90° 80° 70° 60° 50° 40° 30° 20° 10° 



Fig. 3a, Computed temperature distribution in an ocean at rest (equilibrium 

 of heat conduction with given sea surface conditions AyA z = 10'). 



3b. Adjustment of mass distribution (temperature) to wind induced cir- 

 culation with the additional assumption of geostrophic equilibrium 

 (schematic). The line -»--*-■+- indicates the layer of no motion 

 for the wind induced circulation. 



20 



