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    A Two-Dimensional Primitive Equation Model of Frontogenesis Forced by Confluence and Horizontal Shear 

    Source: Journal of the Atmospheric Sciences:;1985:;Volume( 042 ):;issue: 012:;page 1259
    Author(s): Keyser, Daniel; Pecnick, Michael J.
    Publisher: American Meteorological Society
    Abstract: A two-dimensional primitive equation model of frontogenesis forced by a combination of confluence and horizontal shear is formulated for dry, nearly adiabatic and inviscid conditions. The frontogenetical forcing mechanisms ...
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    Diagnosis of Ageostrophic Circulations in a Two-Dimensional Primitive Equation Model of Frontogenesis 

    Source: Journal of the Atmospheric Sciences:;1985:;Volume( 042 ):;issue: 012:;page 1283
    Author(s): Keyser, Daniel; Pecnick, Michael J.
    Publisher: American Meteorological Society
    Abstract: Diagnoses are presented of the transverse ageostrophic circulation patterns for two cases from a two-dimensional primitive equation model of frontogenesis forced by a combination of confluence and horizontal shear. The ...
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    The Effect of Along-front Temperature Variation in a Two-Dimensional Primitive Equation Model of Surface Frontogenesis 

    Source: Journal of the Atmospheric Sciences:;1987:;Volume( 044 ):;issue: 003:;page 577
    Author(s): Keyser, Daniel; Pecnick, Michael J.
    Publisher: American Meteorological Society
    Abstract: The development of frontal zones is examined in a two-dimensional primitive equation model of frontogenesis formulated for dry, nearly adiabatic and inviscid conditions. The model results are interpreted in the context of ...
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    Mechanics of a Strong Subsynoptic Gravity Wave Deduced from Satellite and Surface Observations 

    Source: Journal of the Atmospheric Sciences:;1984:;Volume( 041 ):;issue: 011:;page 1850
    Author(s): Pecnick, Michael J.; Young, John A.
    Publisher: American Meteorological Society
    Abstract: The three-dimensional structure and implied dynamics of a strong tropospheric gravity wave event am studied. It is shown that satellite and continuous surface observations reveal the subsynoptic nature of this ?wave of ...
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    Diagnosis of the Role of Vertical Deformation in a Two-Dimensional Primitive Equation Model of Upper-Level Frontogenesis 

    Source: Journal of the Atmospheric Sciences:;1986:;Volume( 043 ):;issue: 008:;page 839
    Author(s): Keyser, Daniel; Pecnick, Michael J.; Shapiro, M. A.
    Publisher: American Meteorological Society
    Abstract: Equations are developed for the temporal rates of change of the magnitudes of vector gradients of potential temperature and absolute momentum projected onto vertical planes transverse to straight frontal zones. Subject to ...
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    Changes to NMC's Regional Analysis and Forecast System 

    Source: Weather and Forecasting:;1991:;volume( 006 ):;issue: 001:;page 133
    Author(s): Petersen, Ralph A.; DiMego, Geoffrey J.; Hoke, James E.; Mitchell, Kenneth E.; Gerrity, Joseph P.; Wobus, Richard L.; Juang, Hann-Ming H.; Pecnick, Michael J.
    Publisher: American Meteorological Society
    Abstract: The final set of changes to NMC's Regional Analysis and Forecast System (RAFS) is described. The changes include modifications to both the forecast model and the analysis model, as well as development of a Regional Data ...
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