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dc.contributor.authorIskenderian, Haig
dc.date.accessioned2017-06-09T15:26:28Z
dc.date.available2017-06-09T15:26:28Z
dc.date.copyright1995/06/01
dc.date.issued1995
dc.identifier.issn0894-8755
dc.identifier.otherams-4381.pdf
dc.identifier.urihttp://onlinelibrary.yabesh.ir/handle/yetl/4182634
dc.description.abstractA 10-year cool season climatology of tropical cloud plumes in the Northern Hemisphere was generated by visual inspection of infrared satellite imagery. The sample included 1062 plume events during the months of October to May for the years 1974 to 1984. The results show that the westerly ducts of the tropical eastern Pacific and central Atlantic are preferred regions for tropical cloud plume development. Composite fields of streamfunction and outgoing longwave radiation for eastern Pacific plumes indicate that both low-latitude westerlies in the planetary-scale basic-state flow and the presence of synoptic-scale transients appear to be favorable for plume formation. With a knowledge of these features, some of the interannual and intraannual variability shown in the climatology can be explained.
dc.publisherAmerican Meteorological Society
dc.titleA 10-Year Climatology of Northern Hemisphere Tropical Cloud Plumes and Their Composite Flow Patterns
dc.typeJournal Paper
dc.journal.volume8
dc.journal.issue6
dc.journal.titleJournal of Climate
dc.identifier.doi10.1175/1520-0442(1995)008<1630:AYCONH>2.0.CO;2
dc.journal.fristpage1630
dc.journal.lastpage1637
dc.treeJournal of Climate:;1995:;volume( 008 ):;issue: 006
dc.contenttypeFulltext


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