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    Barotropic and Baroclinic Ageostrophic Winds and Completeness of Solution for the Psi Equations 

    Source: Journal of the Atmospheric Sciences:;1993:;Volume( 050 ):;issue: 004:;page 588
    Author(s): Xu, Qin; Keyser, Daniel
    Publisher: American Meteorological Society
    Abstract: This paper examines the completeness of the solutions for three-dimensional ageostrophic circulations determined from the quasigeostrophic psi equations (or from the counterpart semigeostrophic psi equations in ...
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    On the Formation of Potential-Vorticity Anomalies in Upper-Level Jet-Front Systems 

    Source: Monthly Weather Review:;1990:;volume( 118 ):;issue: 009:;page 1914
    Author(s): Keyser, Daniel; Rotunno, Richard
    Publisher: American Meteorological Society
    Abstract: We review and discuss a difference in interpretation of the role of turbulence in modifying the potential-vorticity distribution in the vicinity of upper-level jet-front systems. In the late 1970s, M. A. Shapiro presented ...
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    A Climatology of Extratropical Cyclones Leading to Extreme Weather Events over Central and Eastern North America 

    Source: Monthly Weather Review:;2019:;volume 147:;issue 005:;page 1471
    Author(s): Bentley, Alicia M.; Bosart, Lance F.; Keyser, Daniel
    Publisher: American Meteorological Society
    Abstract: AbstractCool-season extreme weather events (EWEs) (i.e., high-impact weather events that are societally disruptive, geographically widespread, exceptionally prolonged, and climatologically infrequent) are typically associated ...
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    Balanced and Unbalanced Upper-Level Frontogenesis 

    Source: Journal of the Atmospheric Sciences:;1988:;Volume( 045 ):;issue: 022:;page 3366
    Author(s): Reeder, Michael J.; Keyser, Daniel
    Publisher: American Meteorological Society
    Abstract: The dynamics of frontogenesis at upper levels are investigated using a hierarchy of three numerical models. They are, in order of decreasing sophistication, the anelastic (AN), the geostrophic momentum (GM), and the ...
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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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    Regional Models: Emerging Research Tools for Synoptic Meteorologists 

    Source: Bulletin of the American Meteorological Society:;1987:;volume( 068 ):;issue: 004:;page 306
    Author(s): Keyser, Daniel; Uccellini, Louis W.
    Publisher: American Meteorological Society
    Abstract: Although the development of limited-area, regional-scale numerical-weather prediction models has been driven largely by the practical need to improve quantitative precipitation forecasts, a related motivation has been ...
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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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    Shear and Curvature vorticity and Potential-Vorticity Interchanges: Interpretation and Application to a Cutoff Cyclone Event 

    Source: Monthly Weather Review:;1993:;volume( 121 ):;issue: 001:;page 76
    Author(s): Bell, Gerald D.; Keyser, Daniel
    Publisher: American Meteorological Society
    Abstract: Equations are presented for the evolution of isobaric shear and curvature vorticity and for isentropic shear and curvature potential vorticity in natural (streamline-following) coordinates, in the case of adiabatic, ...
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    Tests of a Fine-Mesh Model over Europe and the United States 

    Source: Monthly Weather Review:;1979:;volume( 107 ):;issue: 008:;page 963
    Author(s): Anthes, Richard A.; Keyser, Daniel
    Publisher: American Meteorological Society
    Abstract: Thirty?two 24 h forecasts have been run over western Europe and the eastern United States using a six-layer, 60 km mesh primitive equation model. The forecasts show considerable skill in forecasting cyclogenesis over the ...
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