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<br />Fig~re
<br />
<br />4.5
<br />
<br />4,6
<br />
<br />4.7
<br />
<br />4,8
<br />4.9
<br />
<br />4.10
<br />4.11
<br />
<br />4.12
<br />
<br />4.13
<br />
<br />4.14
<br />
<br />4.15
<br />
<br />4.16
<br />
<br />4,17
<br />
<br />4.18
<br />
<br />4.19
<br />
<br />CONT~NTS - Sontinued
<br />
<br />Temporal variability of sounding structure at ~A
<br />on June 4, 1979, from 1500 to 0300 GMT during a
<br />typical line case. . . . , . . . , . , . , .
<br />
<br />Spatial variability of sounding structure on
<br />June 1, 1979, at 1800 G~T during a typical
<br />mesosynoptic case . . . . . . . , . . .
<br />
<br />GOES-Tap KB-4 visible satellite image observed at
<br />1302 G~T, June 5, 1979 . . , . . . . . . . . . .
<br />
<br />Visible satellite image at 2332 G~T, June 5, 1979
<br />
<br />~esoscale wind fields at 900, 700, 500 and 300 mb
<br />at 1500 GMT, June 5, 1979, derived from band-pass
<br />objective analysis . . . . . . . . . . , . .
<br />
<br />Total wind field vectors at 1500 GMT, June 5, 1979
<br />
<br />Three-dimensional wind vectors and conceptual
<br />model of flow at 1800 GMT, June 5, 1979 . . .
<br />
<br />East-west cross section of objective analysis grid
<br />at 330 N. from 102.2 to 100,80 W. at 1800 G~T,
<br />June 5, 1979 . , . . . . . . . . . , . . .
<br />
<br />Composite PPI of maximum echo-top height at 1958
<br />GMT, June 5, 1979 . . . . . . . . . , . . . ,
<br />
<br />East-west cross section at 330 N., 2100 GMT,
<br />June 5, 1979 . . . . , . . . . . . . . , .
<br />
<br />Composite PPI of maximum echo-top height at
<br />2156 GMT, June 5, 1979 . . . , . . . . , .
<br />
<br />Ver~ical profile; of ~Q,~~Qe' momentum and ~ixing
<br />ratlo at 1800 GMI, June ~, 1979 . . . . . . . . .
<br />
<br />Vertical profile of lifting derived from the
<br />objective analysis vertical motion field at the
<br />grid point nearest to PO at 1800 GMT, June 5, 1979,
<br />and MESOCU-predicted changes in temperature and
<br />
<br />de\r/point .. . . . . . . . . . . . . . , . . . . .
<br />
<br />Cumulative temperature changes due to lifting and
<br />c01vection predicted by MESOCU from 1200 to 1500 LS~
<br />basec on the PO sounding shown in Fig. 4.17 . . . , .
<br />
<br />Visible satellite i~age at 2100 GMT, June 24, 1979
<br />
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