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    Strong Mixing Events Observed near the Tropopause with the MU Radar and High-Resolution Balloon Techniques

    Source: Journal of the Atmospheric Sciences:;2002:;Volume( 059 ):;issue: 020::page 2885
    Author:
    Luce, H.
    ,
    Fukao, S.
    ,
    Dalaudier, F.
    ,
    Crochet, M.
    DOI: 10.1175/1520-0469(2002)059<2885:SMEONT>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: In the present paper, strong isotropic radar echo enhancements are shown that are related to the existence of nearly statically neutralized layers (40?120 m thick) observed with high-resolution (10 cm) temperature measurements performed during the Middle and Upper Atmosphere Radar, Temperature Sheets and Interferometry (MUTSI) campaign (8?26 May 2000, Japan). These events have been observed in the immediate vicinity of the tropopause, just above a jet stream maximum. They most likely result from strong turbulent mixing generated by shear instabilities and could be one of the mechanisms responsible for the generation of strong temperature gradients (temperature gradient sheets) at the mixed layer edges. Further investigations will be necessary to evaluate the occurrence of this neutralization mechanism and its contribution to the generation of strong temperature gradient sheets within the free atmosphere.
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      Strong Mixing Events Observed near the Tropopause with the MU Radar and High-Resolution Balloon Techniques

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4159727
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    • Journal of the Atmospheric Sciences

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    contributor authorLuce, H.
    contributor authorFukao, S.
    contributor authorDalaudier, F.
    contributor authorCrochet, M.
    date accessioned2017-06-09T14:37:55Z
    date available2017-06-09T14:37:55Z
    date copyright2002/10/01
    date issued2002
    identifier issn0022-4928
    identifier otherams-23193.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4159727
    description abstractIn the present paper, strong isotropic radar echo enhancements are shown that are related to the existence of nearly statically neutralized layers (40?120 m thick) observed with high-resolution (10 cm) temperature measurements performed during the Middle and Upper Atmosphere Radar, Temperature Sheets and Interferometry (MUTSI) campaign (8?26 May 2000, Japan). These events have been observed in the immediate vicinity of the tropopause, just above a jet stream maximum. They most likely result from strong turbulent mixing generated by shear instabilities and could be one of the mechanisms responsible for the generation of strong temperature gradients (temperature gradient sheets) at the mixed layer edges. Further investigations will be necessary to evaluate the occurrence of this neutralization mechanism and its contribution to the generation of strong temperature gradient sheets within the free atmosphere.
    publisherAmerican Meteorological Society
    titleStrong Mixing Events Observed near the Tropopause with the MU Radar and High-Resolution Balloon Techniques
    typeJournal Paper
    journal volume59
    journal issue20
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(2002)059<2885:SMEONT>2.0.CO;2
    journal fristpage2885
    journal lastpage2896
    treeJournal of the Atmospheric Sciences:;2002:;Volume( 059 ):;issue: 020
    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
    yabeshDSpacePersian