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    The Surface-Wind Response to Transient Mesoscale Pressure Fields Associated with Squall Lines 

    Source: Monthly Weather Review:;1992:;volume( 120 ):;issue: 009:;page 1837
    Author(s): Vescio, Michael D.; Johnson, Richard H.
    Publisher: American Meteorological Society
    Abstract: The two most prominent surface pressure features associated with squall lines are 1) a surface mesohigh, centered within the heavy-rain region, and 2) a wake low, located at the back edge of the trailing area of light ...
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    FORECASTER’S FORUM: Subjective Tornado Probability Forecasts in Severe Weather Watches 

    Source: Weather and Forecasting:;2001:;volume( 016 ):;issue: 001:;page 192
    Author(s): Vescio, Michael D.; Thompson, Richard L.
    Publisher: American Meteorological Society
    Abstract: An experiment was conducted at the Storm Prediction Center (SPC) to assess the accuracy of subjective probability forecasts for tornadoes within individual convective watch areas. Probability forecasts for one or more and ...
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    Near-Tropopause Vertical Motion within the Trailing Stratiform Region of a Midlatitude Squall Line 

    Source: Journal of the Atmospheric Sciences:;1989:;Volume( 047 ):;issue: 018:;page 2200
    Author(s): Johnson, Richard H.; Gallus, William A.; Vescio, Michael D.
    Publisher: American Meteorological Society
    Abstract: Rawinsonde observations have been used to determine the flow structure in the vicinity of the tropopause atop the trailing stratiform precipitation region of an intense midlatitude squall line. Computations of vertical ...
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    Storm Prediction Center Forecasting Issues Related to the 3 May 1999 Tornado Outbreak 

    Source: Weather and Forecasting:;2002:;volume( 017 ):;issue: 003:;page 544
    Author(s): Edwards, Roger; Corfidi, Stephen F.; Thompson, Richard L.; Evans, Jeffry S.; Craven, Jeffrey P.; Racy, Jonathan P.; McCarthy, Daniel W.; Vescio, Michael D.
    Publisher: American Meteorological Society
    Abstract: Forecasters at the Storm Prediction Center (SPC) were faced with many challenges during the 3 May 1999 tornado outbreak. Operational numerical forecast models valid during the outbreak gave inaccurate, inconsistent, and/or ...
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