Abstract

Intensive observations of the low frequency (less than one cycle per day) response of upwelling regimes to fluctuations in the wind have been made in two locations: the Oregon coast near 45°15'N, and the Northwest African coast at 21°40'N. Both regimes show an equatorward coastal jet at the surface, quasi-barotropic fluctuations in the alongshore flow, and a poleward undercurrent....

Share

COinS