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    Evaluation of Soil Moisture Effects on the Generation and Modification of Mesoscale Circulations

    Source: Monthly Weather Review:;1984:;volume( 112 ):;issue: 011::page 2281
    Author:
    Ookouchi, Y.
    ,
    Segal, M.
    ,
    Kessler, R. C.
    ,
    Pielke, R. A.
    DOI: 10.1175/1520-0493(1984)112<2281:EOSMEO>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: The current study provides an evaluation of thermally induced circulation over flat terrain due to nonuniform horizontal distribution of soil moisture availability. Additionally, the effect of soil moisture availability on the thermally induced upslope flow during the daylight hours is examined. The results indicate that in flat terrain, which has a nonhomogeneous moisture availability, the intensity of thermal circulations approaches that of sea-breeze circulations for the case of large contrasts. Even small amounts of water in thesoil, adjacent to dry areas, can still result in a significant mesoscale flow. The upslope flow has been indicated to be perturbed significantly when the moisture availability ii~creases or when the horizontal contrast of soil moisture availability becomes large.
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      Evaluation of Soil Moisture Effects on the Generation and Modification of Mesoscale Circulations

    URI
    http://yetl.yabesh.ir/yetl1/handle/yetl/4201227
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    • Monthly Weather Review

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    contributor authorOokouchi, Y.
    contributor authorSegal, M.
    contributor authorKessler, R. C.
    contributor authorPielke, R. A.
    date accessioned2017-06-09T16:05:06Z
    date available2017-06-09T16:05:06Z
    date copyright1984/11/01
    date issued1984
    identifier issn0027-0644
    identifier otherams-60545.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4201227
    description abstractThe current study provides an evaluation of thermally induced circulation over flat terrain due to nonuniform horizontal distribution of soil moisture availability. Additionally, the effect of soil moisture availability on the thermally induced upslope flow during the daylight hours is examined. The results indicate that in flat terrain, which has a nonhomogeneous moisture availability, the intensity of thermal circulations approaches that of sea-breeze circulations for the case of large contrasts. Even small amounts of water in thesoil, adjacent to dry areas, can still result in a significant mesoscale flow. The upslope flow has been indicated to be perturbed significantly when the moisture availability ii~creases or when the horizontal contrast of soil moisture availability becomes large.
    publisherAmerican Meteorological Society
    titleEvaluation of Soil Moisture Effects on the Generation and Modification of Mesoscale Circulations
    typeJournal Paper
    journal volume112
    journal issue11
    journal titleMonthly Weather Review
    identifier doi10.1175/1520-0493(1984)112<2281:EOSMEO>2.0.CO;2
    journal fristpage2281
    journal lastpage2292
    treeMonthly Weather Review:;1984:;volume( 112 ):;issue: 011
    contenttypeFulltext
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