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    Self-Organization and Maintenance of Simulated Nocturnal Convective Systems from PECAN 

    Source: Monthly Weather Review:;2021:;volume( 149 ):;issue: 004:;page 999
    Author(s): Parker, Matthew D.
    Publisher: American Meteorological Society
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    How Well Must Surface Vorticity Be Organized for Tornadogenesis? 

    Source: Journal of the Atmospheric Sciences:;2023:;volume( 080 ):;issue: 006:;page 1433
    Author(s): Parker, Matthew D.
    Publisher: American Meteorological Society
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    Simulated Convective Lines with Parallel Stratiform Precipitation. Part I: An Archetype for Convection in Along-Line Shear 

    Source: Journal of the Atmospheric Sciences:;2007:;Volume( 064 ):;issue: 002:;page 267
    Author(s): Parker, Matthew D.
    Publisher: American Meteorological Society
    Abstract: This article, the first of two describing convective lines with parallel stratiform (PS) precipitation, addresses the basic kinematic and precipitation features of these systems. The PS mode appears to be the preferred ...
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    Simulated Convective Lines with Parallel Stratiform Precipitation. Part II: Governing Dynamics and Associated Sensitivities 

    Source: Journal of the Atmospheric Sciences:;2007:;Volume( 064 ):;issue: 002:;page 289
    Author(s): Parker, Matthew D.
    Publisher: American Meteorological Society
    Abstract: This article is the second of two describing convective lines with parallel stratiform (PS) precipitation. The PS mode appears to be the preferred organizational structure in environments with line-parallel vertical wind ...
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    Impacts of Lapse Rates on Low-Level Rotation in Idealized Storms 

    Source: Journal of the Atmospheric Sciences:;2011:;Volume( 069 ):;issue: 002:;page 538
    Author(s): Parker, Matthew D.
    Publisher: American Meteorological Society
    Abstract: diabatic lapse rates appear to be a common feature in the lower troposphere on tornado days. This article reviews physical reasons why lapse rates may influence surface vortex intensification and reports on numerical ...
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    Relationship between System Slope and Updraft Intensity in Squall Lines 

    Source: Monthly Weather Review:;2010:;volume( 138 ):;issue: 009:;page 3572
    Author(s): Parker, Matthew D.
    Publisher: American Meteorological Society
    Abstract: In recent years there has been debate about whether squall lines have an ?optimal state.? It has been repeatedly demonstrated that the slope of a squall line?s convective region is related to the comparative magnitudes of ...
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    Comments on “A Comparison of Tropical and Midlatitude Thunderstorm Evolution in Response to Wind Shear” 

    Source: Journal of the Atmospheric Sciences:;2010:;Volume( 067 ):;issue: 005:;page 1700
    Author(s): Parker, Matthew D.
    Publisher: American Meteorological Society
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    Composite VORTEX2 Supercell Environments from Near-Storm Soundings 

    Source: Monthly Weather Review:;2013:;volume( 142 ):;issue: 002:;page 508
    Author(s): Parker, Matthew D.
    Publisher: American Meteorological Society
    Abstract: hree-dimensional composite analyses using 134 soundings from the second Verification of the Origins of Rotation in Tornadoes Experiment (VORTEX2) reveal the nature of near-storm variability in the environments of supercell ...
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    Response of Simulated Squall Lines to Low-Level Cooling 

    Source: Journal of the Atmospheric Sciences:;2008:;Volume( 065 ):;issue: 004:;page 1323
    Author(s): Parker, Matthew D.
    Publisher: American Meteorological Society
    Abstract: Organized convection has long been recognized to have a nocturnal maximum over the central United States. The present study uses idealized numerical simulations to investigate the mechanisms for the maintenance, propagation, ...
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    How Much Does “Backing Aloft” Actually Impact a Supercell? 

    Source: Weather and Forecasting:;2017:;volume( 032 ):;issue: 005:;page 1937
    Author(s): Parker, Matthew D.
    Publisher: American Meteorological Society
    Abstract: AbstractAmong forecasters and storm chasers, there is a common perception that hodographs with counterclockwise curvature or kinking in the midlevels (sometimes called backing aloft or veer?back?veer profiles) are unfavorable ...
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