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I'm wondering how the weatherbench2 pipeline handles regridding of variables that have land-sea masks, where land points are NaN. For example, when regridding sea surface temperature, conservative regridding expands sea cells into land areas. The plot below shows an example of this.
the top panel is a slice of SST from gs://weatherbench2/datasets/era5/1959-2023_01_10-6h-240x121_equiangular_with_poles_conservative.zarr
the middle panel is a conservative regridding to the same 240x121 grid, starting from gs://weatherbench2/datasets/era5/1959-2022-full_37-6h-0p25deg_derived.zarr
the bottom panel is the difference
The differences are extremely small, but the land-sea pattern is very different. Is there another step in the pipeline that restores a more realistic land-sea mask in the regridded data?
I'm wondering how the weatherbench2 pipeline handles regridding of variables that have land-sea masks, where land points are NaN. For example, when regridding sea surface temperature, conservative regridding expands sea cells into land areas. The plot below shows an example of this.
gs://weatherbench2/datasets/era5/1959-2023_01_10-6h-240x121_equiangular_with_poles_conservative.zarr
gs://weatherbench2/datasets/era5/1959-2022-full_37-6h-0p25deg_derived.zarr
The differences are extremely small, but the land-sea pattern is very different. Is there another step in the pipeline that restores a more realistic land-sea mask in the regridded data?
The full script producing that figure is below:
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