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<br />to initialize a diagnostic cloud model. The model then predicts the <br />effect of lifting on convective cloud growth in specific local regions <br />represented by the sounding. These model predictions help explain the <br /> <br />large natural variations, thus permitting objective stratification of <br />events into similar mesoscale classes of convective potential. <br /> <br /> <br />Meso-l3 Scale Analysis PO <br />Grid I <:> <br /> ~ <:)LA 33. <br /> SN <br /> <:) <br /> I <br /> I SE 32. <br /> . 31.8N <br /> 102.4OW i020 1010 100.60 <br /> I .. 94 km 'I / <br /> i AMA/ / <br /> I / <br /> I <br /> / <br /> / LOOt <br /> r"jPO -, / <br />HOB S~ LA <:) <br />. <:> SN GSW <br />I I BG <:) / A <br />MA e SE/ <br />. fJ e <br />INK <br />FST I~ 472 km <br /> Synoptic-scole ~etwork <br /> <br /> <br /> <br /> <br />VCT <br />A <br /> <br />G.i Synoptic Rowinsonde Site <br /><:> Meso-13 Rowinsonde Site <br /> <br />Figure 1.1 Synoptic and meso-p scale analysis area of the <br />Texas HIPLEX Program. <br /> <br />f.. <br />