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    Atmospheric Gravity Waves and Coastal Cyclones

    Source: Monthly Weather Review:;1979:;volume( 107 ):;issue: 006::page 667
    Author:
    Gedzelman, Stanley David
    ,
    Donn, William L.
    DOI: 10.1175/1520-0493(1979)107<0667:AGWACC>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Relations between the behavior of atmospheric gravity waves and the meteorological conditions during the approach of coastal cyclones at Palisades, New York (near New York City) are investigated. It is shown that the temperature and wind conditions favoring the development of the largest amplitude waves are most likely to occur when coastal cyclones strike. This wave record can be used to distinguish between those storms which do and those which do not produce precipitation at New York City. The wave record is also shown to provide a monitor for some of the finer scale features of the storm structures such as the shallow pockets of cold air that often form to the cast of the Appalachian Mountains. Finally, climatological aspects of the gravity-wave behavior for coastal cyclones are investigated and it is shown that there is frequently an abrupt increase in wave amplitudes some 6?12 h prior to the onset of precipitation and an abrupt decrease in wave amplitudes at about the time precipitation ends.
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      Atmospheric Gravity Waves and Coastal Cyclones

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4200050
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    contributor authorGedzelman, Stanley David
    contributor authorDonn, William L.
    date accessioned2017-06-09T16:02:29Z
    date available2017-06-09T16:02:29Z
    date copyright1979/06/01
    date issued1979
    identifier issn0027-0644
    identifier otherams-59487.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4200050
    description abstractRelations between the behavior of atmospheric gravity waves and the meteorological conditions during the approach of coastal cyclones at Palisades, New York (near New York City) are investigated. It is shown that the temperature and wind conditions favoring the development of the largest amplitude waves are most likely to occur when coastal cyclones strike. This wave record can be used to distinguish between those storms which do and those which do not produce precipitation at New York City. The wave record is also shown to provide a monitor for some of the finer scale features of the storm structures such as the shallow pockets of cold air that often form to the cast of the Appalachian Mountains. Finally, climatological aspects of the gravity-wave behavior for coastal cyclones are investigated and it is shown that there is frequently an abrupt increase in wave amplitudes some 6?12 h prior to the onset of precipitation and an abrupt decrease in wave amplitudes at about the time precipitation ends.
    publisherAmerican Meteorological Society
    titleAtmospheric Gravity Waves and Coastal Cyclones
    typeJournal Paper
    journal volume107
    journal issue6
    journal titleMonthly Weather Review
    identifier doi10.1175/1520-0493(1979)107<0667:AGWACC>2.0.CO;2
    journal fristpage667
    journal lastpage681
    treeMonthly Weather Review:;1979:;volume( 107 ):;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
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