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Fields that can get used for storm tracking.

  PN  sea level pressure [hPa]
  PNS  smoothed sea level pressure [hPa]
  VORT  relative vorticity at 850 hPa [1/s]
  VORS  smoothed relative vorticity at 850 hPa [1/s]
  UGEO
  geostrophic u-wind at 500 hPa [m/s]
  VGEO
  geostrophic v-wind at 500 hPa [m/s]
  UU  10m u-wind [knots]
  VV  10m v-wind [knots]

Location:
    UQAM: ~data/ReAnalysis/ERA5/Stormfields

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 Evaporation  evaporation 3
 t2m 2 metre temperature [K] 1-hourly forecast
 d2m 2 metre dewpoint temperature [K] 1-hourly forecast
 tp Total precipitation1 [m] 1-hourly forecast
 tp_deaccum Deaccumulated total precipitation2 [mm] 1-hourly forecast
 u10 10 metre U wind component [m/s] 1-hourly forecast
 v10 10 metre V wind component [m/s] 1-hourly forecast
 e Evaporation3 [m of water equivalent] 1-hourly forecast
 e_deaccum Deaccumulated evaporation4 [mm] 1-hourly forecast
 sd Snow depth (snow water equivalent) [m of water equivalent] 1-hourly analysis
 sde Snow depth (physical snow depth) [m] 1-hourly forecast
 skt Skin temperature [K] 1-hourly analysis
 ssrd Surface solar radiation downwards5 [J m-2] 1-hourly forecast
 ssrd_deaccumSurface solar radiation downwards6 [W m-2] 1-hourly forecast

1tp is the total precipitation download directly from ERA5-Land which accumulate daily up to 00Z. tp at 00Z is then the total accumulation for the previous day.

2tp_deaccum is the deaccumulated total precipitation which was locally computed. The output of tp_deaccum at hZ is then the accumulated precipitation from ]h-1,h].

3e is the evaporation download directly from ERA5-Land which accumulate daily up to 00Z. tp at 00Z is then the total accumulation for the previous day.

4e_deaccum is the deaccumulated evaporation which was locally computed. The output of e_deaccum at hZ is then the accumulated evaporation from ]h-1,h].

5ssrd is the surface solar radiation downwards download directly from ERA5-Land which accumulate daily up to 00Z. tp at 00Z is then the total accumulation for the previous day.

6ssrd_deaccum is the deaccumulated surface solar radiation downwards which was locally computed. The output of e_deaccum at hZ is then the accumulated evaporation from ]h-1,h].

Location:
    UQAM:
         NetCDF format: ~archive/REANALYSES/ERA5-Land

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