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    Late-Morning Jump in TKE in the Mixed Layer over a Mountain Basin 

    Source: Journal of the Atmospheric Sciences:;1985:;Volume( 042 ):;issue: 004:;page 407
    Author(s): Banta, Robert M.
    Publisher: American Meteorological Society
    Abstract: The turbulence or ?gustiness? of the winds new the surface in a mountain valley increases sharply after the nocturnal inversion layer dissipates, normally in the late morning or early afternoon. This increase?almost all ...
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    Vertical Wind Velocities from Superpressure Balloons: A Case Study using Eole Data 

    Source: Monthly Weather Review:;1976:;volume( 104 ):;issue: 005:;page 628
    Author(s): Banta, Robert M.
    Publisher: American Meteorological Society
    Abstract: A method for determining vertical wind velocities (&?) using the pressure-and temperature?change data from superpressure(constant?density) balloons was proposed in an earlier paper. In this paper, we present a case study ...
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    Sea Breezes Shallow and Deep on the California Coast 

    Source: Monthly Weather Review:;1995:;volume( 123 ):;issue: 012:;page 3614
    Author(s): Banta, Robert M.
    Publisher: American Meteorological Society
    Abstract: Analyses of Doppler lidar data reveal sea breezes occurring on two different depth and time scales at Monterey Bay, California, on a day with offshore gradient flow indicated before sunrise and after sunset. The lidar data ...
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    Daytime Boundary-Layer Evolution over Mountainous Terrain. Part 1: Observations of the Dry Circulations 

    Source: Monthly Weather Review:;1984:;volume( 112 ):;issue: 002:;page 340
    Author(s): Banta, Robert M.
    Publisher: American Meteorological Society
    Abstract: This paper presents the boundary layer structure which accompanies the development of daytime local wind systems in a broad mountain valley, as revealed by cross sections of potential temperature. It describes how this ...
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    Daytime Boundary Layer Evolution over Mountainous Terrain. Part II: Numerical Studies of Upslope Flow Duration 

    Source: Monthly Weather Review:;1986:;volume( 114 ):;issue: 006:;page 1112
    Author(s): Banta, Robert M.
    Publisher: American Meteorological Society
    Abstract: Numerical simulators of upslope flow forming on the lee side of a heated mountain ridge showed this flow to be a transient phenomenon, in agreement with observations. The simulations, performed with a two-dimensional, dry ...
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    Assimilating Coherent Doppler Lidar Measurements into a Model of the Atmospheric Boundary Layer. Part I: Algorithm Development and Sensitivity to Measurement Error 

    Source: Journal of Atmospheric and Oceanic Technology:;2004:;volume( 021 ):;issue: 009:;page 1328
    Author(s): Newsom, Rob K.; Banta, Robert M.
    Publisher: American Meteorological Society
    Abstract: A four-dimensional variational data assimilation (4DVAR) algorithm for retrieval of spatially and temporally resolved velocity and thermodynamic fields within the atmospheric boundary layer (ABL) is described and applied ...
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    Assimilating Coherent Doppler Lidar Measurements into a Model of the Atmospheric Boundary Layer. Part II: Sensitivity Analyses 

    Source: Journal of Atmospheric and Oceanic Technology:;2004:;volume( 021 ):;issue: 012:;page 1809
    Author(s): Newsom, Rob K.; Banta, Robert M.
    Publisher: American Meteorological Society
    Abstract: A series of trials are performed to evaluate the sensitivity of a 4DVAR algorithm for retrieval of microscale wind and temperature fields from single-Doppler lidar data. These trials use actual Doppler lidar measurements ...
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    Stable Boundary Layer Depth from High-Resolution Measurements of the Mean Wind Profile 

    Source: Journal of Applied Meteorology and Climatology:;2010:;volume( 049 ):;issue: 001:;page 20
    Author(s): Pichugina, Yelena L.; Banta, Robert M.
    Publisher: American Meteorological Society
    Abstract: The depth h of the stable boundary layer (SBL) has long been an elusive measurement. In this diagnostic study the use of high-quality, high-resolution (?z = 10 m) vertical profile data of the mean wind U(z) and streamwise ...
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    Thunderstorm Genesis Zones in the Colorado Rocky Mountains as Determined by Traceback of Geosynchronous Satellite Images 

    Source: Monthly Weather Review:;1987:;volume( 115 ):;issue: 002:;page 463
    Author(s): Banta, Robert M.; Barker Schaaf, Crystal
    Publisher: American Meteorological Society
    Abstract: Mountain thunderstorms often originate in preferred regions of the topography, as shown qualitatively by pilot reports and more quantitatively by meteorological radar, satellite, and lightning detector studies. To further ...
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    Shear-Flow Instability in the Stable Nocturnal Boundary Layer as Observed by Doppler Lidar during CASES-99 

    Source: Journal of the Atmospheric Sciences:;2003:;Volume( 060 ):;issue: 001:;page 16
    Author(s): Newsom, Rob K.; Banta, Robert M.
    Publisher: American Meteorological Society
    Abstract: This study investigates a shear-flow instability observed in the stably stratified nighttime boundary layer on 6 October 1999 during the Cooperative Atmosphere?Surface Exchange Study (CASES-99) in south-central Kansas. A ...
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