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<br />." ." <br /> l' . .. <br /> , <br />... . ( <br /> ... , . <br /> . <br />... ... <br />... ... <br />u. u. <br />". '" <br />D' D. <br />D' D' <br />,.. ,.. <br />... ... <br /> <br />Detailed Analog El Nino Composites for 2004-5 <br />NDJ Precipitation Composites <br />(1963,1969,1977,1986,1990,1991,1994.2002,2003) <br /> <br />NDJ Precipitation Composites <br />(1988.1990.1991.1994) mlnu. (1963.1989.1977.2003) <br /> <br /> <br /> <br /> <br />.,.. . <br />" . <br /> <br />'" <br /> <br />124. 1m 12O'f tin <br /> <br /> <br />". <br />..... <br /> <br />1111' <br /> <br />1141 IIn <br /> <br />110'1 Ion <br /> <br />lOISI' 104. <br /> <br />'1lrI <br /> <br />10lr30!f <br /> <br />1241 122' 120. tin <br /> <br />".. <br /> <br />114t' IIn <br /> <br />110. <br /> <br />102'1 IGOY <br /> <br />...... .... <br />~1001~ <br /> <br />.. ............ <br />10 2'll 30 40 so 80 70 80 to lOOllCI20130UOI~ <br /> <br />A station-by-stalion analysis for 9 analog El Nino composite cases (left) looks dry for mOSl of the Upper <br />Colorado basin into early 2005. If the current event were to grow rather than shrink into the winter, there <br />would be a better ehance for increased moisture over lower elevations, while NC mountains ofUT and CO <br />would be even less likely to receive adequate snowfall (right). These results are not field significant. <br />