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    A CASE STUDY OF CONFLUENCE AS RELATED TO THE JET STREAM

    Source: Journal of Meteorology:;1951:;volume( 008 ):;issue: 004::page 231
    Author:
    Clapp, Philip F.
    ,
    Winston, Jay S.
    DOI: 10.1175/1520-0469(1951)008<0231:ACSOCA>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: This is the second report on a continuing project designed to investigate quantitatively the confluence process and associated changes in the strength and location of the mid-tropospheric jet stream. An empirical study has been made of a case of large-scale confluence as observed on a sequence of 5-day mean charts. It is found that the local change in wind speed is related to the relative advection of cold and warm air on either side of the jet axis and also to the advection of wind speed along the axis. Tentative estimates of vertical motion indicate sinking motion in the cold air north of the jet axis and rising motion in the warm air to the south.
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      A CASE STUDY OF CONFLUENCE AS RELATED TO THE JET STREAM

    URI
    http://yetl.yabesh.ir/yetl1/handle/yetl/4149343
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    contributor authorClapp, Philip F.
    contributor authorWinston, Jay S.
    date accessioned2017-06-09T14:10:26Z
    date available2017-06-09T14:10:26Z
    date copyright1951/08/01
    date issued1951
    identifier issn0095-9634
    identifier otherams-13848.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4149343
    description abstractThis is the second report on a continuing project designed to investigate quantitatively the confluence process and associated changes in the strength and location of the mid-tropospheric jet stream. An empirical study has been made of a case of large-scale confluence as observed on a sequence of 5-day mean charts. It is found that the local change in wind speed is related to the relative advection of cold and warm air on either side of the jet axis and also to the advection of wind speed along the axis. Tentative estimates of vertical motion indicate sinking motion in the cold air north of the jet axis and rising motion in the warm air to the south.
    publisherAmerican Meteorological Society
    titleA CASE STUDY OF CONFLUENCE AS RELATED TO THE JET STREAM
    typeJournal Paper
    journal volume8
    journal issue4
    journal titleJournal of Meteorology
    identifier doi10.1175/1520-0469(1951)008<0231:ACSOCA>2.0.CO;2
    journal fristpage231
    journal lastpage243
    treeJournal of Meteorology:;1951:;volume( 008 ):;issue: 004
    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