Teleconnections and Sea Ice Variability in the Greenland Sea.

The purpose of this study is to examine and test the hypothesis that the multiyear sea ice variability in the East Greenland Current is related to the El Nino/Southern Oscillation phenomenon and/or the North Atlantic Oscillation via atmospheric teleconnections. 'Teleconnection' is defined...

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Bibliographic Details
Main Author: Wilson,Ward A , III
Other Authors: NAVAL POSTGRADUATE SCHOOL MONTEREY CA
Format: Text
Language:English
Published: 1986
Subjects:
Soi
Ice
Online Access:http://www.dtic.mil/docs/citations/ADA173550
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA173550
Description
Summary:The purpose of this study is to examine and test the hypothesis that the multiyear sea ice variability in the East Greenland Current is related to the El Nino/Southern Oscillation phenomenon and/or the North Atlantic Oscillation via atmospheric teleconnections. 'Teleconnection' is defined here, after Wallace and Gutzler (1981), as significant simultaneous correlations between temporal fluctuations in oceanic and atmospheric parameters at widely separated points on the earth. The teleconnections included in this test are the Southern Oscillation Index (SOI) and the North Atlantic Oscillation Index (NAO). Anomalous monthly time series for the sea ice extent, SOI, and the NAO are examined for the 25-year period of 1953-1977. The results show that the sea ice anomaly is negatively correlated with the SOI anomaly when the sea ice lags the SOI 24 to 29 months. Cross correlations of the data sets by season failed to reveal any significant seasonal dependence. Keywords: El Nino; Air sea interactions.