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Grid geometry

ERA5 data is produced and archived not on a Cartesian grid (a two-dimensional rectangular grid), but on a reduced Gaussian grid - think of it as a globe with a series of evenly spaced data points along each parallel, and parallels spaced at regular intervals. So near the poles you have only few points along a parallel, but close to the equator you have many data points along a parallel.

 

The ERA5 HRES (High Resolution) and  EDA (Ensemble) data are archived in these grid representations:

  • Some (mostly model level) parameters are archived as spectral coefficients (indicated in the data as 'sh', Spherical Harmonics) with a triangular truncation of T639 (HRES) and T319 (EDA)
  • Some (mostly pressure level and surface level) parameters are archived on a reduced Gaussian grid with a resolution of N320 (HRES) and N160 (EDA). These grids are so called "linear grids", sometimes referred to as TL639 (HRES) and TL319 (EDA).

For wave data, both HRES and EDA are archived on a reduced latitude/longitude grid.

For a list of spectral, Gaussian and equivalent lat/lon grids see the Open IFS FAQ > OpenIFS questions: general and runtime >   "What does the 'T' mean in 'T511', 'T1279' etc?"  and "How do I know the grid from from the 'T' number?"

 

When you download ERA5 data, the grid geometry of your output data depends on the selected data format:

  • If you request the data in the native GRIB format it is delivered with the above grid geometry.
  • If you request the data in NetCDF format, it is automatically converted and interpolated from the above grids to a regular lat/lon grid.

Grid resolution

The ERA5 HRES (High Resolution) data has a native resolution of 0.28125 degrees (31km), and the EDA (Ensemble) has a resolution of 0.5625 degrees (62km).

The wave HRES (High Resolution) data has a native resolution of 0.36 degrees, and and the wave EDA (ensemble) has a resolution of 1.0 degrees (EDA).

Projection

All data is made available in spherical coordinates, i.e. unprojected. Some GIS software applications call this 'Geographic Coordinate Systems'.

Coordinate system

All data is made available in Decimal Degrees, lat/lon, with latitude [-90;90] referenced to the equator and longitude [-180;180] referenced to the Greenwich Prime Meridian

Earth model

For data in GRIB1 format the earth model is a sphere with radius = 6367.47 km, as defined in the WMO GRIB Edition 1 specifications, Table 7, GDS Octet 17

For data in GRIB2 format the earth model is a sphere with radius = 6371.2290 km, as defined in the WMO GRIB2 specifications, section 2.2.1, Code Table 3.2, Code figure 6.

For data in NetCDF format (i.e. converted from the native GRIB format to NetCDF), the earth model is inherited from the GRIB data.

Interpolation

When you download ERA5 data you optionally can have the data interpolated to a custom grid and horizontal resolution (eg. 'grid':'0.5/0.5'). The default interpolation method is bilinear for continuous parameters (e.g. Temperature) and nearest neighbour for discrete parameters (eg. Vegetation).

The lat/long equivalent of T639 is 0.28125 deg (360/(2*(639+1))). However, the GRIB1 format only supports three decimals, so we recommend you in any case round the resolution; we recommend to at least 0.3 deg. Specifying a higher resolution is technically possible, e.g. as 'grid':'0.1/0.1', but  this only oversamples the data and does not improve the accuracy of the data.

If you request data in NetCDF format ('format':'netcdf'), interpolation to a regular grid is mandatory, because ECMWF's NetCDF implementation only supports regular grids. Specify the desired lat/lon grid with the 'grid' keyword, for example 'grid':'0.5/0.5'.

Visualisation of regular lat/lon data

If you use ERA5 data in a regular lat/lon grid, many software applications by default visualise the data as a continuous tiled surface, as in plot (a) on the right.

However, you might prefer to think of the ERA5 data as point data with a regular spacing, as shown on the right in plot (b): here global ERA5 data was downloaded with a regular lat/lon grid and a resolution r of 0.3 deg, and plotted on top of a satellite image with 0.25 degree image resolution. The 'top left' ERA5 data point is always at Longitude=0 ; Latitude=90, with further grid points spaced by r, and the 'bottom right' grid point at Longitude=360-r ; Latitude=-90.

(a) Visualisation of regular lat/lon data as a continuous tiled surface

(b) Visualisation of regular lat/lon data as point matrix

For GIS users

Some software applications do not recognise the spatial reference information embedded in the data file and may require you to manually assign a spatial reference. In this case use a 6367.47km sphere for all data if possible. This GRIB1 sphere does not have an EPSG code.

Comparison with other ERA products

  • ERA-Interim is  produced and stored as spectral coefficients with a truncation of T639 or on the N320 reduced Gaussian grid (depending on the parameter). See ERA-Interim: What is the spatial reference

  • ERA-40 has a resolution of T159 (triangular truncation of 159), N80 (80 latitude circles, pole to equator), L60 (model levels).
  • ERA-15 has a resolution of T106 with 31 vertical hybrid levels.

 

 

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