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exoscientist<br />(<font color="#66ccff"><b>B</b></font>)<br />03/12/03 02:38 AM<br /><br />Snowpack Temperature and Tensile Strength<br />R. S. Rosso<br />TSI, Incorporated, 356 South West Temple, Salt Lake City, Utah 84115; tel. 801-262-0651; fax. 801-262-0942; email. steve@holix.com<br />D. Howlett and S. Calhoun<br />"In an effort to understand post-control and other natural avalanches that occur shortly after rain begins or the sun's rays start to warm the starting zone, several experiments were conducted. The use of inexpensive, commercially available data-loggers for in-situ temperature data acquisition and recording is presented along with the results of several temperature tests. By monitoring the snowpack temperature at various depths we found warming from the sun to reach as deep as 50 cm within hours after the sun's rays reached the slope. At shallower depths the sun's radiation warmed the snowpack (not just the surface) to temperatures well above the air temperature. Under conditions artificially created to simulate rain, the snowpack temperature was found to increase at depths of as much as 20 cm as the rain crust froze on the snow surface above. Finally, by conducting in-situ tensile strength tests on the upper snow layers, during simulated rain, we found average decreases in snow strength of approximately 15%. We theorize that avalanche failure of a snow slab over an extensive weak shear layer could be the result of a decrease in tensile strength caused by snowpack warming related to the onset of the sun's radiation or a rain event."<br />http://www.issw.noaa.gov/effects_of_warming_and_rain.htm<br /><br /><br />Bob C.