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    THE GULF STREAM FRONT: A CAUSE OF STRATUS ON THE LOWER ATLANTIC COAST

    Source: Monthly Weather Review:;1950:;volume( 078 ):;issue: 006::page 91
    Author:
    CARSON, ROBE B.
    DOI: 10.1175/1520-0493(1950)078<0091:TGSFAC>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Wintertime stratus along the lower Atlantic coast of the United States is discussed and the frontal hypothesis for its formation is stated. Evidence from sequences of weather charts is presented in support of the frontal interpretation.
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      THE GULF STREAM FRONT: A CAUSE OF STRATUS ON THE LOWER ATLANTIC COAST

    URI
    https://yetl.yabesh.ir/yetl1/handle/yetl/4196785
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    contributor authorCARSON, ROBE B.
    date accessioned2017-06-09T15:54:28Z
    date available2017-06-09T15:54:28Z
    date copyright1950/06/01
    date issued1950
    identifier issn0027-0644
    identifier otherams-56548.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4196785
    description abstractWintertime stratus along the lower Atlantic coast of the United States is discussed and the frontal hypothesis for its formation is stated. Evidence from sequences of weather charts is presented in support of the frontal interpretation.
    publisherAmerican Meteorological Society
    titleTHE GULF STREAM FRONT: A CAUSE OF STRATUS ON THE LOWER ATLANTIC COAST
    typeJournal Paper
    journal volume78
    journal issue6
    journal titleMonthly Weather Review
    identifier doi10.1175/1520-0493(1950)078<0091:TGSFAC>2.0.CO;2
    journal fristpage91
    journal lastpage101
    treeMonthly Weather Review:;1950:;volume( 078 ):;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