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contributor authorCzaja, Arnaud
date accessioned2017-06-09T16:22:42Z
date available2017-06-09T16:22:42Z
date copyright2004/08/01
date issued2004
identifier issn0894-8755
identifier otherams-6676.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4208133
description abstractIt is suggested that the seasonal dependence of interannual variability displayed by observed sea surface temperature (SST) over the north tropical Atlantic primarily reflects the seasonality of the remote forcing associated with the North Atlantic and Southern Oscillations and is controlled by the mean damping time scale of SST anomaly. A stochastic model including a seasonally dependent forcing is used to test this hypothesis against observations.
publisherAmerican Meteorological Society
titleWhy Is North Tropical Atlantic SST Variability Stronger in Boreal Spring?
typeJournal Paper
journal volume17
journal issue15
journal titleJournal of Climate
identifier doi10.1175/1520-0442(2004)017<3017:WINTAS>2.0.CO;2
journal fristpage3017
journal lastpage3025
treeJournal of Climate:;2004:;volume( 017 ):;issue: 015
contenttypeFulltext


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