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<br />Figure <br /> <br />3 <br /> <br />4 <br /> <br />5 <br /> <br />6 <br /> <br />7 <br /> <br />8 <br /> <br />9 <br /> <br />10 <br /> <br />11 <br />12 <br /> <br />CONTENTS - Continued <br /> <br />Synoptic-scale geographic variability of <br />PBL thermodynamic variables for 1977 . <br /> <br />Geographic vari abil ity of two cloud model <br />variables - cloud-top height and <br />maximum updraft speed - for 1977 at <br />MLS, GLD, and BGS . . . . . . . . . . . <br /> <br />Synoptic-scale annual vari abil ity of PBL <br />thermodynamic variables for Goodland, <br />Kansas, in summers of 1975, 1976, and 1977 <br /> <br />Synoptic-scale annual variability of updraft <br />speed and cloud~top height for Goodland, <br />Kansas, 1975, 1976, and 1977 . . . . . . . <br /> <br />GOES-EAST KA-4 sector of visible satellite <br />imagery with approximately l-km resolution <br />showing typical mesoscale and convective <br />cloud patterns over the High Plains on <br />August 1 and 2, 1977 . . . . . . . . . . <br /> <br />Percent frequency of occurrence of mesoscale <br />triggering and cloud types observed in <br />satellite imagery at the HIPLEX site in <br />1976 and 1977 . . . . . . . . . . . . . . <br /> <br />Mean model-diagnosed cloud-top height and <br />maximum updraft speed for natural cloud <br />simulations as a function of a radius <br />classified by four satellite-observed <br />cloud types . . . . . . . . . . . . . . <br /> <br />Skew T-log P diagram showing typical thermo- <br />dynamic structure of cases where large <br />DMP ex i st s . . . . . . . . . . . . . . <br /> <br />Internal profiles of modeled cloud variables <br /> <br />Cumulative frequency of maximum DMP showing <br />the geographic and annual variability of <br />DMP at each site for the 1975 to 1977 <br />field seasons . . . . . . . . . . . . . . <br /> <br />vi i <br /> <br />Page <br /> <br />27 <br /> <br />29 <br /> <br />31 <br /> <br />32 <br /> <br />35 <br /> <br />37 <br /> <br />39 <br /> <br />42 <br />43 <br /> <br />44 <br />