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    An Analysis of Multiple Predecessor Rain Events ahead of Tropical Cyclones Ike and Lowell: 10–15 September 2008

    Source: Monthly Weather Review:;2011:;volume( 140 ):;issue: 004::page 1081
    Author:
    Bosart, Lance F.
    ,
    Cordeira, Jason M.
    ,
    Galarneau, Thomas J.
    ,
    Moore, Benjamin J.
    ,
    Archambault, Heather M.
    DOI: 10.1175/MWR-D-11-00163.1
    Publisher: American Meteorological Society
    Abstract: n analysis of three predecessor rain events (PREs) that occurred ahead of North Atlantic tropical cyclone (TC) Ike and east Pacific TC Lowell during 10?15 September 2008 is presented. The three PREs produced all-time daily record rainfall at many locations, including Lubbock, Texas (189.5 mm); Wichita, Kansas (262 mm); and Chicago?O?Hare, Illinois (169 mm), on 11?13 September, respectively.PRE 1 organized over Texas on 10 September with moisture from a stalled frontal boundary and the Bay of Campeche, and matured with moisture from TC Lowell. PRE 2 organized over the Texas Panhandle on 11 September with moisture from the Bay of Campeche, and developed and matured over Kansas and Missouri with moisture from TC Lowell. PRE 3 developed over Texas on 11 September, merged with and absorbed PRE 2 over Kansas and Missouri, and matured as it ingested moisture from TC Ike. All three PREs matured in the equatorward entrance region of an intensifying subtropical jet stream (STJ).Heavy rainfall with the three PREs occurred along a plume of moist air characterized by high precipitable water values that extended poleward over the central United States near the juxtaposition of the nose of a low-level jet, a region of lower-tropospheric forcing for ascent along a surface baroclinic zone, and the STJ equatorward entrance region. The cumulative upscale effect of persistent deep convection from the three PREs enhanced and ?locked in? a favorable upper-tropospheric flow pattern conducive to ridge development over the Ohio Valley and STJ intensification over the central U.S. and Great Lakes region.
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      An Analysis of Multiple Predecessor Rain Events ahead of Tropical Cyclones Ike and Lowell: 10–15 September 2008

    URI
    http://yetl.yabesh.ir/yetl1/handle/yetl/4229724
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    • Monthly Weather Review

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    contributor authorBosart, Lance F.
    contributor authorCordeira, Jason M.
    contributor authorGalarneau, Thomas J.
    contributor authorMoore, Benjamin J.
    contributor authorArchambault, Heather M.
    date accessioned2017-06-09T17:29:30Z
    date available2017-06-09T17:29:30Z
    date copyright2012/04/01
    date issued2011
    identifier issn0027-0644
    identifier otherams-86193.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4229724
    description abstractn analysis of three predecessor rain events (PREs) that occurred ahead of North Atlantic tropical cyclone (TC) Ike and east Pacific TC Lowell during 10?15 September 2008 is presented. The three PREs produced all-time daily record rainfall at many locations, including Lubbock, Texas (189.5 mm); Wichita, Kansas (262 mm); and Chicago?O?Hare, Illinois (169 mm), on 11?13 September, respectively.PRE 1 organized over Texas on 10 September with moisture from a stalled frontal boundary and the Bay of Campeche, and matured with moisture from TC Lowell. PRE 2 organized over the Texas Panhandle on 11 September with moisture from the Bay of Campeche, and developed and matured over Kansas and Missouri with moisture from TC Lowell. PRE 3 developed over Texas on 11 September, merged with and absorbed PRE 2 over Kansas and Missouri, and matured as it ingested moisture from TC Ike. All three PREs matured in the equatorward entrance region of an intensifying subtropical jet stream (STJ).Heavy rainfall with the three PREs occurred along a plume of moist air characterized by high precipitable water values that extended poleward over the central United States near the juxtaposition of the nose of a low-level jet, a region of lower-tropospheric forcing for ascent along a surface baroclinic zone, and the STJ equatorward entrance region. The cumulative upscale effect of persistent deep convection from the three PREs enhanced and ?locked in? a favorable upper-tropospheric flow pattern conducive to ridge development over the Ohio Valley and STJ intensification over the central U.S. and Great Lakes region.
    publisherAmerican Meteorological Society
    titleAn Analysis of Multiple Predecessor Rain Events ahead of Tropical Cyclones Ike and Lowell: 10–15 September 2008
    typeJournal Paper
    journal volume140
    journal issue4
    journal titleMonthly Weather Review
    identifier doi10.1175/MWR-D-11-00163.1
    journal fristpage1081
    journal lastpage1107
    treeMonthly Weather Review:;2011:;volume( 140 ):;issue: 004
    contenttypeFulltext
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