Closed mlangguth89 closed 3 months ago
The windspeed data downloaded from here cannot be remapped with CDO since the coordinate data cannot be correctly infered.
To enable this, several changes to the netCDF-file have to be undertaken as listed below:
RLAT
and RLON
: ncks -C -O -x -v <file> <file>
rlat
and rlon
(the actual coordinate data): ncatted -O -a long_name,rlon,o,c,"longitude in rotated pole grid" <file>
, ncatted -O -a long_name,rlat,o,c,"latitude in rotated pole grid" <file>
, ncatted -O -a standard_name,rlon,o,c,"grid_longitude" <file>
and ncatted -O -a standard_name,rlat,o,c,"grid_latitude" <file>
ncks -A -v rotated_pole ../T_2M/T_2M.2D.201812.nc <file>
grid_mapping
-attribute to data variable: ncatted -O -a grid_mapping,wind_speed,o,c,rotated_pole <file>
This ensures that conservative reampping is handling the underlying curvilinear grid in a correct way. The downloaded data has been processed with a Bash-script accordingly.
For consistency, the variable is also renamed into WS_100M
(instead of wind_speed
).
Final 100m wind speed dataset is now available under /p/scratch/deepacf/maelstrom/maelstrom_data/ap5/downscaling_benchmark_dataset/benchmark_wind/dataset
.
Support of pressure-based vaiables is implemented and thus, the issue can be closed.
The study of [Höhlein et al., 2020] suggests the 500 hPa geopotential as predictor variable (to identify large-scale weather patterns). While pressure-level based variables from ERA5 can be retrieved [here](), the pre-processing does not support handling of these variables yet. This will be fixed in the related issue-branch.
Furthermore, fixes/adaptions in handling the target COSMO REA6 data will be documented in this issue (see below).