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    Wind Disturbance by a Vertical Cylinder in the Atmospheric Surface Layer

    Source: Journal of Applied Meteorology:;1968:;volume( 007 ):;issue: 003::page 367
    Author:
    Dabberdt, Walter F.
    DOI: 10.1175/1520-0450(1968)007<0367:WDBAVC>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: The velocity distribution in the neighborhood of a cylindrical obstacle was measured over the frozen surface of Lake Mendota, Madison, Wis. Non-dimensional isotach patterns were constructed depicting the velocity distribution at two levels within the atmospheric surface layer. Differences in the vertical shear between the two levels is seen to affect the nature of the patterns. Wind speed reductions of 6% are noted upwind of the cylinder and in excess of 40% downwind. The upwind pattern is fairly well represented by the potential solution; the more complex downwind pattern is asymmetrical. Large vertical components of the velocity were computed.
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      Wind Disturbance by a Vertical Cylinder in the Atmospheric Surface Layer

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4219133
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    contributor authorDabberdt, Walter F.
    date accessioned2017-06-09T16:56:01Z
    date available2017-06-09T16:56:01Z
    date copyright1968/06/01
    date issued1968
    identifier issn0021-8952
    identifier otherams-7666.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4219133
    description abstractThe velocity distribution in the neighborhood of a cylindrical obstacle was measured over the frozen surface of Lake Mendota, Madison, Wis. Non-dimensional isotach patterns were constructed depicting the velocity distribution at two levels within the atmospheric surface layer. Differences in the vertical shear between the two levels is seen to affect the nature of the patterns. Wind speed reductions of 6% are noted upwind of the cylinder and in excess of 40% downwind. The upwind pattern is fairly well represented by the potential solution; the more complex downwind pattern is asymmetrical. Large vertical components of the velocity were computed.
    publisherAmerican Meteorological Society
    titleWind Disturbance by a Vertical Cylinder in the Atmospheric Surface Layer
    typeJournal Paper
    journal volume7
    journal issue3
    journal titleJournal of Applied Meteorology
    identifier doi10.1175/1520-0450(1968)007<0367:WDBAVC>2.0.CO;2
    journal fristpage367
    journal lastpage371
    treeJournal of Applied Meteorology:;1968:;volume( 007 ):;issue: 003
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
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