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    Processes Controlling the Structure and Longevity of Two Quasi-Linear Convective Systems Crossing the Southern New England Coast

    Source: Monthly Weather Review:;2013:;volume( 141 ):;issue: 011::page 3710
    Author:
    Lombardo, Kelly
    ,
    Colle, Brian A.
    DOI: 10.1175/MWR-D-12-00336.1
    Publisher: American Meteorological Society
    Abstract: his paper explores the structural evolution and physical processes that explain the modification of two quasi-linear convective systems (QLCSs) that encountered the densely populated New York City?Atlantic coastal region. One QLCS on 31 May 2002 traversed the Atlantic coastal boundary with little change in its intensity, producing widespread severe wind damage across New York City and Long Island. During this event, warm air advection at 925 hPa helped destabilize the layer above this level over the coastal zone, while the marine boundary layer deepened below this level. The 0?3-km line-perpendicular vertical wind shear was relatively strong, which supported ascent along the leading edge of the diabatically generated cold pool. The surface-based convective system became slightly elevated as it moved over the marine waters. In contrast, the 23 July 2002 QLCS decayed upon encountering the Atlantic coastline, despite its coincidence with a surface cold front. The most unstable CAPE values during this decaying event were 400?800 J kg?1 greater than the sustaining 31 May event, though the 0?3-km vertical wind shear was approximately half. Weaker shear likely contributed to limited ascent along the leading edge of the surface based cold pool, and ultimately the demise of the convective line. Sensitivity tests highlight the importance of the relationship between the cold pool and vertical shear during these two events, and illustrate the limited role of the marine layer in modifying the evolution of these two convective systems.
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      Processes Controlling the Structure and Longevity of Two Quasi-Linear Convective Systems Crossing the Southern New England Coast

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    contributor authorLombardo, Kelly
    contributor authorColle, Brian A.
    date accessioned2017-06-09T17:30:52Z
    date available2017-06-09T17:30:52Z
    date copyright2013/11/01
    date issued2013
    identifier issn0027-0644
    identifier otherams-86535.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4230104
    description abstracthis paper explores the structural evolution and physical processes that explain the modification of two quasi-linear convective systems (QLCSs) that encountered the densely populated New York City?Atlantic coastal region. One QLCS on 31 May 2002 traversed the Atlantic coastal boundary with little change in its intensity, producing widespread severe wind damage across New York City and Long Island. During this event, warm air advection at 925 hPa helped destabilize the layer above this level over the coastal zone, while the marine boundary layer deepened below this level. The 0?3-km line-perpendicular vertical wind shear was relatively strong, which supported ascent along the leading edge of the diabatically generated cold pool. The surface-based convective system became slightly elevated as it moved over the marine waters. In contrast, the 23 July 2002 QLCS decayed upon encountering the Atlantic coastline, despite its coincidence with a surface cold front. The most unstable CAPE values during this decaying event were 400?800 J kg?1 greater than the sustaining 31 May event, though the 0?3-km vertical wind shear was approximately half. Weaker shear likely contributed to limited ascent along the leading edge of the surface based cold pool, and ultimately the demise of the convective line. Sensitivity tests highlight the importance of the relationship between the cold pool and vertical shear during these two events, and illustrate the limited role of the marine layer in modifying the evolution of these two convective systems.
    publisherAmerican Meteorological Society
    titleProcesses Controlling the Structure and Longevity of Two Quasi-Linear Convective Systems Crossing the Southern New England Coast
    typeJournal Paper
    journal volume141
    journal issue11
    journal titleMonthly Weather Review
    identifier doi10.1175/MWR-D-12-00336.1
    journal fristpage3710
    journal lastpage3734
    treeMonthly Weather Review:;2013:;volume( 141 ):;issue: 011
    contenttypeFulltext
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