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<br />Precipitation (mm) Compo6ite Anomaly 1 J71- 20(){) climo <br /> <br />Precipitation (mm) Compo6ite Anomaly 1 J71- 20(){) climo <br /> <br /> <br /> <br />-I2~ <br /> <br />-I2~ J <br />12. <br /> <br />+1,5~ <br /> <br />+1,5~ <br /> <br /> 6 <br />-IaN . <br />JRoN 1 3 JRoN <br /> 39N <br /> 0 <br /> J5.oN <br /> <br />1001lJ 10511J 1 DIW 10ew 105W 10-WJ 100W 1 aZlIJ 1 D111J <br />Mar to May: 1955.1963.1965.1967.1965,1972. i 975.1985,1996. i 997.2001 <br /> <br />10-WJ 100W 1 aZlIJ 1 D111J <br /> <br />Does it make a difference for our SPRING moisture whether we <br />have a weak La Nina during the winter or wring? Using an 11- <br />member composite average for March-May based on the familiar weak <br />La Nifia winters (left) versus weak La Nifia springs (right), we find <br />little difference for the northern Front Range (both 'dry') and much of <br />western Colorado (both 'wet'), but more changes for the southern Front <br />I Range and the eastern plains. Since these composited anomalies are <br />small compared to normal, these results are not considered robust! <br /> <br />12. <br /> <br />9 <br /> <br />6 <br /> <br />3 <br /> <br />o <br /> <br />-3 <br /> <br />-0 <br /> <br />.-9 <br /> <br />-1" <br />