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    Comments on “U. S. Navy Fleet Numerical Weather Central Operational Five-Level Fourth-Order Primitive-Equation Model” 

    Source: Monthly Weather Review:;1978:;volume( 106 ):;issue: 007:;page 1021
    Author(s): Kálnay-Rivas, Eugenia
    Publisher: American Meteorological Society
    Abstract: Although.there is some ambiguity in the description of the U.S. Navy Fleet fourth-order primitive-equation model developed by Mihok and Kaitala (1976), the finite differences used for the continuity equation and pressure ...
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    High-Latitude Truncation Errors of Box-Type Primitive Equation Models 

    Source: Monthly Weather Review:;1976:;volume( 104 ):;issue: 008:;page 1066
    Author(s): Kálnay-Rivas, Eugenia
    Publisher: American Meteorological Society
    Abstract: The ?box-type? finite-difference method includes a weighted average of the pressure gradient with weights proportional to the surface of the grid walls. It is shown that this averaging introduces first-order truncation ...
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    A Simple Mechanism for Blocking 

    Source: Journal of the Atmospheric Sciences:;1981:;Volume( 038 ):;issue: 010:;page 2077
    Author(s): Kalnay-Rivas, Eugenia; Merkine, Lee-Or
    Publisher: American Meteorological Society
    Abstract: Numerical experiments show that blocking in a barotropic atmosphere can occur as a resonant enhancement of Rossby lee waves forced by two stationary sources of potential vorticity. In particular, if an upstream source of ...
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    Rotating Stratified Flow over Finite Isolated Topography 

    Source: Journal of the Atmospheric Sciences:;1976:;Volume( 033 ):;issue: 006:;page 908
    Author(s): Merkine, Lee-Or; Kálnay-Rivas, Eugenia
    Publisher: American Meteorological Society
    Abstract: Inviscid, steady, stratified rotating flow over a finite, isolated topographic feature is critically analyzed. The formulation is based on approximating the horizontal momentum by the geostrophic momentum. A boundary value ...
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