Fig. 3From: The dependence of upper ocean gyres on wind and buoyancy forcingThe zonally averaged zonal velocity (colors) and temperature (contours) from experiments a G1B1W1 and b G2B1W1. c The zonally and vertically averaged temperature above 500Â m in the subpolar region for the two experiments. d The zonally and vertically integrated northward heat transport above 500Â m by the mean flow and eddies for G2B1W1Back to article page