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    Nonclassical Mesoscale Circulations Caused by Surface Sensible Heat-Flux Gradients 

    Source: Bulletin of the American Meteorological Society:;1992:;volume( 073 ):;issue: 010:;page 1593
    Author(s): Segal, M.; Arritt, R. W.
    Publisher: American Meteorological Society
    Abstract: Significant spatial heterogeneities of daytime surface sensible heat flux are common over land within mesoscale domains. Thermally induced circulations, similar to the sea/lake breeze [termed nonclassical mesoscale ...
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    On the Potential Impact of Daytime Surface Sensible Heat Flux on the Dissipation of Martian Cold Air Outbreaks 

    Source: Journal of the Atmospheric Sciences:;1997:;Volume( 054 ):;issue: 011:;page 1544
    Author(s): Segal, M.; Arritt, R. W.; Tillman, J. E.
    Publisher: American Meteorological Society
    Abstract: The Martian daytime soil surface temperature is governed primarily by the net irradiance balance and surface soil heat flux. Thus the outbreak of a cold air mass generates increased sensible heat flux that is conducive to ...
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    Sensitivity of Local Deep Convection Potential over Water Bodies to Sea Surface Temperature and Wind Speed 

    Source: Monthly Weather Review:;1994:;volume( 122 ):;issue: 009:;page 2210
    Author(s): Segal, M.; Mitchell, M. J.; Arritt, R. W.
    Publisher: American Meteorological Society
    Abstract: The sea surface temperature (SST), wind speed, and surface-layer thermal stability affect surface thermal fluxes that are conducive to deep convection. In the present study, numerical model sensitivity evaluations were ...
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    A Simple and Efficient Scheme for Performing One-and Two-Dimensional Numerical Model Sensitivity Experiments 

    Source: Monthly Weather Review:;1993:;volume( 121 ):;issue: 006:;page 1871
    Author(s): Segal, M.; Arritt, R. W.; Heim, J. E.
    Publisher: American Meteorological Society
    Abstract: A simple and efficient scheme for utilizing a virtual 3D mesoscale numerical model in 1D and 2D sensitivity studies is outlined. The scheme involves several straightforward adjustments in the model code that enable ...
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    Some Sensitivity Evaluations of Potential 2xCO2 Climate Impact on Deep Convection over Water Bodies 

    Source: Journal of Climate:;1994:;volume( 007 ):;issue: 006:;page 1014
    Author(s): Segal, M.; Mitchell, M. J.; Arritt, R. W.
    Publisher: American Meteorological Society
    Abstract: A boundary-layer numerical model was used to evaluate the impact of GCMs? predicted 2xCO2 climate on surface thermal fluxes over water bodies, in situations conducive to deep convection following short-range airmass ...
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    Sensitivity of Simulated Regional Surface Thermal Fluxes during Warm Advection Snowmelt to Selection of the Lowest Model Level Height 

    Source: Journal of Hydrometeorology:;2001:;Volume( 002 ):;issue: 004:;page 395
    Author(s): Wei, H.; Segal, M.; Gutowski, W. J.; Pan, Z.; Arritt, R. W.; Gallus, W. A.
    Publisher: American Meteorological Society
    Abstract: Under strong warm advection, sensible and latent heat fluxes may provide larger energy for surface snowmelt than does net radiation flux. With these thermally stable conditions, the height of the first model level may be ...
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    The Enhancement of Cold-Front Temperature Contrast by Differential Cloud Cover 

    Source: Monthly Weather Review:;1993:;volume( 121 ):;issue: 003:;page 867
    Author(s): Segal, M.; Physick, W. L.; Heim, J. E.; Arritt, R. W.
    Publisher: American Meteorological Society
    Abstract: The thermal impact of differential cloud shading across a cold front is evaluated briefly through conceptual, scaling, and numerical-modeling approaches. It is suggested that in summer the shading may enhance the boundary-layer ...
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    Some Observations of the Clearing of Cumulus Clouds Downwind from Snow-Covered Areas 

    Source: Monthly Weather Review:;1999:;volume( 127 ):;issue: 007:;page 1687
    Author(s): Segal, M.; Anderson, C.; Arritt, R. W.; Rabin, R. M.; Martin, D. W.
    Publisher: American Meteorological Society
    Abstract: Satellite images that illustrate the clearing of cumulus clouds downwind from snow-covered areas are presented. The cloud clearing resembles that occasionally observed with lakes during warm advection, supporting the ...
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    A Method to Determine Nonhydrostatic Effects within Subdomains in a Mesoscale Model 

    Source: Journal of the Atmospheric Sciences:;1985:;Volume( 042 ):;issue: 020:;page 2110
    Author(s): Song, J. L.; Pielke, R. A.; Segal, M.; Arritt, R. W.; Kessler, R. C.
    Publisher: American Meteorological Society
    Abstract: The exact solution of the nonhydrostatic pressure residual (total pressure perturbation minus hydrostatic pressure perturbation) in Defant's linear model is derived. The quasi-nonhydrostatic residual, introduced by Pielke, ...
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    Scaling Evaluation of the Effect of Surface Characteristics on Potential for Deep Convection over Uniform Terrain 

    Source: Monthly Weather Review:;1995:;volume( 123 ):;issue: 002:;page 383
    Author(s): Segal, M.; Arritt, R. W.; Clark, C.; Rabin, R.; Brown, J.
    Publisher: American Meteorological Society
    Abstract: The effect of surface characteristics on the daytime change in the potential for development of deep convection resulting from surface flux of heat and moisture is evaluated by conceptual, scaling, and numerical modeling ...
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