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<br />Figure <br /> <br />5.4 <br /> <br />5,~ <br /> <br />5.6 <br /> <br />5.7 <br /> <br />5.8 <br /> <br />5.9 <br />5.10 <br /> <br />5.11 <br /> <br />5.12 <br /> <br />5,13 <br /> <br />5.14 <br /> <br />5.15 <br /> <br />5.16 <br /> <br />CONTE~TS - Continuec <br /> <br />FreqJency distribution of maximuT: and average echo- <br />top heights and temperatures for all echoes within <br />150 km lasting ffiore than 1 h ........... <br /> <br />Frequency distribution of echo-top te~perature and <br />height by mesoscale types . . . . . . . . , . <br /> <br />Vertical profiles af average Qe for each type of <br />event at 1800 GMT . . . . .. . . . . . . <br /> <br />Vertical profiles of ~Qe with 95% confidence <br />intervals about the ~ean at 1500, 1800, 2100 and <br />0000 GMT , , . , . . , . , <br /> <br />Composite soundings of mean temperature and dewpoint <br />for all 572 soundings and all 2100 GMT soundings <br /> <br />Composite profiles of relative humiaity . . , , <br /> <br />Composite average values of precipitable water, PBL <br />mixing ratio and TOTALS-TOTALS index . . . . <br /> <br />Composite profiles of minimum vertical motion at <br />1500, 1800, 2100 and 0000 GMT . . , . . . . , <br /> <br />Time series plots of wind speed at 300 mb, 300 to <br />900 mb vertical wind shear, minimum ~ at 500 mb, <br />and average w for all grid points having values <br />of ~ less than -5 ~bars from 1500 to 0300 GMT for <br />each type of event . . . . , . . , , . , . . <br /> <br />Composite average of MESOCU-predicted maximum <br />cloud-top height and convective potential index <br />for each type . , . . , . . . . . . , . . . . . . <br /> <br />Composite average surface mixing ratio and cloud- <br />base level environffiental and saturation mixing <br />ratios, cloud-base height and -base temperature <br />for clouds predicted by MESOC~ for each type of <br /> <br />event . . . , . , . . , . . . . , . . . . . . . <br /> <br />Co~posite rate of change in releasable ;nstability <br />and PB~ moist static energy for different types <br />from ~ESOC~ analyses .....,..,..... <br /> <br />Releasable instability, releasable instabil ty due <br />to lifting, lifting rate at 500 mb and lift ng rate <br />at 900 mb in ~ESOCJ analyses .........., <br /> <br />xviii <br /> <br />Page <br /> <br />201 <br /> <br />202 <br /> <br />206 <br /> <br />207 <br /> <br />209 <br />211 <br /> <br />212 <br /> <br />216 <br /> <br />217 <br /> <br />222 <br /> <br />223 <br /> <br />224 <br /> <br />226 <br />