Gulf Stream shifts following ENSO events View Full Text


Ontology type: schema:ScholarlyArticle      Open Access: True


Article Info

DATE

1998-06

AUTHORS

Arnold H. Taylor, Michael B. Jordan, John A. Stephens

ABSTRACT

Over the past three decades the annual mean latitude of the Gulf Stream off the coast of the United States has been forecastable from the intensity of the North Atlantic Oscillation (NAO)1, the predictions accounting for more than half the variance. Here we show that much of the unexplained variance can be accounted for by the Southern Oscillation in the Pacific, the Gulf Stream being displaced northwards following El Niño-Southern Oscillation (ENSO) events. This provides a link between events in the equatorial Pacific and the circulation and weather conditions of the North Atlantic. More... »

PAGES

638-638

Identifiers

URI

http://scigraph.springernature.com/pub.10.1038/31380

DOI

http://dx.doi.org/10.1038/31380

DIMENSIONS

https://app.dimensions.ai/details/publication/pub.1041884462


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