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<br />expected to parallel the slope of the cold dome. Thus the highest <br />cloud bases might be expected along the mean trajectory of the tops of <br />the cold domes with lower cloud bases along the western edge of these <br /> <br />air masses. <br /> <br />4.3.2. Cloud top height <br />Figure 12 shows the mean heights of the tops of seedab1e moist <br />layers in the High Plains. These heights vary from 1800 m in the <br />north to approximately 3400 m in the south with a large gradient of <br />heights in the south. An axis of relatively high cloud tops parallels <br />the axis of high cloud bases (fig. 11). <br /> <br />UPSLOPE' 'SEEDABLE' SITUATIONS <br /> <br /> <br />Moist Layer Top (meters AGL) <br /> <br />Figw>e 12: Mean aZoud top <br />heights in meters above ground <br />Ze ve Z. <br /> <br />I <br /> <br />1 <br /> <br />18 <br />