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<br />SEPTEMBER 1988 <br /> <br />MARK F. HEGGLI AND ROBERT M. RAUBER <br /> <br />1009 <br /> <br /> <br />\ <br />I <br />I <br /> <br />,...,.r..';-. ,/..,....,....,.. T7...... ,..,.............. <br /> <br />-40 <br />I <br />\ <br />\ <br /> <br />~5 <br /> <br />30- - .' - <br /> <br />.. <br /> <br />.'.~ <br />~ <br />:~!,'.~~. -..... <br /> <br />...,.. <br />. ' <br />. <br /> <br />FIG. 16. As in Fig. 4, but for 0000 UTe 2 February 1985, <br />The satellite photograph was taken at 0200 UTe. <br /> <br />Offshore storms were usually very cold, sometimes <br />producing significant amounts of snow near sea level. <br />Winds over the Sierra Nevada were weak at all levels. <br />Sustained amounts of supercooled water were rarely <br /> <br />observed in the cold trough, which was dominated by <br />strong convection. Convective peaks of supercooled <br />water sometimes reached 0.50 mm but again, were very <br />short lived. Precipitation was typically 3 mm h-1 and <br />