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    Source: Monthly Weather Review:;2017:;volume( 145 ):;issue: 010::page 3929
    Author:
    Haghi, Kevin R.;Parsons, David B.;Shapiro, Alan
    DOI: 10.1175/MWR-D-16-0415.1
    Publisher: American Meteorological Society
    Abstract: AbstractThis study documents atmospheric bores and other convergent boundaries in the southern Great Plains? nocturnal environment during the IHOP_2002 summer campaign. Observational evidence demonstrates that convective outflows routinely generate bores. Statistically resampled flow regimes, derived from an adaptation of hydraulic theory, agree well with observations. Specifically, convective outflows within the observed environments are likely to produce a partially blocked flow regime, which is a favorable condition for generating a bore. Once a bore develops, the direction of movement generally follows the orientation of the bulk shear vector between the nose of the nocturnal low-level jet and a height of 1.5 or 2.5 km AGL. This relationship is believed to be a consequence of wave trapping through the curvature of the horizontal wind with respect to height. This conclusion comes after analyzing the profile of the Scorer parameter. Overall, these findings provide an impetus for future investigations aimed at understanding and predicting nocturnal deep convection over this region.
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    contributor authorHaghi, Kevin R.;Parsons, David B.;Shapiro, Alan
    date accessioned2018-01-03T11:02:58Z
    date available2018-01-03T11:02:58Z
    date copyright6/29/2017 12:00:00 AM
    date issued2017
    identifier othermwr-d-16-0415.1.pdf
    identifier urihttp://138.201.223.254:8080/yetl1/handle/yetl/4246556
    description abstractAbstractThis study documents atmospheric bores and other convergent boundaries in the southern Great Plains? nocturnal environment during the IHOP_2002 summer campaign. Observational evidence demonstrates that convective outflows routinely generate bores. Statistically resampled flow regimes, derived from an adaptation of hydraulic theory, agree well with observations. Specifically, convective outflows within the observed environments are likely to produce a partially blocked flow regime, which is a favorable condition for generating a bore. Once a bore develops, the direction of movement generally follows the orientation of the bulk shear vector between the nose of the nocturnal low-level jet and a height of 1.5 or 2.5 km AGL. This relationship is believed to be a consequence of wave trapping through the curvature of the horizontal wind with respect to height. This conclusion comes after analyzing the profile of the Scorer parameter. Overall, these findings provide an impetus for future investigations aimed at understanding and predicting nocturnal deep convection over this region.
    publisherAmerican Meteorological Society
    typeJournal Paper
    journal volume145
    journal issue10
    journal titleMonthly Weather Review
    identifier doi10.1175/MWR-D-16-0415.1
    journal fristpage3929
    journal lastpage3946
    treeMonthly Weather Review:;2017:;volume( 145 ):;issue: 010
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
    نرم افزار کتابخانه دیجیتال "دی اسپیس" فارسی شده توسط یابش برای کتابخانه های ایرانی | تماس با یابش
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