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<br />SEPTEMBER 1988 <br /> <br />MARK F. HEGGLI AND ROBIERT M. RAUBER <br /> <br />1003 <br /> <br />I, <br /> <br /> <br />5.28 <br /> <br />......:::.::;. <br /> <br />-30 <br /> <br />--- <br />~_/ 540 <br />- -25- <br /> <br />l <br /> <br />I <br />I <br /> <br />, <br />I <br /> <br />, <br />____'_- <br /> <br />3 - 7 <br />-..... <br /> <br />. <br />. <br />, <br />1t'5 <br />. <br /> <br />516 <br /> <br />, <br />, <br />-, <br /> <br />-15 <br />....... <br /> <br />30- - -- - - - ~ <br /> <br /> <br />.... ". <br />~'~'._':~~':'~~::'~'~.:. ,', <br />. "-~ <br />~ ~i.:,. ". - . <br /> <br />Fla. 10. As in Fig. 4, but for 1200 UTe 22 December 1986. <br />The satellite photograph was taken at 1300 UTe. <br /> <br />suggesting that weak embedded convection cells may <br />have been present. The continual presence of super- <br />cooled water in these cloud systems was most likely <br />associated with inefficient precipitation processes based <br /> <br />on the shallow nature of the clouds and the low pre- <br />cipitation rates. Winds had a cross-barrier component <br />throughout the lifetime of the storms, which supported <br />the presence and sustenance of supercooled water. <br />