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.