Introduction
Studies over the past several decades have used
drifting buoys to improve our understanding of the North Atlantic surface
circulation. Here we focus on the velocities obtained from drifters deployed
during 1993-1997. The goal of the study is to understand the mean and
variability of the surface flow, as well as the nature of the intrinsic
scales in the real ocean and two ocean models, one eddy-permitting and one
eddy-resolving, for that period. The results of these analyses are used to
determine the potential usefulness of the models to synoptic forecasting of the
surface circulation. |
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