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    Characteristics of the Atmospheric Boundary Layer over a Tropical Station as Evidenced by Tethered Balloon Observations

    Source: Journal of Applied Meteorology:;1993:;volume( 032 ):;issue: 008::page 1426
    Author:
    Vernekar, K. G.
    ,
    Mohan, Brij
    ,
    Saxena, Sangeeta
    ,
    Patil, M. N.
    DOI: 10.1175/1520-0450(1993)032<1426:COTABL>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: A tethersonde observational program was conducted for eight days during February and March 1989 at Pune (18°32?N, 73°51?E, 559 m MSL), India, during daytime for the study of mixed-layer evolution. A surface- based nocturnal inversion of intensity 8?10 K (100 m)?1 was observed on most of the days. It takes about 2 h after sunrise for this inversion to start eroding and 4?5 h for complete erosion. Profiles of potential temperature, mixing ratio, and wind are discussed. Using Tennekes and Driedonks? convective boundary-layer model an average sensible heat flux of 129 W m?2 is estimated during morning hours, which is comparable to the flux value obtained by an earlier study using an eddy correlation technique at a nearby site during March and April.
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      Characteristics of the Atmospheric Boundary Layer over a Tropical Station as Evidenced by Tethered Balloon Observations

    URI
    http://yetl.yabesh.ir/yetl1/handle/yetl/4147238
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    • Journal of Applied Meteorology

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    contributor authorVernekar, K. G.
    contributor authorMohan, Brij
    contributor authorSaxena, Sangeeta
    contributor authorPatil, M. N.
    date accessioned2017-06-09T14:04:32Z
    date available2017-06-09T14:04:32Z
    date copyright1993/08/01
    date issued1993
    identifier issn0894-8763
    identifier otherams-11953.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4147238
    description abstractA tethersonde observational program was conducted for eight days during February and March 1989 at Pune (18°32?N, 73°51?E, 559 m MSL), India, during daytime for the study of mixed-layer evolution. A surface- based nocturnal inversion of intensity 8?10 K (100 m)?1 was observed on most of the days. It takes about 2 h after sunrise for this inversion to start eroding and 4?5 h for complete erosion. Profiles of potential temperature, mixing ratio, and wind are discussed. Using Tennekes and Driedonks? convective boundary-layer model an average sensible heat flux of 129 W m?2 is estimated during morning hours, which is comparable to the flux value obtained by an earlier study using an eddy correlation technique at a nearby site during March and April.
    publisherAmerican Meteorological Society
    titleCharacteristics of the Atmospheric Boundary Layer over a Tropical Station as Evidenced by Tethered Balloon Observations
    typeJournal Paper
    journal volume32
    journal issue8
    journal titleJournal of Applied Meteorology
    identifier doi10.1175/1520-0450(1993)032<1426:COTABL>2.0.CO;2
    journal fristpage1426
    journal lastpage1432
    treeJournal of Applied Meteorology:;1993:;volume( 032 ):;issue: 008
    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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