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    Wintertime Observations of Roll Clouds over the Bering Sea 

    Source: Monthly Weather Review:;1980:;volume( 108 ):;issue: 012:;page 2024
    Author(s): Walter, Bernard A.
    Publisher: American Meteorological Society
    Abstract: NOAA-4 satellite photos of roll clouds over the Bering Sea are used to derive quantitative information as to how the interval between the clouds (?) changes with distance south of the edge of the ice pack. Radiosondes are ...
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    Comma Cloud Development and Associated Rapid Cyclogenesis over the Gulf of Alaska: A Case Study Using Aircraft and Operational Data 

    Source: Monthly Weather Review:;1988:;volume( 116 ):;issue: 005:;page 1103
    Author(s): Businger, Steven; Walter, Bernard
    Publisher: American Meteorological Society
    Abstract: The NOAA P-3 aircraft was used to collect data in a genesis region for mesoscale comma clouds over the Gulf of Alaska. Aircraft measurements in the genesis region showed that rainbands with spacings of 65?75 km and ...
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    Analysis of Mesoscale Linear Features Observed in the Arctic Atmospheric Boundary Layer 

    Source: Monthly Weather Review:;1996:;volume( 124 ):;issue: 009:;page 1924
    Author(s): Mourad, Pierre D.; Walter, Bernard A.
    Publisher: American Meteorological Society
    Abstract: The existence of synoptically distributed, coherent, linear mesoscale features with wavelengths of 12?18 km in a shallow (zl ≈ 150 m) atmospheric boundary layer is documented. These were observed north of Alaska over the ...
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    Observations of Longitudinal Rolls in a Near Neutral Atmosphere 

    Source: Monthly Weather Review:;1984:;volume( 112 ):;issue: 001:;page 200
    Author(s): Walter, Bernard A.; Overland, James E.
    Publisher: American Meteorological Society
    Abstract: Aircraft and satellite data an used to study the structure of longitudinal roll vortices in a nearly neutral (zi/L=-1.2, where zi is the inversion height and L is the Monin-Obukhov length) boundary layer over the ice-covered ...
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    Gap Winds in the Strait of Juan de Fuca 

    Source: Monthly Weather Review:;1981:;volume( 109 ):;issue: 010:;page 2221
    Author(s): Overland, James E.; Walter, Bernard A.
    Publisher: American Meteorological Society
    Abstract: Gap winds can be defined as a flow of air in a sea level channel which accelerates under the influence of a pressure gradient parallel to the axis of the channel. In February 1980 two distinct cases of gap winds were ...
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    Response of Stratified Flow in the Lee of the Olympic Mountains 

    Source: Monthly Weather Review:;1982:;volume( 110 ):;issue: 010:;page 1458
    Author(s): Walter, Bernard A.; Overland, James E.
    Publisher: American Meteorological Society
    Abstract: The behavior of stratified air flowing around an isolated mountain is dependent on an internal Froude number (F), which indicates the relative importance of upstream velocity and vertical stratification. Three cases of the ...
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    Research Aircraft Observations of the Mean and Turbulent Structure of a Low-Level Jet Accompanying a Strong Storm 

    Source: Journal of Applied Meteorology:;2002:;volume( 041 ):;issue: 012:;page 1210
    Author(s): Bond, Nicholas A.; Walter, Bernard A.
    Publisher: American Meteorological Society
    Abstract: A NOAA P-3 research aircraft collected measurements in a storm off of the U.S. West Coast that featured a low-level jet with wind speeds approaching 50 m s?1. These measurements have been used to document mean and turbulent ...
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    The Structure of the Unstable Marine Boundary Layer Viewed by Lidar and Aircraft Observations 

    Source: Journal of the Atmospheric Sciences:;1986:;Volume( 043 ):;issue: 013:;page 1301
    Author(s): Atlas, David; Walter, Bernard; Chou, Shu-Hsien; Sheu, P. J.
    Publisher: American Meteorological Society
    Abstract: The combination of vertical lidar and in situ meteorological observations from two aircraft provide an unprecedented view of the marine atmospheric boundary layer (MABL) during a cold air outbreak. To a first approximation, ...
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