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    Evolution of the Surface Wind Field in an Intensifying Tropical Cyclone 

    Source: Journal of the Atmospheric Sciences:;1985:;Volume( 042 ):;issue: 024:;page 2865
    Author(s): Molinari, John; Skubis, Steven
    Publisher: American Meteorological Society
    Abstract: The surface wind field in a developing tropical cyclone (Agnes, 1972) was analyzed over a 1660 km radius for four days using conventional surface data, as the storm evolved from a disorganized depression to a hurricane. ...
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    Calculation of Consistent Flux and Advective Terms from Adjusted Vertical Profiles of Divergence 

    Source: Monthly Weather Review:;1988:;volume( 116 ):;issue: 010:;page 1829
    Author(s): Molinari, John; Skubis, Steven
    Publisher: American Meteorological Society
    Abstract: A simple framework is presented for adjusting the normal wind components in a polygon of data points which produces a vanishing vertical integral of horizontal divergence, allows correct calculation of flux and advective ...
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    External Influences on Hurricane Intensity. Part III: Potential Vorticity Structure 

    Source: Journal of the Atmospheric Sciences:;1995:;Volume( 052 ):;issue: 020:;page 3593
    Author(s): Molinari, John; Skubis, Steven; Vollaro, David
    Publisher: American Meteorological Society
    Abstract: The interaction of Hurricane Elena (1985) with a baroclinic wave was reexamined using both potential vorticity (PV) and a formulation for Eliassen-Palm fluxes in cylindrical coordinates. The hurricane began to deepen rapidly ...
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    Application of the Eliassen Balanced Model to Real-Data Tropical Cyclones 

    Source: Monthly Weather Review:;1993:;volume( 121 ):;issue: 008:;page 2409
    Author(s): Molinari, John; Vollaro, David; Skubis, Steven
    Publisher: American Meteorological Society
    Abstract: The Eliassen balanced vortex model assumes gradient balance of the azimuthal mean flow. This assumption was tested by calculating mean and eddy terms in the radial momentum equation in the synoptic-scale environments of ...
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    Potential Vorticity, Easterly Waves, and Eastern Pacific Tropical Cyclogenesis 

    Source: Monthly Weather Review:;1997:;volume( 125 ):;issue: 010:;page 2699
    Author(s): Molinari, John; Knight, David; Dickinson, Michael; Vollaro, David; Skubis, Steven
    Publisher: American Meteorological Society
    Abstract: A significant sign reversal in the meridional potential vorticity gradient was found during the summer of 1991 on the 310-K isentropic surface (near 700 mb) over the Caribbean Sea. The Charney?Stern necessary condition for ...
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    Origins and Mechanisms of Eastern Pacific Tropical Cyclogenesis: A Case Study 

    Source: Monthly Weather Review:;2000:;volume( 128 ):;issue: 001:;page 125
    Author(s): Molinari, John; Vollaro, David; Skubis, Steven; Dickinson, Michael
    Publisher: American Meteorological Society
    Abstract: The genesis of Hurricane Hernan (1996) in the eastern Pacific was investigated using gridded analyses from the European Centre for Medium-Range Weather Forecasts and gridded outgoing longwave radiation. Hernan developed ...
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    Mountain Waves over Mont Blanc: Influence of a Stagnant Boundary Layer 

    Source: Journal of the Atmospheric Sciences:;2002:;Volume( 059 ):;issue: 013:;page 2073
    Author(s): Smith, Ronald B.; Skubis, Steven; Doyle, James D.; Broad, Adrian S.; Kiemle, Christoph; Volkert, Hans
    Publisher: American Meteorological Society
    Abstract: A stationary mountain wave, embedded in southwesterly flow over Mont Blanc in the Alps, was observed simultaneously by three research aircraft and three types of remote sensing: GPS dropsondes, airborne light detecting and ...
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