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    Models for Crenulation of a Converging Shell 

    Source: Journal of Fluids Engineering:;2014:;volume( 136 ):;issue: 008:;page 84501
    Author(s): Margolin, Len G.; Andrews, Malcolm J.
    Publisher: The American Society of Mechanical Engineers (ASME)
    Abstract: We describe two models for the growth of perturbations on the inner surface of a converging shell: one for a solid shell and one for a shell of incompressible fluid. We consider the cases of both cylindrically and spherically ...
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    Dispersive–Dissipative Eddy Parameterization in a Barotropic Model 

    Source: Journal of Physical Oceanography:;2001:;Volume( 031 ):;issue: 008:;page 2525
    Author(s): Nadiga, Balasubramanya T.; Margolin, Len G.
    Publisher: American Meteorological Society
    Abstract: Recently a new class of coarse-grained equations, known as α models, have been proposed for the mean motion of an ideal incompressible fluid. The use of one such model to represent the time-mean component of a turbulent ...
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    A Class of Nonhydrostatic Global Models 

    Source: Journal of the Atmospheric Sciences:;2001:;Volume( 058 ):;issue: 004:;page 349
    Author(s): Smolarkiewicz, Piotr K.; Margolin, Len G.; Wyszogrodzki, Andrzej A.
    Publisher: American Meteorological Society
    Abstract: A Cartesian, small- to mesoscale nonhydrostatic model is extended to a rotating mountainous sphere, thereby dispensing with the traditional geophysical simplifications of hydrostaticity, gentle terrain slopes, and weak ...
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    On Forward-in-Time Differencing for Fluids: Stopping Criteria for Iterative Solutions of Anelastic Pressure Equations 

    Source: Monthly Weather Review:;1997:;volume( 125 ):;issue: 004:;page 647
    Author(s): Smolarkiewicz, Piotr K.; Grubis̄ić, Vanda; Margolin, Len G.
    Publisher: American Meteorological Society
    Abstract: In this note, the authors address the practical issue of selecting appropriate stopping criteria for iterative solutions to the elliptic pressure equation arising in nonoscillatory, forward-in-time Eulerian and semi-Lagrangian ...
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