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    Analytical Shear Statistics Based on Nocturnal Wind Profiles

    Source: Journal of Climate and Applied Meteorology:;1986:;Volume( 025 ):;Issue: 011::page 1507
    Author:
    Wittich, K-P.
    ,
    Hartmann, J.
    ,
    Roth, R.
    DOI: 10.1175/1520-0450(1986)025<1507:ASSBON>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: For a number of periods since 1978, wind and temperature profile measurements have been taken at two radio masts of 300 m height located in northern Germany. From wind profiles obtained during nocturnal conditions, wind shear data were calculated throughout the boundary layer for six layers of 25 m thickness. The data were analyzed taking into account dependencies on temperature gradients, geostrophic winds, local variations of kinetic energy and cooling rates. Minimum shear values were found for geostrophic winds about 5 m s?1 and strong shear values when the wind field was highly accelerated or decelerated and cooling rates were strong. In addition, increasing shear was found to be associated with increasing temperature gradients up to approximately 4 K per 100 m.
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      Analytical Shear Statistics Based on Nocturnal Wind Profiles

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    https://yetl.yabesh.ir/yetl1/handle/yetl/4146259
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    • Journal of Climate and Applied Meteorology

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    contributor authorWittich, K-P.
    contributor authorHartmann, J.
    contributor authorRoth, R.
    date accessioned2017-06-09T14:01:25Z
    date available2017-06-09T14:01:25Z
    date copyright1986/11/01
    date issued1986
    identifier issn0733-3021
    identifier otherams-11071.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4146259
    description abstractFor a number of periods since 1978, wind and temperature profile measurements have been taken at two radio masts of 300 m height located in northern Germany. From wind profiles obtained during nocturnal conditions, wind shear data were calculated throughout the boundary layer for six layers of 25 m thickness. The data were analyzed taking into account dependencies on temperature gradients, geostrophic winds, local variations of kinetic energy and cooling rates. Minimum shear values were found for geostrophic winds about 5 m s?1 and strong shear values when the wind field was highly accelerated or decelerated and cooling rates were strong. In addition, increasing shear was found to be associated with increasing temperature gradients up to approximately 4 K per 100 m.
    publisherAmerican Meteorological Society
    titleAnalytical Shear Statistics Based on Nocturnal Wind Profiles
    typeJournal Paper
    journal volume25
    journal issue11
    journal titleJournal of Climate and Applied Meteorology
    identifier doi10.1175/1520-0450(1986)025<1507:ASSBON>2.0.CO;2
    journal fristpage1507
    journal lastpage1517
    treeJournal of Climate and Applied Meteorology:;1986:;Volume( 025 ):;Issue: 011
    contenttypeFulltext
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