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    ESTIMATION OF FRICTION OF SURFACE WINDS IN THE AUGUST 1949, FLORIDA HURRICANE

    Source: Monthly Weather Review:;1954:;volume( 082 ):;issue: 003::page 73
    Author:
    JOHNSON, RUSSELL E.
    DOI: 10.1175/1520-0493(1954)082<0073:EOFOSW>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: The equations of motion are adapted for use in computing the tangential and normal components of friction in a model hurricane. Values of the components of friction are estimated from surface data of the August 1949 Florida hurricane. The computations are based upon mean pressure and wind profiles describing the front and rear portions of the storm, within 28 to 70 miles from the center, as it moved through the Lake Okeechobee region. The tangential component of friction appears to be greater than the normal component in the region to the rear of the center, while in advance of the center the opposite is generally observed. All friction curves show a continuous increase of friction with wind speed.
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      ESTIMATION OF FRICTION OF SURFACE WINDS IN THE AUGUST 1949, FLORIDA HURRICANE

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4196985
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    contributor authorJOHNSON, RUSSELL E.
    date accessioned2017-06-09T15:55:14Z
    date available2017-06-09T15:55:14Z
    date copyright1954/03/01
    date issued1954
    identifier issn0027-0644
    identifier otherams-56728.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4196985
    description abstractThe equations of motion are adapted for use in computing the tangential and normal components of friction in a model hurricane. Values of the components of friction are estimated from surface data of the August 1949 Florida hurricane. The computations are based upon mean pressure and wind profiles describing the front and rear portions of the storm, within 28 to 70 miles from the center, as it moved through the Lake Okeechobee region. The tangential component of friction appears to be greater than the normal component in the region to the rear of the center, while in advance of the center the opposite is generally observed. All friction curves show a continuous increase of friction with wind speed.
    publisherAmerican Meteorological Society
    titleESTIMATION OF FRICTION OF SURFACE WINDS IN THE AUGUST 1949, FLORIDA HURRICANE
    typeJournal Paper
    journal volume82
    journal issue3
    journal titleMonthly Weather Review
    identifier doi10.1175/1520-0493(1954)082<0073:EOFOSW>2.0.CO;2
    journal fristpage73
    journal lastpage79
    treeMonthly Weather Review:;1954:;volume( 082 ):;issue: 003
    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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