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    A Reanalysis of Hurricane Andrew's Intensity

    Source: Bulletin of the American Meteorological Society:;2004:;volume( 085 ):;issue: 011::page 1699
    Author:
    Landsea, Christopher W.
    ,
    Franklin, James L.
    ,
    McAdie, Colin J.
    ,
    Beven, John L.
    ,
    Gross, James M.
    ,
    Jarvinen, Brian R.
    ,
    Pasch, Richard J.
    ,
    Rappaport, Edward N.
    ,
    Dunion, Jason P.
    ,
    Dodge, Peter P.
    DOI: 10.1175/BAMS-85-11-1699
    Publisher: American Meteorological Society
    Abstract: Hurricane Andrew of 1992 caused unprecedented economic devastation along its path through the Bahamas, southeastern Florida, and Louisiana. Damage in the United States was estimated to be $26 billion (in 1992 dollars), making Andrew one of the most expensive natural disasters in U.S. history. This hurricane struck southeastern Florida with maximum 1-min surface winds estimated in a 1992 poststorm analysis at 125 kt (64 m s?1). This original assessment was primarily based on an adjustment of aircraft reconnaissance flight-level winds to the surface. Based on recent advancements in the understanding of the eyewall wind structure of major hurricanes, the official intensity of Andrew was adjusted upward for five days during its track across the Atlantic Ocean and Gulf of Mexico by the National Hurricane Center Best Track Change Committee. In particular, Andrew is now assessed by the National Hurricane Center to be a Saffir?Simpson Hurricane Scale category-5 hurricane (the highest intensity category possible) at its landfall in southeastern Florida, with maximum 1-min winds of 145 kt (75 m s?1). This makes Andrew only the third category-5 hurricane to strike the United States since at least 1900. Implications for how this change impacts society's planning for such extreme events are discussed.
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      A Reanalysis of Hurricane Andrew's Intensity

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    contributor authorLandsea, Christopher W.
    contributor authorFranklin, James L.
    contributor authorMcAdie, Colin J.
    contributor authorBeven, John L.
    contributor authorGross, James M.
    contributor authorJarvinen, Brian R.
    contributor authorPasch, Richard J.
    contributor authorRappaport, Edward N.
    contributor authorDunion, Jason P.
    contributor authorDodge, Peter P.
    date accessioned2017-06-09T16:42:24Z
    date available2017-06-09T16:42:24Z
    date copyright2004/11/01
    date issued2004
    identifier issn0003-0007
    identifier otherams-72649.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4214675
    description abstractHurricane Andrew of 1992 caused unprecedented economic devastation along its path through the Bahamas, southeastern Florida, and Louisiana. Damage in the United States was estimated to be $26 billion (in 1992 dollars), making Andrew one of the most expensive natural disasters in U.S. history. This hurricane struck southeastern Florida with maximum 1-min surface winds estimated in a 1992 poststorm analysis at 125 kt (64 m s?1). This original assessment was primarily based on an adjustment of aircraft reconnaissance flight-level winds to the surface. Based on recent advancements in the understanding of the eyewall wind structure of major hurricanes, the official intensity of Andrew was adjusted upward for five days during its track across the Atlantic Ocean and Gulf of Mexico by the National Hurricane Center Best Track Change Committee. In particular, Andrew is now assessed by the National Hurricane Center to be a Saffir?Simpson Hurricane Scale category-5 hurricane (the highest intensity category possible) at its landfall in southeastern Florida, with maximum 1-min winds of 145 kt (75 m s?1). This makes Andrew only the third category-5 hurricane to strike the United States since at least 1900. Implications for how this change impacts society's planning for such extreme events are discussed.
    publisherAmerican Meteorological Society
    titleA Reanalysis of Hurricane Andrew's Intensity
    typeJournal Paper
    journal volume85
    journal issue11
    journal titleBulletin of the American Meteorological Society
    identifier doi10.1175/BAMS-85-11-1699
    journal fristpage1699
    journal lastpage1712
    treeBulletin of the American Meteorological Society:;2004:;volume( 085 ):;issue: 011
    contenttypeFulltext
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