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<br />fINAL SOUNDING AT 8 HR 0 MIN <br /> <br />fINAL SOUNDING AT 11 HR 0 MIN <br /> <br />20 <br /> <br /> <br />-30 LEGEND <br />I . - CASE <br />. - CASE <br />. - CASE <br /> <br />10 <br /> <br />-90 <br /> <br />-70 <br /> <br />-50 -40 <br /> <br />10 <br /> <br /> <br />e <br /> <br />20 <br /> <br />a: <br />0... 30 30 <br />~ <br />w <br />a::: <br />::J <br />If) 10 ,10 <br />If) <br />w <br />a::: <br />0... <br /> 50 50 <br /> 60 60 <br /> 70 40 70 40 <br /> 80 80 <br /> 85 85 <br /> 100 100 <br /> TEMPERATURE (Cl TEMPERATURE (~: ) <br /> <br />e <br /> <br />Figure 5.1. - Themodynamic changes of temperature <br />(solid) and dewpoint (dashed) plotted on a SKEW-T <br />diagram for model responses using the Good'land, <br />August 19, 1977, 1200 G.m.t. raob. <br /> <br />I <br />Figure 5.2. - Same as figure 5+1 for 1800 G.m.t. <br />raob. <br /> <br />CLOUD DEPTH AND PRECIP VERSUS TIME <br /> <br />CLOUD DEPTH AND PRECIP VERSUS TIME <br /> <br />12.0 <br /> <br />LEGEND <br />o~OEPIH- <br />0" SURfACE PREe I P I TAT I ON <br />A" ClOUD BASE PREelP <br />+ .. PREe I P I TRBLE HRTER <br /> <br />12.0 <br /> <br />LEGEND <br />O-OEPnl- <br />0" SURrFlCE PRECIPITATION <br />A" CLOUD BASE f'RECIP <br />+.. PRECIPITABLE wATER <br /> <br />'.0 <br /> <br /> <br />5<>.0 <br /> <br />',0 <br /> <br />~ .--' <br />'-'. -- --'--+------ <br /> <br /> <br />.~...,. I~ <br />,:.~ <br /> <br />13 11 <br />TIME ILsn <br /> <br />2.0 <br /> <br />0.0 <br /> <br />0.0 <br />12 <br /> <br />Figure 5.3. - Cloud depth and precipitation <br />diagnosed by the model for the August 19, <br />1977, 1200 G.m.t. Goodland raob. <br /> <br />Figure 5.4. - Same as figure 5~3 for 1800 G.m.t. <br />raob. <br /> <br />e <br /> <br />Figure 5. - Same as figure 4; however, lifting depth is increased from 70 kpa to 20 kPC! (3 to 12 km). <br />Note the increase in cloud depth and precipitation in contrast to figure 4. <br />