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Niwot Ridge LTER Snow Report for Mar 2006 At Niwot (C1), the manually measured snowpack showed 13.25 inches of water (SWE), a depth of 43”, and a density of 32%, on 31 March 2006. The 13.25” SWE is 103% of the long-term average, and exactly the same percent of average reported by the Snotel network. If it had not been for the single massive snowfall in late March 2003, this would be the highest Niwot March snowpack since 1997. The Snowpack Index (SI) is less than one (103% SWE divided by the 111% cumulative winter precipitation to date) at Niwot, but nearly one for the South Platte basin (108% vs 110%), meaning non-precipitation climatic factors effecting snowpack are just about normal (only slightly detrimental to snowpack development). The State of Colorado, according to the Snotel network, has a snowpack of 96% of average, and seasonal precipitation of 100%, so a SI of just under one. The highest snowpack is in the Upper Colorado basin, with 111% and 114% (SWE and cumulative precipitation, respectively). The lowest is the Upper Rio Grande, with 65% and 79%, respectively. This is a good increase from last months 43% and 63%, particularly since this is near the start of their spring melt out! In the western US, Oregon and Nevada have the highest snowpacks, with 134%, and both also have SI’s of greater than one. Montana, Utah, and Washington also have SI’s greater than one. This is good news for snowpack development, and a rare occurrence for so many states to be so positive in this regard, compared to the last several years. Of the major river basins, the Colorado, Columbia, and Great Basin Rivers SI’s are also one or greater. As mentioned above, there was a slight shift in atmospheric flow this month, a little less zonal and more meridional. The ENSO index is still near neutral to slightly La Nina, and likely to stay this way during the next 3-6 months (9 March 2006, NOAA CPC), so ENSO may not explain this seasons precipitation patterns. The weakening of the zonal flow might be an expected feature of spring onset, but it also coincided with the first time in the last three months that the phase of the Madden-Julian Oscillation (MJO) became indefinable, almost to the day. Whatever the reason, it came just in time for our southern areas! Until next month, Mark
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| This material is based upon work supported by the National Science Foundation under Cooperative Agreement #DEB-0423662. 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. |