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    TEMPERATURE CHANGES DURING FORMATION AND DISSIPATION OF WEST COAST STRATUS

    Source: Journal of Meteorology:;1944:;volume( 001 ):;issue: 001::page 29
    Author:
    Neiburger, Morris
    DOI: 10.1175/1520-0469(1944)001<0029:TCDFAD>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: At three-hourly intervals during three 24- to 48-hour periods in the summer of 1943, radiosonde observations were made at the University of California at Los Angeles; to ascertain the changes in vertical temperature distribution during typical stratus situations. These observations show that the base of the subsidence inversion characteristic of all summer soundings in this region undergoes marked diurnal variations in height and temperature. Computations show that advection can account for only part of the cooling at the inversion base during the formation of stratus over the station, while radiational exchange tends to raise the temperature there, rather than to lower it. Turbulence is shown to be practically negligible, and convection to play only a slight role. Vertical motion is found to account for the otherwise unexplained changes in temperature and inversion height. A possible cause of vertical motion with diurnal period is convergence in the land and sea breeze.
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      TEMPERATURE CHANGES DURING FORMATION AND DISSIPATION OF WEST COAST STRATUS

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4148980
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    contributor authorNeiburger, Morris
    date accessioned2017-06-09T14:09:35Z
    date available2017-06-09T14:09:35Z
    date copyright1944/09/01
    date issued1944
    identifier issn0095-9634
    identifier otherams-13520.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4148980
    description abstractAt three-hourly intervals during three 24- to 48-hour periods in the summer of 1943, radiosonde observations were made at the University of California at Los Angeles; to ascertain the changes in vertical temperature distribution during typical stratus situations. These observations show that the base of the subsidence inversion characteristic of all summer soundings in this region undergoes marked diurnal variations in height and temperature. Computations show that advection can account for only part of the cooling at the inversion base during the formation of stratus over the station, while radiational exchange tends to raise the temperature there, rather than to lower it. Turbulence is shown to be practically negligible, and convection to play only a slight role. Vertical motion is found to account for the otherwise unexplained changes in temperature and inversion height. A possible cause of vertical motion with diurnal period is convergence in the land and sea breeze.
    publisherAmerican Meteorological Society
    titleTEMPERATURE CHANGES DURING FORMATION AND DISSIPATION OF WEST COAST STRATUS
    typeJournal Paper
    journal volume1
    journal issue1
    journal titleJournal of Meteorology
    identifier doi10.1175/1520-0469(1944)001<0029:TCDFAD>2.0.CO;2
    journal fristpage29
    journal lastpage41
    treeJournal of Meteorology:;1944:;volume( 001 ):;issue: 001
    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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