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    A 10-Year Climatology of Northern Hemisphere Tropical Cloud Plumes and Their Composite Flow Patterns

    Source: Journal of Climate:;1995:;volume( 008 ):;issue: 006::page 1630
    Author:
    Iskenderian, Haig
    DOI: 10.1175/1520-0442(1995)008<1630:AYCONH>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: A 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.
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      A 10-Year Climatology of Northern Hemisphere Tropical Cloud Plumes and Their Composite Flow Patterns

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4182634
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    contributor authorIskenderian, Haig
    date accessioned2017-06-09T15:26:28Z
    date available2017-06-09T15:26:28Z
    date copyright1995/06/01
    date issued1995
    identifier issn0894-8755
    identifier otherams-4381.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4182634
    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.
    publisherAmerican Meteorological Society
    titleA 10-Year Climatology of Northern Hemisphere Tropical Cloud Plumes and Their Composite Flow Patterns
    typeJournal Paper
    journal volume8
    journal issue6
    journal titleJournal of Climate
    identifier doi10.1175/1520-0442(1995)008<1630:AYCONH>2.0.CO;2
    journal fristpage1630
    journal lastpage1637
    treeJournal of Climate:;1995:;volume( 008 ):;issue: 006
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
    نرم افزار کتابخانه دیجیتال "دی اسپیس" فارسی شده توسط یابش برای کتابخانه های ایرانی | تماس با یابش
    yabeshDSpacePersian