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<br />High Plains, there is little indication of the isolated cold air pocket <br />appearing on the surface. <br />The moist layer top temperatures (fig. 23) are lowest in the <br />western, higher elevation portions of the High Plains; Denver, Colorado, <br />and Lander, Wyoming, have the lowest top temperatures. <br /> <br />It is instructive to compare the average cloud top temperatures <br />of precipitating layers (fig. 24) with those of nonprecipitating <br />layers (fig. 25). For the nonprecipitating cases, the top tempera- <br /> <br />UPSLOPE' 'SEEDABLE'SITUA TIONS <br />-10 -10 <br /> <br /> <br />Moist Layer Top Temperature (OC) <br />for Precipitating Cases <br /> <br />Figu.re 24: Mean cloud top <br />temperotures t c) for precipi- <br />tating seedable upslope aloud <br />systems. <br /> <br />UPSLOPE' 'SEEDABLE' SITUATIONS <br />-9 <br /> <br /> <br />Moist Layer Top Temperature (OC) <br /> <br />for Non,preclpltatlng Cases <br /> <br />FigUI'e 25: Mean a loud top <br />o <br />temperatures ( c) for nonpre- <br />aipitating seedable upslope <br />aloud systems. <br /> <br />30 <br />