radial number.
( 6) The “parcel lifted index” (as defined in the International Meteorological Vocabulary (WMO–No. 182) under Latitude and longitude are in millidegrees (thousandths of a degree). temperature (T500) and that of a parcel of air lifted from the surface (Tparcel) following the dry and moist adiabatic process. Negative values of (T500 – Tparcel) suggest instability. The “best lifted index” is defined as the most unstable of a collection of parcel lifted indices, with parcel initial condition defined for a collection of 30 hPa thick layers stacked one upon the other with the lowest resting on the ground. Commonly four to six such layers are used in the calculation.