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at Harold's slidepath. An early morning shoot by the Utah deflection in the sensors. By April the depth of snow in
Department of Transportation producedsmall sluffs on the Harold's was over 4 meters. Based on the examination of
south facing avalanche paths. However, at 1145 hours sensor #3, this depth of snow renderedthe sensors useless
WhitePine #3 naturallyreleasedandcrossed Highway210. for the remainder of the winter. The snowpack was hard,
This natural release correspondedto the rapid increasein cold and deep.
creepratesat 1145 hours. Thesnow movementacceleration
for the period between 1145 and 1215 hours was 20.8 cm/
hr . Potentially, this rapid rise in creep rate relates to 4.4 Modifications to Instrumentation
2
possible widespread instability within the new snow For the winter of 1996-1997 a few changeswill be imple-
during this storm. mented to avoid the aforementioned problems. In order to
prevent the ready rods from bending under the pressure of
4.3 Climatic Effects on Instruments creep and glide, angle irons will be welded on the uphill
side of the ready rods. This should prevent any bendingof
During the winter of 1995-1996 valuable lesson were the mounting equipment. The wires that run from the
learned that could lead to more accurate and viable data instrumentation downhill to the sensors will be buried
collection. The creep and glide of the snowpack had a underground. These alterations will allow the sensor to
profound effect on the ready rods, sensors and wiring. make readings that are solely based on the angle of the
In April sensor #3 was excavated and examined. The sensor not both the ready rod and the sensor.
sensor was bent at an angle of 135 degrees from plumb. Location of the sensors is under review. The current
The ready rod was bent at an angle of 45 degrees. The site at Alta provides a good location. However, other sites
snow was gliding around the sensor. Since the sensor was may provide better conditions for the project. A site with
bent beyond 90 degrees, readings on snowpack creep and a shallower snowpack would assure creepand glide read-
glide wereinvalid. The condition of sensor # 3 lead to low ings throughout most of the winter.
confidencein thedatareceivedfrom sensors #1 and2. Also,
apparent was the tension that built up on the wires that
ran up hill to the datalogger. The tension from the wires 4.5 Summary
pulled downhillon sensor #3 and could be a causeof some
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