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    Dynamics of the Sea Breeze in the Atmospheric Boundary Layer: A Case Study of the Free Convection Regime

    Source: Monthly Weather Review:;1973:;volume( 101 ):;issue: 003::page 187
    Author:
    HSU, SHIH-ANG
    DOI: 10.1175/1520-0493(1973)101<0187:DOTSBI>2.3.CO;2
    Publisher: American Meteorological Society
    Abstract: Simultaneous measurements of temperature and wind profiles in the surface boundary layer (below 10-m elevation over a beach and below 100-m elevation over an inland site) under the effect of the sea breeze were made near Fort Walton Beach, Fla. We found that the sea breeze in the atmospheric boundary layer is in the free convection regime and that observed sea-breeze wind and temperature profiles behave according to minus one-third power laws. These experiments also substantiate evidence that the Prandtl-Obukhov-Priestley prediction of the free convection regime is a valid one under appropriate atmospheric conditions.
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      Dynamics of the Sea Breeze in the Atmospheric Boundary Layer: A Case Study of the Free Convection Regime

    URI
    http://yetl.yabesh.ir/yetl1/handle/yetl/4198977
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    • Monthly Weather Review

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    contributor authorHSU, SHIH-ANG
    date accessioned2017-06-09T16:00:12Z
    date available2017-06-09T16:00:12Z
    date copyright1973/03/01
    date issued1973
    identifier issn0027-0644
    identifier otherams-58521.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4198977
    description abstractSimultaneous measurements of temperature and wind profiles in the surface boundary layer (below 10-m elevation over a beach and below 100-m elevation over an inland site) under the effect of the sea breeze were made near Fort Walton Beach, Fla. We found that the sea breeze in the atmospheric boundary layer is in the free convection regime and that observed sea-breeze wind and temperature profiles behave according to minus one-third power laws. These experiments also substantiate evidence that the Prandtl-Obukhov-Priestley prediction of the free convection regime is a valid one under appropriate atmospheric conditions.
    publisherAmerican Meteorological Society
    titleDynamics of the Sea Breeze in the Atmospheric Boundary Layer: A Case Study of the Free Convection Regime
    typeJournal Paper
    journal volume101
    journal issue3
    journal titleMonthly Weather Review
    identifier doi10.1175/1520-0493(1973)101<0187:DOTSBI>2.3.CO;2
    journal fristpage187
    journal lastpage194
    treeMonthly Weather Review:;1973:;volume( 101 ):;issue: 003
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
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