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contributor authorDeser, Clara
contributor authorBlackmon, Maurice L.
date accessioned2017-06-09T15:26:34Z
date available2017-06-09T15:26:34Z
date copyright1995/06/01
date issued1995
identifier issn0894-8755
identifier otherams-4384.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4182667
description abstractEmpirical orthogonal function analysis of winter sea surface temperature (SST) anomalies over the Pacific domain (60°N?20°S) reveals an El Niño-Southern Oscillation (ENSO) mode that is linked to the eastern North Pacific, and a North Pacific mode that is linearly independent of ENSO. The North Pacific mode exhibits maximum amplitude and variance explained along ?40°N, west of ?170°W. SSTs in this region have decreased by ?1.5°C from 1950 to 1987. The cooling in winter has been associated with a strengthening of the overlying westerly winds.
publisherAmerican Meteorological Society
titleOn the Relationship between Tropical and North Pacific Sea Surface Temperature Variations
typeJournal Paper
journal volume8
journal issue6
journal titleJournal of Climate
identifier doi10.1175/1520-0442(1995)008<1677:OTRBTA>2.0.CO;2
journal fristpage1677
journal lastpage1680
treeJournal of Climate:;1995:;volume( 008 ):;issue: 006
contenttypeFulltext


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