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    Mesoscale Vortices in the Weddell Sea Region (Antarctica)

    Source: Monthly Weather Review:;1990:;volume( 118 ):;issue: 003::page 779
    Author:
    Heinemann, Günther
    DOI: 10.1175/1520-0493(1990)118<0779:MVITWS>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Preliminary results of investigations of Antarctic mesocyclones in the Weddell Sea region are presented for the Antarctic summer periods 1983?88. Based on NOAA and METEOR satellite images, a total of 195 mesoscale vortices (scale less than 1000 km) were observed and classified using a simple classification scheme, depending on lifetime and cortex diameter. The highest frequency of vortices was found over the ice free part of the eastern Weddell Sea. Mean synoptic conditions for vortices with scales less than 400 km near Halley Station indicate an offshore flow being most favorable for their development. A case study with satellite images, surface measurements, synoptic analyses derived from TOVS data shows the evolution of several mesoscale vortices in a pool of cold air in the eastern Weddell Sea.
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      Mesoscale Vortices in the Weddell Sea Region (Antarctica)

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4202382
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    contributor authorHeinemann, Günther
    date accessioned2017-06-09T16:07:46Z
    date available2017-06-09T16:07:46Z
    date copyright1990/03/01
    date issued1990
    identifier issn0027-0644
    identifier otherams-61585.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4202382
    description abstractPreliminary results of investigations of Antarctic mesocyclones in the Weddell Sea region are presented for the Antarctic summer periods 1983?88. Based on NOAA and METEOR satellite images, a total of 195 mesoscale vortices (scale less than 1000 km) were observed and classified using a simple classification scheme, depending on lifetime and cortex diameter. The highest frequency of vortices was found over the ice free part of the eastern Weddell Sea. Mean synoptic conditions for vortices with scales less than 400 km near Halley Station indicate an offshore flow being most favorable for their development. A case study with satellite images, surface measurements, synoptic analyses derived from TOVS data shows the evolution of several mesoscale vortices in a pool of cold air in the eastern Weddell Sea.
    publisherAmerican Meteorological Society
    titleMesoscale Vortices in the Weddell Sea Region (Antarctica)
    typeJournal Paper
    journal volume118
    journal issue3
    journal titleMonthly Weather Review
    identifier doi10.1175/1520-0493(1990)118<0779:MVITWS>2.0.CO;2
    journal fristpage779
    journal lastpage793
    treeMonthly Weather Review:;1990:;volume( 118 ):;issue: 003
    contenttypeFulltext
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