Forecasting Severe Storms: SPC Presentation by Greg Dial

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Best viewed in a web browser that supports frames (e.g. Netscape or Internet Explorer). <HR> <H1><CENTER>Forecasting Severe Storms: SPC Presentation by Greg Dial</CENTER></H1> <HR> <H2>Table of Contents</H2> <H4>Select a slide or start at the <A HREF="fslide1.html">beginning</A>.</H4> <UL> <LI><A HREF="fslide1.html">Forecasting Severe Storms</A> <BR><LI><A HREF="fslide2.html">Forecasting Hail</A> <BR><LI><A HREF="fslide3.html">Forecasting Large Hail</A> <BR><LI><A HREF="fslide4.html">Forecasting Large Hail</A> <BR><LI><A HREF="fslide5.html">Forecasting Large Hail</A> <BR><LI><A HREF="fslide6.html">Forecasting Large Hail</A> <BR><LI><A HREF="fslide7.html">Forecasting Large Hail</A> <BR><LI><A HREF="fslide8.html">Forecasting Hail</A> <BR><LI><A HREF="fslide9.html">(Untitled)</A> <BR><LI><A HREF="fslide10.html">Organized Severe Wind Events</A> <BR><LI><A HREF="fslide11.html">In weakly capped environment, rapid squall line development is more likely when:</A> <BR><LI><A HREF="fslide12.html">In strongly capped environments, rapid squall line development is more likely when:</A> <BR><LI><A HREF="fslide13.html">(Untitled)</A> <BR><LI><A HREF="fslide14.html">(Untitled)</A> <BR><LI><A HREF="fslide15.html">(Untitled)</A> <BR><LI><A HREF="fslide16.html">(Untitled)</A> <BR><LI><A HREF="fslide17.html">(Untitled)</A> <BR><LI><A HREF="fslide18.html">Severe Bow Echo Formation</A> <BR><LI><A HREF="fslide19.html">Squall Line Organization</A> <BR><LI><A HREF="fslide20.html">(Untitled)</A> <BR><LI><A HREF="fslide21.html">(Untitled)</A> <BR><LI><A HREF="fslide22.html">(Untitled)</A> <BR><LI><A HREF="fslide23.html">(Untitled)</A> <BR><LI><A HREF="fslide24.html">(Untitled)</A> <BR><LI><A HREF="fslide25.html">(Untitled)</A> <BR><LI><A HREF="fslide26.html">(Untitled)</A> <BR><LI><A HREF="fslide27.html">(Untitled)</A> <BR><LI><A HREF="fslide28.html">Synoptic Patterns</A> <BR><LI><A HREF="fslide29.html">(Untitled)</A> <BR><LI><A HREF="fslide30.html">(Untitled)</A> <BR><LI><A HREF="fslide31.html">Supercell Lines</A> <BR><LI><A HREF="fslide32.html">(Untitled)</A> <BR><LI><A HREF="fslide33.html">(Untitled)</A> <BR><LI><A HREF="fslide34.html">(Untitled)</A> <BR><LI><A HREF="fslide35.html">Supercells and Tornadoes</A> <BR><LI><A HREF="fslide36.html">(Untitled)</A> <BR><LI><A HREF="fslide37.html">A Conceptual Model For Supercell Tornadogenesis</A> <BR><LI><A HREF="fslide38.html">A Conceptual Model For Tornadogenesis</A> <BR><LI><A HREF="fslide39.html">A Conceptual Model For Tornadogenesis</A> <BR><LI><A HREF="fslide40.html">A Conceptual Model For Tornadogenesis</A> <BR><LI><A HREF="fslide41.html">The creation of vorticity</A> <BR><LI><A HREF="fslide42.html">A Conceptual Model For Tornadogenesis</A> <BR><LI><A HREF="fslide43.html">A Conceptual Model For Tornadogenesis</A> <BR><LI><A HREF="fslide44.html">A Conceptual Model For Tornadogenesis</A> <BR><LI><A HREF="fslide45.html">Tornado Events</A> <BR><LI><A HREF="fslide46.html">Discrete Cells are more likely when:</A> <BR><LI><A HREF="fslide47.html">Upper Patterns</A> <BR><LI><A HREF="fslide48.html">Localized Convergence</A> <BR><LI><A HREF="fslide49.html">LFC/LCL Heights</A> <BR><LI><A HREF="fslide50.html">Horizontal Convective Rolls</A> <BR><LI><A HREF="fslide51.html">(Untitled)</A> <BR><LI><A HREF="fslide52.html">(Untitled)</A> <BR><LI><A HREF="fslide53.html">(Untitled)</A> <BR><LI><A HREF="fslide54.html">Tornadogenesis Failure Modes</A> <BR><LI><A HREF="fslide55.html">Upper Patterns</A> <BR><LI><A HREF="fslide56.html">Miller Type A Pattern</A> <BR><LI><A HREF="fslide57.html">Miller Type B Pattern</A> <BR><LI><A HREF="fslide58.html">Nowcasting Potential Tornadoes Using Diagnostic Analysis</A> <BR><LI><A HREF="fslide59.html">Diagnostic Analysis</A> <BR><LI><A HREF="fslide60.html">Diagnostic Analysis</A> <BR><LI><A HREF="fslide61.html">Diagnostic Analysis</A> <BR><LI><A HREF="fslide62.html">Objective Analysis</A> <BR><LI><A HREF="fslide63.html">Objective Analysis</A> <BR><LI><A HREF="fslide64.html">(Untitled)</A> <BR><LI><A HREF="fslide65.html">Categorical Outlook Definitions</A> <BR><LI><A HREF="fslide66.html">(Untitled)</A> <BR><LI><A HREF="fslide67.html">(Untitled)</A> <BR><LI><A HREF="fslide68.html">(Untitled)</A> <BR><LI><A HREF="fslide69.html">(Untitled)</A> <BR><LI><A HREF="fslide70.html">(Untitled)</A> <BR><LI><A HREF="fslide71.html">(Untitled)</A> <BR><LI><A HREF="fslide72.html">(Untitled)</A> <BR><LI><A HREF="fslide73.html">(Untitled)</A> <BR><LI><A HREF="fslide74.html">(Untitled)</A> <BR><LI><A HREF="fslide75.html">(Untitled)</A> <BR><LI><A HREF="fslide76.html">(Untitled)</A> <BR><LI><A HREF="fslide77.html">(Untitled)</A> <BR><LI><A HREF="fslide78.html">(Untitled)</A> <BR><LI><A HREF="fslide79.html">(Untitled)</A> <BR><LI><A HREF="fslide80.html">(Untitled)</A> <BR><LI><A HREF="fslide81.html">(Untitled)</A> <BR><LI><A HREF="fslide82.html">(Untitled)</A> <BR><LI><A HREF="fslide83.html">(Untitled)</A> <BR><LI><A HREF="fslide84.html">Improving Warnings In Areas With Limited Radar Coverage</A> <BR><LI><A HREF="fslide85.html">Improving Warnings In Areas With Limited Radar Coverage</A> <BR><LI><A HREF="fslide86.html">(Untitled)</A> <BR><LI><A HREF="fslide87.html">(Untitled)</A> <BR><LI><A HREF="fslide88.html">(Untitled)</A> <BR><LI><A HREF="fslide89.html">(Untitled)</A> <BR><LI><A HREF="fslide90.html">(Untitled)</A> <BR><LI><A HREF="fslide91.html">(Untitled)</A> <BR><LI><A HREF="fslide92.html">(Untitled)</A> <BR><LI><A HREF="fslide93.html">(Untitled)</A> <BR><LI><A HREF="fslide94.html">(Untitled)</A> <BR><LI><A HREF="fslide95.html">(Untitled)</A> <BR><LI><A HREF="fslide96.html">(Untitled)</A> <BR><LI><A HREF="fslide97.html">(Untitled)</A> <BR><LI><A HREF="fslide98.html">(Untitled)</A> <BR><LI><A HREF="fslide99.html">(Untitled)</A> <BR><LI><A HREF="fslide100.html">(Untitled)</A> <BR><LI><A HREF="fslide101.html">(Untitled)</A> <BR><LI><A HREF="fslide102.html">(Untitled)</A> <BR><LI><A HREF="fslide103.html">(Untitled)</A> <BR><LI><A 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