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<br />Tab 1 e <br /> <br />1 <br />2 <br /> <br />3 <br /> <br />4 <br /> <br />5 <br /> <br />6 <br />7 <br /> <br />8 <br /> <br />9 <br /> <br />Figure <br /> <br />1 <br /> <br />2 <br /> <br />CONTENTS - Continued <br /> <br />TABLES <br /> <br />Rawinsonde sample sizes <br /> <br />Model-predicted cloud development vs. observed <br />convective clouds in 1976 samples at MLS, GLD, <br />and BGS, and 1977 at GLD and BGS ..... <br /> <br />Model vs. aircraft observations of cloud-base <br />height and cloud-top height, Miles City, <br />summer 1977 . . . . . . . . . . . . . . . . <br /> <br />Sample means for different cloud types observed <br />at Miles City, Montana, in 1976-77 during days <br />for which satellite population statistics of <br />convection clouds were available . . . . <br /> <br />Spatial differences in 1975 Montana mesonet <br />thermodynamic and cloud model variables <br /> <br />Legend for tables and figures. . . . . . . <br /> <br />Maximum DMP for operational days stratified <br />by observed cloud type in 1976 for maximum <br />DMP greater than 1.0 km . . . . . . . . . . <br /> <br />Maximum OMP for operational days stratified <br />by observed mesoscale trigger type in 1976 <br />for maximum OMP greater than 1.0km . . . <br /> <br />Maximum DMP for operational days stratified <br />by all Cu, Cu+, and Cb cases in 1976 for <br />maximum OMP greater than 1.0 km . . . . . <br /> <br />FIGURES <br /> <br />Map of HIPLEX field sites and special <br />rawinsonde sites and networks used in <br />this study . . . . . . . . . . . . . . <br /> <br />Seasonal averages of cloud model-diagnosed <br />cloud-top height and maximum updraft speed <br />as a function of cloud updraft radius for <br />three mesonet stations (MLS, GO, PL) in <br /> <br />1975 . . . . . . . . . . . . . . . . . . . <br /> <br />vi <br /> <br />Page <br /> <br />4 <br /> <br />, <br />~ <br /> <br />13 <br /> <br />15 <br /> <br />19 <br /> <br />22 <br />34 <br /> <br />46 <br /> <br />47 <br /> <br />48 <br /> <br />3 <br /> <br />25 <br />