Self - Induced Ekman Pumping Over Oceanic Mesoscale Eddies

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The Influence Ekman Pumping of Wind from Eddy Direction Surface on Currents Gaussian for an Idealized Anticyclonic Gaussian Eddy and Winds from Various Directions Eddy-induced at Ekman 30°S Pumping cm day -1 Contour Interval is 3 cm day -1
4. Ekman Pumping from the Combined Effects of SST Influence and Eddy Surface Currents for an Idealized Gaussian Eddy
Page 1 and 2: Self-Induced Ekman Pumping overOcea
Page 3 and 4: 1. Eddy Influence on SST and Wind S
Page 5: Global Composite Averages of Wind S
Page 10 and 11: The Influence Ekman Pumping of Wind
Page 12 and 13: 3. Ekman Pumping from Eddy Surface
Page 16 and 17: Ekman The Pumping Influence from of
Page 18 and 19: 5. Is the previous Ekman pumping fo
Page 20 and 21: Composite Averages of Eddy-Induced
Page 22 and 23: 6. Influence of Ekman Pumping on Oc
Page 24 and 25: eddy scale Eddy eddy Radius scale A

Self - Induced Ekman Pumping Over Oceanic Mesoscale Eddies

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