The role of wind-evaporation-SST feedback in tropical variability
The role of wind-evaporation-SST feedback in tropical variability
The role of wind-evaporation-SST feedback in tropical variability
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Annual Mean Climatology: <strong>SST</strong> (Reynolds and<br />
Smith), precipitation (CMAP) and <strong>w<strong>in</strong>d</strong>s (SODA)<br />
(Wang et al., 2004)<br />
Introduction: Roles <strong>of</strong><br />
06-19-2008 CCSM Workshop 2008 W<br />
the WES Feedback<br />
2. Equatorial Annual Cycle:<br />
Westward Propagation<br />
Ocean Temperature: TOGA-TAO moor<strong>in</strong>g data at<br />
the equator and 110 W (Xie, 1994)<br />
H<br />
H<br />
+<br />
Equatorial Section Schematic<br />
L<br />
+<br />
L<br />
+<br />
E
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