044
HALL
24,
20 16 12
08
04 00 96 92 88 i 88 \96\ 04
|
Ke
<=
+
0
5
610
rere
NAUTICAL MILES
Fig. 14—Storm position with radar-echo-intensity contours (db) for
2029 CST on May 9, 1964.
Figures 15 to 20 are the rainfall-sample cross sections for
stations 5 through 10, respectively. These, along with Figs. 21 to 26,
the time cross sections of echo intensity and radar storm tops over
Stations 5 through 10, respectively, show the general nature of the
beta-concentration profiles. The figures show that with the exception
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