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<br />2.1.1 Initialization <br /> <br />2.1.2 Finer resolution <br /> <br />2.2 Model architecture (Any of the open <br />data sets can be used in addition to the <br />proposed case) <br /> <br />3. Applications to Further Understanding <br /> <br />3.1 Convective situation <br /> <br />3.2 Nimbostratus situation <br /> <br />CCOPE <br />6/20/81 <br /> <br />GATE 226 <br />8/14/74 <br /> <br />CCOPE <br />8/1/81 <br /> <br />CCOPE <br />7/19/81 <br /> <br />CCOPE <br />7/19/81 <br /> <br />CCOPE <br />8/1/81 <br /> <br />PEP <br />5/20/81 <br /> <br />Table 2. - (Continued) <br /> <br />Andy We-i nhei mer <br /> <br />Suppressed case with little synoptic <br />scale forcing. Large cumulus congestus <br />developed with isolated cumulonimbus, <br />cloud tops to 7.9 km MSL by 1300 MST. <br />Cb developed by 1247, 15 Anvil penetra- <br />tions, mature storm observations, <br />Doppler radar, mesonet rawinsondes and <br />surface data, multiple aircraft <br />observations. <br /> <br />Peggy Lemone <br /> <br />GATE P82 experiment with convergence <br />and moisture flux from aircraft (see <br />above). <br /> <br />Chuc k I~ade <br /> <br />PBL observations from mesonet, <br />aircraft strong outflow region deve- <br />loped from early ~b resulting in a <br />line of thunderstorms that produced <br />hail within network. Tri-Doppler, <br />three rawinsonde, multiple aircraft <br />penetrations. <br /> <br />Jim Dye <br /> <br />Excellent case for incloud and cloud <br />boundary mixing processes. Complete <br />sailplane observations of cumulus <br />congestus development, radar rawin- <br />sonde, and -multiple aircraft. Also <br />see 1.1.1.3. <br /> <br />Ji m Dye <br /> <br />See 2.1.2 <br /> <br />Chuck Wade <br /> <br />Excellent Doppler andcprecipitation- <br />-trajectory analyses available. Many <br />scientists stUdying this case. <br /> <br />Gabor Val i <br /> <br />Excellent PEP case with aircraft, <br />radar, surface and rawinsonde data. <br /> <br />9. <br />