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Niwot Ridge LTER Snow Report for April 2001 The recent large snowfall helped salvage the April snowpack level however, it was not enough to beat the March 30 reading, so for this season, the maximum snowpack will be recorded as occurring on March 30th. The snowpack measurement at C1 on April 30, 2001 shows 9.125 inches of snow water equivalent, for 64% of the long term average. The snow depth is 27 inches with an average density of 34%. One month ago, the corresponding values were 10.0 " SWE (74% of avaerge), 40" depth, and 25% density. (The increasing density of the snowpack is a clear sign that spring is here). Although the C1 snowpack is only at 64%, the winter precipitation is at 89%. This suggests that we have recieved closer to average precipitation than is indicated by the snowpack figures alone, but it has been warmer than usual, so less of this precipitation is in the form of snow still on the ground. As low as this April's snowpack may be, last year it was lower, at 7.6 ", and then it was not until April 1989, 5.6", that it was less. It is interesting to note how fast snow conditions can change this time of year. Seven days ago, the snowpack was 74% of average, and three days before that it was 61%. C1 recieved just under two feet of snow and 2 inches of water in the April 21-22 storm. Statewide, the NRCS figures show the same snowpack trends that have existed all winter; normal to above in the south, and below normal in the north. Our South Platte basin has 88% of average snowpack, the Upper Rio Grande basin has 119%, for the highest percentile of average in the state, and the Yampa/White River basin just barely squeezed by the Laramie/N. Platte for the lowest with 73%. The Laramie/N. Platte has 74%. In the S. Platte, not all areas are low. Loveland and Hoosier Pass are doing quite well with 124% and 103% respectively. This may be the last end-of-the-month report for this season, unless May produces some large snowfalls, which definitely does happen some years, noteably May 1995. But if not, see you next season. Cheers! Mark
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| This material is based upon work supported by the National Science Foundation under Cooperative Agreement #DEB-9810218. Any opinions, findings, conclusions, or recommendations expressed in the material are those of the author(s) and do not necesarily reflect the views of the National Science Foundation. Please contact lternwt@colorado.edu with questions, comments, or for technical assistance regarding this web site. |