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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

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