Thursday, 17 May 2001: 2:14 PM
Global climate models have poor performance in the Arctic region due
to their inability to adequately represent Arctic cloud systems and
cloud/atmosphere/surface albedo radiative interactions. Their
parameterizations of clouds, radiation, and other processes were
developed for the environments vastly different from the Arctic.
In this research a single-column model based on the NOAA National
Centers for Environmental Prediction (NCEP) Global Forecast Model
is adopted and compared with observations from the Surface HEat
Budget of the Arctic Ocean Experiment (SHEBA). The model's
performance in simulating Arctic boundary layer and Arctic cloud
processes under different atmospheric condition is evaluated.
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