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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Introduction: Roles <strong>of</strong><br />
4. Atlantic response to ENSO<br />
06-19-2008 CCSM Workshop 2008<br />
the WES Feedback<br />
Large scale<br />
impacts <strong>of</strong> ENSO<br />
on vertical<br />
motions (Kle<strong>in</strong> et<br />
al., 1999)<br />
Correlation<br />
between<br />
Atlantic <strong>SST</strong><br />
and N<strong>in</strong>o3<br />
<strong>in</strong>dex <strong>in</strong><br />
spr<strong>in</strong>g<br />
(Saravanan<br />
and Chang,<br />
2000)<br />
Correlation between ENSO <strong>in</strong>dex and<br />
upper tropospheric humidity, cloud cover<br />
(ISCCP) and <strong>in</strong>solation (ERBE) (Kle<strong>in</strong> et<br />
al., 1999)
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