WMO Code table 2 - Indicator of parameter

      Code
      figure

      Field parameter

      Unit
      000Reserved
      001PressurePa
      002Pressure reduced to MSL Pa
      003Pressure tendencyPa s-1
      004Potential vorticityK m2 kg-1 s-1
      005ICAO Standard Atmosphere reference heightm
      006Geopotentialm2 s-2
      007Geopotential heightgpm
      008Geometrical heightm
      009Standard deviation of height m
      010Total ozoneDobson
      011TemperatureK
      012Virtual temperatureK
      013Potential temperature K
      014Pseudo-adiabatic potential temperatureK
      015Maximum temperatureK
      016Minimum temperatureK
      017Dew-point temperature K
      018Dew-point depression (or deficit) K
      019Lapse rateK m-1
      020Visibilitym
      021Radar spectra (1)-
      022Radar spectra (2)-
      023Radar spectra (3)-
      024Parcel lifted index (to 500 hPa) (see Note 6)K
      025Temperature anomalyK
      026Pressure anomalyPa
      027Geopotential height anomaly gpm
      028Wave spectra (1)-
      029Wave spectra (2)-
      030Wave spectra (3)-
      031Wind directionDegree true
      032Wind speedm s-1
      033u-component of wind (see Note 4)m s-1
      034v-component of wind (see Note 4)m s-1
      035Stream functionm2 s-1
      036Velocity potentialm2 s-1
      037Montgomery stream function m2 s-1
      038Sigma coordinate vertical velocity s-1
      039Vertical velocityPa s-1
      040Vertical velocitym s-1
      041Absolute vorticitys-1
      042Absolute divergences-1
      043Relative vorticitys-1
      044Relative divergences-1
      045Vertical u-component shear (see Note 4)s-1
      046Vertical v-component shear (see Note 4)s-1
      047Direction of currentDegree true
      048Speed of currentm s-1
      049u-component of current (see Note 4)m s-1
      050v-component of current (see Note 4)m s-1
      051Specific humiditykg kg-1
      052Relative humidity%
      053Humidity mixing ratio kg kg-1
      054Precipitable waterkg m-2
      055Vapor pressurePa
      056Saturation deficitPa
      057Evaporationkg m-2
      058Cloud icekg m-2
      059Precipitation ratekg m-2 s-1
      060Thunderstorm probability %
      061Total precipitationkg m-2
      062Large scale precipitation kg m-2
      063Convective precipitation kg m-2
      064Snowfall rate water equivalent kg m-2 s-1
      065Water equivalent of accumulated snow depthkg m-2
      066Snow depthm
      067Mixed layer depthm
      068Transient thermocline depth m
      069Main thermocline depth m
      070Main thermocline anomaly m
      071Total cloud cover%
      072Convective cloud cover %
      073Low cloud cover%
      074Medium cloud cover%
      075High cloud cover%
      076Cloud waterkg m-2
      077Best lifted index (to 500 hPa) (see Note 6)K
      078Convective snowkg m-2
      079Large scale snowkg m-2
      080Water temperatureK
      081Land cover (1 = land, 0 = sea) Proportion
      082Deviation of sea level from mean m
      083Surface roughnessm
      084Albedo%
      085Soil temperatureK
      086Soil moisture content kg m-2
      087Vegetation%
      088Salinitykg kg-1
      089Densitykg m-3
      090Water run-offkg m-2
      091Ice cover (1 = ice, 0 = no ice) Proportion
      092Ice thicknessm
      093Direction of ice drift Degree true
      094Speed of ice driftm s-1
      095u-component of ice drift (see Note 4)m s-1
      096v-component of ice drift (see Note 4)m s-1
      097Ice growth ratem s-1
      098Ice divergences-1
      099Snow meltkg m-2
      100Significant height of combined wind waves and swellm
      101Direction of wind waves Degree true
      102Significant height of wind waves m
      103Mean period of wind waves s
      104Direction of swell waves Degree true
      105Significant height of swell waves m
      106Mean period of swell waves s
      107Primary wave direction Degree true
      108Primary wave mean period s
      109Secondary wave direction Degree true
      110Secondary wave mean period s
      111Net short-wave radiation flux (surface) (see Note 3)W m-2
      112Net long-wave radiation flux (surface) (see Note 3)W m-2
      113Net short-wave radiation flux (top of atmosphere) (see Note 3)W m-2
      114Net long-wave radiation flux (top of atmosphere) (see Note 3)W m-2
      115Long-wave radiation flux (see Note 3)W m-2
      116Short-wave radiation flux (see Note 3)W m-2
      117Global radiation flux (see Note 3)W m-2
      118Brightness temperature K
      119Radiance (with respect to wave number)W m-1 sr-1
      120Radiance (with respect to wave length)W m-3 sr-1
      121Latent heat fluxW m-2
      122Sensible heat fluxW m-2
      123Boundary layer dissipation W m-2
      124Momentum flux, u-component (see Note 4)N m-2
      125Momentum flux, v-component (see Note 4)N m-2
      126Wind mixing energyJ
      127Image data
      128-254Reserved for originating center use
      255Missing value



      NOTES:

      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 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 centers; since the products generated by centers can be extremely diverse, code figures 128 to 254 are reserved for definition by the originating center and may differ from center to center.

      3. By convention, downward fluxes of radiation or other quantities shall be assigned negative values; upward fluxes of radiation or other quantites shall be assigned positive values.

      4. The u- and v-components of vector quantities are defined in Code table 7.

      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 Meteorology Vocabulary (WMO-No. 182) under the listing "lifted index") is defined as the temperature difference between the ambient 500 hPa 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 conditions 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.



      Back to Top