摘要:This study uses reanalysis data from ECMWF ERA-Interim and GCM output from the
CCSM3 to investigate how sea ice and clouds interact locally (within individual
grid boxes) and whether similar variability between the two datasets is captured.
During autumn (October), the vertically integrated low cloud amount increases
over increased sea ice in the reanalysis, but decreases in the GCM output. Closer
inspection, however, reveals that both datasets have more low cloud cover over
increased sea ice within the lower boundary layer (1000–925 hPa for the reanalysis and
1000–975 hPa for the GCM output), but they differ in their integrated response
within the lower troposphere. These results highlight the differences between the
datasets and show the importance of understanding where cloud changes occur,
because clouds vary in their effect on the radiation budget as a function of height.