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    The Role of the Winter Land Breeze in the Formation of Great Lake Snow Storms

    Source: Bulletin of the American Meteorological Society:;1981:;volume( 062 ):;issue: 004::page 482
    Author:
    Passarelli, Richard E.
    ,
    Braham, Roscoe R.
    DOI: 10.1175/1520-0477(1981)062<0482:TROTWL>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Radar and aircraft data are presented, in the form of case studies, for three shoreline-parallel snow bands that occurred over Lake Michigan. In all three cases a winter land breeze from one or both shores is shown to have an important role in organizing the low-level convergence and convective motions. These cases are compared with earlier studies of lake-effect snow bands on Lakes Erie and Ontario.
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      The Role of the Winter Land Breeze in the Formation of Great Lake Snow Storms

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4160610
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    contributor authorPassarelli, Richard E.
    contributor authorBraham, Roscoe R.
    date accessioned2017-06-09T14:39:57Z
    date available2017-06-09T14:39:57Z
    date copyright1981/04/01
    date issued1981
    identifier issn0003-0007
    identifier otherams-23989.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4160610
    description abstractRadar and aircraft data are presented, in the form of case studies, for three shoreline-parallel snow bands that occurred over Lake Michigan. In all three cases a winter land breeze from one or both shores is shown to have an important role in organizing the low-level convergence and convective motions. These cases are compared with earlier studies of lake-effect snow bands on Lakes Erie and Ontario.
    publisherAmerican Meteorological Society
    titleThe Role of the Winter Land Breeze in the Formation of Great Lake Snow Storms
    typeJournal Paper
    journal volume62
    journal issue4
    journal titleBulletin of the American Meteorological Society
    identifier doi10.1175/1520-0477(1981)062<0482:TROTWL>2.0.CO;2
    journal fristpage482
    journal lastpage492
    treeBulletin of the American Meteorological Society:;1981:;volume( 062 ):;issue: 004
    contenttypeFulltext
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