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    Observations and Mixed-Layer Modeling of a Terrain-Induced Mesoscale Gyre: The Denver Cyclone 

    Source: Monthly Weather Review:;1988:;volume( 116 ):;issue: 008:;page 1599
    Author(s): Wilczak, J. M.; Glendening, J. W.
    Publisher: American Meteorological Society
    Abstract: In northeastern Colorado a frequently observed feature of the surface wind field is a stationary, terrain-induced mesoscale gyre, which is often associated with the formation of severe weather. Because of the gyre's proximity ...
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    Observations and Mixed-Layer Modeling of a Terrain-Induced Mesoscale Gyre: The Denver Cyclone 

    Source: Monthly Weather Review:;1988:;volume( 116 ):;issue: 012:;page 2688
    Author(s): Wilczak, J. M.; Glendening, J. W.
    Publisher: American Meteorological Society
    Abstract: In northeastern Colorado a frequently observed feature of the surface wind field is a stationary, terrain-induced mesoscale gyre, which is often associated with the formation of severe weather. Because of the gyre/s proximity ...
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    Boundary-Layer Transition across a Stratocumulus Cloud Edge in a Coastal Zone 

    Source: Monthly Weather Review:;1991:;volume( 119 ):;issue: 010:;page 2337
    Author(s): Skupniewicz, C. E.; Glendening, J. W.; Kamada, R. F.
    Publisher: American Meteorological Society
    Abstract: We examine the lateral transition from a stratocumulus-covered boundary layer to a clear-sky convective boundary layer during onshore flow in a coastal environment, using both mobile sodar observations and a numerical ...
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