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    Doppler Radar Measurements of Turbulent Kinetic Energy Dissipation Rates in a Northeastern Colorado Convective Storm

    Source: Journal of Applied Meteorology:;1976:;volume( 015 ):;issue: 009::page 1012
    Author:
    Frisch, A. S.
    ,
    Strauch, R. G.
    DOI: 10.1175/1520-0450(1976)015<1012:DRMOTK>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: In this paper we report the results of measurements of turbulent kinetic energy dissipation rates within a convective storm. The measurements were obtained with two Doppler radars, one scanning the storm from a distance at low elevation angles and the other pointing vertically with the storm passing overhead. With the scanning radar we measured the wind shear in the radial velocity field and the turbulent kinetic energy dissipation rates within the storm. These dissipation rates showed good agreement with those measured by the zenith-pointing radar data; dissipation rates ranged from 30 cm2 s?3 to greater than 3500 cm2 s?3 in the region between the updraft and downdraft.
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      Doppler Radar Measurements of Turbulent Kinetic Energy Dissipation Rates in a Northeastern Colorado Convective Storm

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4232603
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    contributor authorFrisch, A. S.
    contributor authorStrauch, R. G.
    date accessioned2017-06-09T17:38:45Z
    date available2017-06-09T17:38:45Z
    date copyright1976/09/01
    date issued1976
    identifier issn0021-8952
    identifier otherams-9147.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4232603
    description abstractIn this paper we report the results of measurements of turbulent kinetic energy dissipation rates within a convective storm. The measurements were obtained with two Doppler radars, one scanning the storm from a distance at low elevation angles and the other pointing vertically with the storm passing overhead. With the scanning radar we measured the wind shear in the radial velocity field and the turbulent kinetic energy dissipation rates within the storm. These dissipation rates showed good agreement with those measured by the zenith-pointing radar data; dissipation rates ranged from 30 cm2 s?3 to greater than 3500 cm2 s?3 in the region between the updraft and downdraft.
    publisherAmerican Meteorological Society
    titleDoppler Radar Measurements of Turbulent Kinetic Energy Dissipation Rates in a Northeastern Colorado Convective Storm
    typeJournal Paper
    journal volume15
    journal issue9
    journal titleJournal of Applied Meteorology
    identifier doi10.1175/1520-0450(1976)015<1012:DRMOTK>2.0.CO;2
    journal fristpage1012
    journal lastpage1017
    treeJournal of Applied Meteorology:;1976:;volume( 015 ):;issue: 009
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
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