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    The Sensitivity of the Nocturnal Minimum Temperature over Dry Terrain to Temperature and Humidity Changes Aloft 

    Source: Monthly Weather Review:;1980:;volume( 108 ):;issue: 003:;page 286
    Author(s): Gall, R. L.; Herman, B. M.
    Publisher: American Meteorological Society
    Abstract: The sensitivity of the nocturnal minimum temperature over dry soil under clear calm conditions to changes in the distribution of temperature and humidity aloft is estimated. To make the estimates, the minimum temperature ...
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    Hydrodynamic Instability of Small Eddies in a Tornado Vortex 

    Source: Journal of the Atmospheric Sciences:;1984:;Volume( 041 ):;issue: 003:;page 422
    Author(s): Staley, D. O.; Gall, R. L.
    Publisher: American Meteorological Society
    Abstract: A numerical method is shown for solving problems of nonaxisymmetric perturbations in incompressible, inviscid, swirling flow for arbitrary undisturbed azimuthal and axial flows. Exclusive attention is given to the hydrodynamic ...
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    On the Wavelength of Maximum Baroclinic Instability 

    Source: Journal of the Atmospheric Sciences:;1977:;Volume( 034 ):;issue: 011:;page 1679
    Author(s): Staley, D. O.; Gall, R. L.
    Publisher: American Meteorological Society
    Abstract: A four-level quasigeostrophic model of a baroclinic atmosphere is used to examine the instability of short (?2000 km) baroclinic waves. It is determined that only a slight decrease in the low-level static stability or ...
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    Barotropic Instability in a Tornado Vortex 

    Source: Journal of the Atmospheric Sciences:;1979:;Volume( 036 ):;issue: 006:;page 973
    Author(s): Staley, D. O.; Gall, R. L.
    Publisher: American Meteorological Society
    Abstract: The barotropic instability of a tornado described by Hoecker is investigated. It is found that wavenumbers of the order of 1 to 5 are significantly unstable, with growth rates of the order of 0.1 to 0.5 s?1, yielding ...
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    Gravity Waves Generated during Frontogenesis 

    Source: Journal of the Atmospheric Sciences:;1988:;Volume( 045 ):;issue: 015:;page 2204
    Author(s): Gall, R. L.; Williams, R. T.; Clark, T. L.
    Publisher: American Meteorological Society
    Abstract: Gravity waves forced by nonhydrostatic and nongeostrophic processes within a frontal zone are discussed. In particular, stationary waves immediately above and below the surface front are considered. The waves that appear ...
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    On the Minimum Scale of Surface Fronts 

    Source: Journal of the Atmospheric Sciences:;1987:;Volume( 044 ):;issue: 018:;page 2562
    Author(s): Gall, R. L.; Williams, R. T.; Clark, T. L.
    Publisher: American Meteorological Society
    Abstract: A series of numerical experiments of a surface front forced by stretching deformation using Clark's nonhydrostatic model at very high resolution is presented. These simulations are compared to those reported by Williams ...
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