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Niwot Ridge LTER Snow Report for March 2002 The "catch-up" amounts of snowfall continue to elude us. The C1 snowpack on 29 March 2002 contained 7.563 inches of water, which is 57% of the long term mean value, about the same perentage as last month. The snow depth was 28 inches, and density was 28%. This snowpack value is certainly the lowest in my records, behind 1999, and 1991 March end snowpacks. In both those years, the end of April snowpack had increased from March levels, so there is hope, perhaps, for somewhat of a recovery. The year that holds the 'spring recovery' record was 1995, when the March end snowpack was 10 inches. That year, the snowfall began in ernest on April 9, and continued until June 1. The March snowpack value of 10" grew to 16.75" in April, and 19.75" by the end of May, a time when it is normally zero at C1. A quick check of many climate related indicies, however, does not show spring of 2002 to compare similarly to the spring of 1995. So, I will not guess about the upcoming April snowfall frequency or amount. The state of Colorado, according to the NRCS SnoTel records, shows low snowpack overall, with the lowest still in the southwest, as has been the case all season. The San Miguel, Dolores, Animas, San Juan basins are at 40%, and the upper Rio Grande is 41% of average, for the lowest in the state. The highest basin is the Yampa, White at 68%, and the Laramie/N. Platte, and Upper Colorado basins are also in the mid to upper 60th percentile. Our South Platte basin is at 57%, but with 70% of average precipitation, indicating a little less than usual amounts of the winter precipitation is stored in the snowpack at this time. And for those of you who follow Wolf Creek Pass amounts, it is at 31% today. So, there is still another month to make up this deficit, and we shall see if it will. The full record of manual samples of C1 snowpack follows. Unitl next month, Mark L
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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. |