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    Boundary Layer Adjustment as an Initial Value Problem 

    Source: Journal of the Atmospheric Sciences:;1968:;Volume( 025 ):;issue: 002:;page 207
    Author(s): Nickerson, Everett C.
    Publisher: American Meteorological Society
    Abstract: Previous investigations of boundary layer adjustment, such as those by Panofsky and Townsend, and more recently by Townsend, have been based upon similarity arguments. In this paper, however, the adjustment of a neutrally ...
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    The Role of Surface Friction in Downslope Windstorms 

    Source: Journal of Applied Meteorology:;1989:;volume( 028 ):;issue: 004:;page 241
    Author(s): Richard, Evelyne; Mascart, Patrick; Nickerson, Everett C.
    Publisher: American Meteorological Society
    Abstract: Numerical simulations of the 11 January 1972 windstorm in Boulder, Colorado, were carded out using a hydrostatic model with a turbulent kinetic energy parameterization to investigate the role of fictional effects in the ...
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    On the Existence of Atmospheric Vortices Downwind of Hawaii during the HAMEC Project 

    Source: Journal of Applied Meteorology:;1981:;volume( 020 ):;issue: 008:;page 868
    Author(s): Nickerson, Everett C.; Dias, Michael A.
    Publisher: American Meteorological Society
    Abstract: Aircraft observations west of the island of Hawaii in June 1980 during the Hawaii Mesoscale Energy and Climate (HAMEC) Project have provided the first in situ measurements of airflow within atmospheric vortices downwind ...
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    Surface Layer and Energy Budget Parameterizations for Mesoscale Models 

    Source: Journal of Applied Meteorology:;1975:;volume( 014 ):;issue: 003:;page 297
    Author(s): Nickerson, Everett C.; Smiley, Virginia E.
    Publisher: American Meteorological Society
    Abstract: A transcendental equation is presented for the Monin-Obukhov length L based upon (i) the Businger-Dyer surface layer formulations, (ii) parameterizations of the moisture flux, ground storage, and radiation terms in the ...
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    Numerical Simulation of Orographic Enhancement of Rain with a Mesoscale Model 

    Source: Journal of Climate and Applied Meteorology:;1987:;Volume( 026 ):;Issue: 006:;page 661
    Author(s): Richard, Evelyne; Chaumerliac, Nadine; Mahfouf, Jean Francois; Nickerson, Everett C.
    Publisher: American Meteorological Society
    Abstract: Orographic precipitation enhancement associated with the feeder mechanism proposed by Bergeron has been simulated using a two dimensions model based upon primitive equations including detailed parameter microphysics. A ...
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    The Numerical Simulation of Clouds, Rains and Airflow over the Vosges and Black Forest Mountains: A Meso-β Model with Parameterized Microphysics 

    Source: Monthly Weather Review:;1986:;volume( 114 ):;issue: 002:;page 398
    Author(s): Nickerson, Everett C.; Richard, Evelyne; Rosset, Robert; Smith, David R.
    Publisher: American Meteorological Society
    Abstract: A three-dimensional meso-? model with parameterized microphysics is presented. The model is capable of simulating orographically forced clouds, rain, and airflow. Tests using a two-dimensional version confirm the ability ...
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    Impact of Two Microphysical Schemes upon Gas Scavenging and Deposition in a Mesoscale Meteorological Model 

    Source: Journal of Applied Meteorology:;1991:;volume( 030 ):;issue: 001:;page 88
    Author(s): Chaumerliac, Nadine; Richard, Evelyne; Rosset, Robert; Nickerson, Everett C.
    Publisher: American Meteorological Society
    Abstract: Two widely used microphysical schemes are compared to evaluate their possible impact on wet deposition mechanisms. They are based upon different spectral distributions for raindrops (Marshall-Palmer and lognormal distributions) ...
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    The Influence of Vegetation on the Development and Structure of Mountain Waves 

    Source: Journal of Applied Meteorology:;1995:;volume( 034 ):;issue: 010:;page 2230
    Author(s): Romero, Romualdo; Alonso, Sergio; Nickerson, Everett C.; Ramis, Clemente
    Publisher: American Meteorological Society
    Abstract: The influence of vegetative cover on the development of mountain waves is analyzed using a two-dimensional meso-? model. The model includes a detailed representation of surface fluxes and friction that evolve in time as ...
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