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dc.contributor.authorSellers, William D.
dc.contributor.authorLiu, Wen
dc.date.accessioned2017-06-09T15:07:39Z
dc.date.available2017-06-09T15:07:39Z
dc.date.copyright1988/06/01
dc.date.issued1988
dc.identifier.issn0894-8755
dc.identifier.otherams-3510.pdf
dc.identifier.urihttp://onlinelibrary.yabesh.ir/handle/yetl/4172957
dc.description.abstractEmpirical orthogonal functions (E0Fs) and stepwise regression are used to investigate zonally averaged seasonal temperature anomaly patterns and trends in the upper troposphere and lower stratosphere. The first three EOFs explain more than 50% of the temperature variance and can be related, respectively to the solar flux and El Niño/Southern Oscillation (ENSO), the quasi-biennial oscillation (QBO) and ENSO, and atmospheric carbon dioxide and turbidity (volcanism).
dc.publisherAmerican Meteorological Society
dc.titleTemperature Patterns and Trends in the Upper Troposphere and Lower Stratosphere
dc.typeJournal Paper
dc.journal.volume1
dc.journal.issue6
dc.journal.titleJournal of Climate
dc.identifier.doi10.1175/1520-0442(1988)001<0573:TPATIT>2.0.CO;2
dc.journal.fristpage573
dc.journal.lastpage581
dc.treeJournal of Climate:;1988:;volume( 001 ):;issue: 006
dc.contenttypeFulltext


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