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    Damage Survey of Hurricane Andrew and Its Relationship to the Eyewall

    Source: Bulletin of the American Meteorological Society:;1994:;volume( 075 ):;issue: 002::page 189
    Author:
    Wakimoto, Roger M.
    ,
    Black, Peter G.
    DOI: 10.1175/1520-0477(1994)075<0189:DSOHAA>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: A damage map documenting Hurricane Andrew's destructive land fall over southern Florida is presented. Vectors that represent the direction of winds causing damage to trees and structures are shown along with an F-scale rating in order to assess the strength of the near-surface winds. It is hypothesized that increased surface roughness once the hurricane made landfall may have contributed to a surface wind enhancement resulting in the strongest winds ever estimated (F3) for a landfall hurricane. This intense damage occurred primarily during the ?second? period of strong winds associated with the east side of the eyewall. For the first time, a well-defined circulation in the damage pattern by the second wind was documented. A superposition of radar data from Miami and Key West on top of the damage map provides the first detailed examination of the relationship between the eyewall and the surface flow field as estimated from the damage vectors.
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      Damage Survey of Hurricane Andrew and Its Relationship to the Eyewall

    URI
    http://yetl.yabesh.ir/yetl1/handle/yetl/4161188
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    • Bulletin of the American Meteorological Society

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    contributor authorWakimoto, Roger M.
    contributor authorBlack, Peter G.
    date accessioned2017-06-09T14:41:20Z
    date available2017-06-09T14:41:20Z
    date copyright1994/02/01
    date issued1994
    identifier issn0003-0007
    identifier otherams-24508.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4161188
    description abstractA damage map documenting Hurricane Andrew's destructive land fall over southern Florida is presented. Vectors that represent the direction of winds causing damage to trees and structures are shown along with an F-scale rating in order to assess the strength of the near-surface winds. It is hypothesized that increased surface roughness once the hurricane made landfall may have contributed to a surface wind enhancement resulting in the strongest winds ever estimated (F3) for a landfall hurricane. This intense damage occurred primarily during the ?second? period of strong winds associated with the east side of the eyewall. For the first time, a well-defined circulation in the damage pattern by the second wind was documented. A superposition of radar data from Miami and Key West on top of the damage map provides the first detailed examination of the relationship between the eyewall and the surface flow field as estimated from the damage vectors.
    publisherAmerican Meteorological Society
    titleDamage Survey of Hurricane Andrew and Its Relationship to the Eyewall
    typeJournal Paper
    journal volume75
    journal issue2
    journal titleBulletin of the American Meteorological Society
    identifier doi10.1175/1520-0477(1994)075<0189:DSOHAA>2.0.CO;2
    journal fristpage189
    journal lastpage200
    treeBulletin of the American Meteorological Society:;1994:;volume( 075 ):;issue: 002
    contenttypeFulltext
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