YaBeSH Engineering and Technology Library

    • Journals
    • PaperQuest
    • YSE Standards
    • YaBeSH
    • Login
    View Item 
    •   YE&T Library
    • AMS
    • Monthly Weather Review
    • View Item
    •   YE&T Library
    • AMS
    • Monthly Weather Review
    • View Item
    • All Fields
    • Source Title
    • Year
    • Publisher
    • Title
    • Subject
    • Author
    • DOI
    • ISBN
    Advanced Search
    JavaScript is disabled for your browser. Some features of this site may not work without it.

    Archive

    The Great Plains Low-Level Jet during the Warm Season of 1993

    Source: Monthly Weather Review:;1997:;volume( 125 ):;issue: 009::page 2176
    Author:
    Arritt, Raymond W.
    ,
    Rink, Thomas D.
    ,
    Segal, Moti
    ,
    Todey, Dennis P.
    ,
    Clark, Craig A.
    ,
    Mitchell, Mark J.
    ,
    Labas, Kenneth M.
    DOI: 10.1175/1520-0493(1997)125<2176:TGPLLJ>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Hourly wind profiler observations from the NOAA Profiler Network were used to develop a climatology of the low-level jet (LLJ) over the Great Plains of the central United States from April to September of 1993. The peak precipitation episode of the 1993 flood was associated with a sustained period of high incidence of strong low-level jets (over 20 m s?1). Consistent with previous studies, strong low-level jets were found to be promoted in the warm sector of an extratropical cyclone. Comparison of datasets formulated using velocity variance thresholds with unthresholded data similar to the operational hourly data suggests that the profiler observations often were contaminated by radar returns from migrating birds, especially during the months of April and May. The strong low-level jets during the peak precipitation episode of the 1993 flood over the upper Mississippi River basin were associated with a high-amplitude upper-level wave pattern over and upstream of the continental United States. Separating the composite 850-mb wind for strong low-level jets into geostrophic and ageostrophic components showed that the magnitudes of the ageostrophic component and the anomalous geostrophic component were comparable.
    • Download: (811.3Kb)
    • Show Full MetaData Hide Full MetaData
    • Item Order
    • Go To Publisher
    • Price: 5000 Rial
    • Statistics

      The Great Plains Low-Level Jet during the Warm Season of 1993

    URI
    http://yetl.yabesh.ir/yetl1/handle/yetl/4203914
    Collections
    • Monthly Weather Review

    Show full item record

    contributor authorArritt, Raymond W.
    contributor authorRink, Thomas D.
    contributor authorSegal, Moti
    contributor authorTodey, Dennis P.
    contributor authorClark, Craig A.
    contributor authorMitchell, Mark J.
    contributor authorLabas, Kenneth M.
    date accessioned2017-06-09T16:11:30Z
    date available2017-06-09T16:11:30Z
    date copyright1997/09/01
    date issued1997
    identifier issn0027-0644
    identifier otherams-62964.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4203914
    description abstractHourly wind profiler observations from the NOAA Profiler Network were used to develop a climatology of the low-level jet (LLJ) over the Great Plains of the central United States from April to September of 1993. The peak precipitation episode of the 1993 flood was associated with a sustained period of high incidence of strong low-level jets (over 20 m s?1). Consistent with previous studies, strong low-level jets were found to be promoted in the warm sector of an extratropical cyclone. Comparison of datasets formulated using velocity variance thresholds with unthresholded data similar to the operational hourly data suggests that the profiler observations often were contaminated by radar returns from migrating birds, especially during the months of April and May. The strong low-level jets during the peak precipitation episode of the 1993 flood over the upper Mississippi River basin were associated with a high-amplitude upper-level wave pattern over and upstream of the continental United States. Separating the composite 850-mb wind for strong low-level jets into geostrophic and ageostrophic components showed that the magnitudes of the ageostrophic component and the anomalous geostrophic component were comparable.
    publisherAmerican Meteorological Society
    titleThe Great Plains Low-Level Jet during the Warm Season of 1993
    typeJournal Paper
    journal volume125
    journal issue9
    journal titleMonthly Weather Review
    identifier doi10.1175/1520-0493(1997)125<2176:TGPLLJ>2.0.CO;2
    journal fristpage2176
    journal lastpage2192
    treeMonthly Weather Review:;1997:;volume( 125 ):;issue: 009
    contenttypeFulltext
    DSpace software copyright © 2002-2015  DuraSpace
    نرم افزار کتابخانه دیجیتال "دی اسپیس" فارسی شده توسط یابش برای کتابخانه های ایرانی | تماس با یابش
    yabeshDSpacePersian
     
    DSpace software copyright © 2002-2015  DuraSpace
    نرم افزار کتابخانه دیجیتال "دی اسپیس" فارسی شده توسط یابش برای کتابخانه های ایرانی | تماس با یابش
    yabeshDSpacePersian