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    Surface Roughness and Internal Boundary Layer Near a Coastline

    Source: Journal of Applied Meteorology:;1972:;volume( 011 ):;issue: 004::page 658
    Author:
    Echols, W. T.
    ,
    Wagner, N. K.
    DOI: 10.1175/1520-0450(1972)011<0658:SRAIBL>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Wind profile observations obtained at two sites near the upper Texas coast during onshore winds in June 1968 are used to determine local toughness parameters. Values of 3?4 cm are obtained at a 32 m tower site 90 m inland and 0.81?1.5 cm at 4.8 km inland; both are in close agreement with results of others for similar terrain. The portion of the wind profile obtained at heights between 6.7 and 27 m near the beach is extrapolated downward to obtain a roughness between 0,0001 and 0.0003 cm for the Gulf of Mexico. An internal boundary layer was detected from the data obtained 90 m inland. The mean height was observed to he 6.7 m? a value associated with a mean slope of about 1:13 for an internal boundary originating at the upwind shoreline roughness discontinuity. Daytime values for the internal boundary height are somewhat higher than the mean, averaging 7.2 m, while the nighttime mean is 5.9 m. The data also suggest a wind speed dependence on the height of the internal boundary layer.
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      Surface Roughness and Internal Boundary Layer Near a Coastline

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4227000
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    contributor authorEchols, W. T.
    contributor authorWagner, N. K.
    date accessioned2017-06-09T17:21:24Z
    date available2017-06-09T17:21:24Z
    date copyright1972/06/01
    date issued1972
    identifier issn0021-8952
    identifier otherams-8374.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4227000
    description abstractWind profile observations obtained at two sites near the upper Texas coast during onshore winds in June 1968 are used to determine local toughness parameters. Values of 3?4 cm are obtained at a 32 m tower site 90 m inland and 0.81?1.5 cm at 4.8 km inland; both are in close agreement with results of others for similar terrain. The portion of the wind profile obtained at heights between 6.7 and 27 m near the beach is extrapolated downward to obtain a roughness between 0,0001 and 0.0003 cm for the Gulf of Mexico. An internal boundary layer was detected from the data obtained 90 m inland. The mean height was observed to he 6.7 m? a value associated with a mean slope of about 1:13 for an internal boundary originating at the upwind shoreline roughness discontinuity. Daytime values for the internal boundary height are somewhat higher than the mean, averaging 7.2 m, while the nighttime mean is 5.9 m. The data also suggest a wind speed dependence on the height of the internal boundary layer.
    publisherAmerican Meteorological Society
    titleSurface Roughness and Internal Boundary Layer Near a Coastline
    typeJournal Paper
    journal volume11
    journal issue4
    journal titleJournal of Applied Meteorology
    identifier doi10.1175/1520-0450(1972)011<0658:SRAIBL>2.0.CO;2
    journal fristpage658
    journal lastpage662
    treeJournal of Applied Meteorology:;1972:;volume( 011 ):;issue: 004
    contenttypeFulltext
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