I've created historical forcing data from ERA-interim.
I used the total cloud cover of ERA-interim (which is mostly higher than 0.9 over the Arctic) for cloud fraction (cldf), an input variable of CICE. Then, sea ice grows rapidly and becomes thicker than 10 meters within 10 years.
This is probably because ERA-interim's total cloud fraction is too high (higher than 0.9), which substantially weakens incoming shortwave radiation to the surface. In July, CICE-simulated shortwave to the surface is only around 150 W/m2, which is far small than the usual (250 W/m2).
The summer shortwave radiation at the surface was simulated reasonably well in the case when I used ERA-interim's high cloud cover (which is around 0.6-0.7). Am I supposed to use high cloud cover for the CICE cloud fraction (cldf)?
I've created historical forcing data from ERA-interim.
I used the total cloud cover of ERA-interim (which is mostly higher than 0.9 over the Arctic) for cloud fraction (cldf), an input variable of CICE. Then, sea ice grows rapidly and becomes thicker than 10 meters within 10 years. This is probably because ERA-interim's total cloud fraction is too high (higher than 0.9), which substantially weakens incoming shortwave radiation to the surface. In July, CICE-simulated shortwave to the surface is only around 150 W/m2, which is far small than the usual (250 W/m2).
The summer shortwave radiation at the surface was simulated reasonably well in the case when I used ERA-interim's high cloud cover (which is around 0.6-0.7). Am I supposed to use high cloud cover for the CICE cloud fraction (cldf)?