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<br />1000 <br /> <br />JOURNAL OF APPLIED METEOROLOGY <br /> <br />VOLUME 27 <br /> <br />......-. <br />...... .t...,......: <br />" <br /> <br />......"... ............. <br />------":--- <br />----..:". <br /> <br />--35:~::s.::.::.:::::;. _ <br /> <br />r< <br />:2~" :::, <br />----,-----. <br />I <br />I <br /> <br /> <br />I <br />I <br />I 576 <br />I <br />I I \ <br />30- - - - - :.. :,~- :"':15': ~ - -=- - ~ - - - - - - _ _ _ ~ _ .. _ _ _ _ _ _ __{,15_-= _ <br /> <br /> <br />. .. <br />. ". _. ....~"r_". <br /> <br />~~':i.., . s..~'~ <br />.:;,:....;,.."r..:..',~': <br /> <br />.....~ <br />, <br /> <br />FIG. 7. As in Fig. 4, but for 1200 UTe 24 February 1984. <br />The satellite photograph was taken at 1215 UTe. <br /> <br />cipitation rates reduced substantially and shallow con- <br />vective cells developed over the foothills and higher <br />Sierra Nevada. These cells were often embedded in an <br />orographic cloud. <br /> <br />Complete radiometer data were available during six <br />storms in the category. The remaining storms had high <br />freezing levels producing rain at Kingvale. The highest <br />supercooled water measurements in these storms were <br /> <br />