Eastern Boundary Upwelling Systems response to different atmospheric forcing in a global eddy-permitting ocean model
Three-dimensional ocean dynamics (eg coastal upwelling, Ekman Pumping, meridional
currents) in the Eastern Boundary Upwelling Systems (EBUS) is largely dictated by the
strength of equatorward wind and its cross-shore gradients. Ocean dynamics, in turn, affects
the coastal sea surface temperature (SST). Mis-representing the wind fields may therefore
lead to inaccurate current structures and, thus, to significant SST biases. Analysis of two
atmospheric reanalysis products, ERAInterim (ERAINT) and JRA55-do version 1.1 (JRA55) …
currents) in the Eastern Boundary Upwelling Systems (EBUS) is largely dictated by the
strength of equatorward wind and its cross-shore gradients. Ocean dynamics, in turn, affects
the coastal sea surface temperature (SST). Mis-representing the wind fields may therefore
lead to inaccurate current structures and, thus, to significant SST biases. Analysis of two
atmospheric reanalysis products, ERAInterim (ERAINT) and JRA55-do version 1.1 (JRA55) …
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