ENSO Teleconnections and the North Atlantic Ocean An Exercise in ...
ENSO Teleconnections and the North Atlantic Ocean An Exercise in ...
ENSO Teleconnections and the North Atlantic Ocean An Exercise in ...
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Conclusions<br />
• <strong>ENSO</strong> has areas of significant correlation<br />
aga<strong>in</strong>st SSTA <strong>in</strong> <strong>the</strong> <strong>North</strong> <strong>Atlantic</strong><br />
• <strong>ENSO</strong> doesn't seem to contribute significantly<br />
to <strong>the</strong> NAO, <strong>in</strong>stead may act to weaken it<br />
• Atmospheric processes appear to generate a<br />
negative SSTA correlation <strong>in</strong> <strong>the</strong> subtropical<br />
<strong>North</strong> <strong>Atlantic</strong><br />
• This perturbation <strong>the</strong>n evolves <strong>in</strong>to a region of<br />
positive correlation<br />
• Gulf Stream dynamics are difficult to extract<br />
from a 1-year lag study, especially if <strong>ENSO</strong>'s<br />
signal is felt at an average lag of 2 years<br />
• Correlation studies are useful tools, but<br />
require much more work <strong>and</strong> <strong>in</strong>sight to isolate<br />
14<br />
<strong>the</strong> responsible dynamics