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benchedtestedandcalibrated. Thesensors werecalibrated, sensors were connected to the hardware via 50 meters of
so that a voltage would correspond to a specific angle of cable. Sincethe sensors were installedin January thecable
tilt. Once seven corresponding angles were known in the was laid on the snow surface.
x and y directions, and repeatability established, a linear
relationship is established to derive the remaining angles
of tilt. The linear equation derived for sensor #3 in the x- 2.5 Data retrieval
direction is: The data was downloaded from the datalogger via RF te-
lemetry every week for analysis. During a storm cycle data
y = 0.0054x + 0.1543 Eq. (3) was downloaded and analyzed more frequently. This
where: allowed examination of snowpack strength andactivity on
y = voltage a real time basis.
x = angle of tilt of sensor 3. PRELIMINARY RESULTS

By knowing the voltage produced by the sensor, the an- The preliminary results obtained from the creepand glide
gle of tilt of the sensor is derived from Eq. (3). For each of sensors showed promise. The major problem was the in-
the three sensors a linear equation was derived in both the stallation and operation of the sensors. Since the sensors
x and y direction. became operational in late January, sensors #1 and 2 were
buried under 2.5 meters of snow. Sensor #3 was the only
2.4 Instrumentation working sensor once the system was operational. Two
Once the C&G sensors are in placein the starting zone, the important results were obtained from the data. The elastic
data collectionstation was installed. The station consisted response of the snowpack to explosives and the increase
of a datalogger, multiplexer and 12 volt dc solar power in creep rates due to loading were recorded that preceded
supply. Thestation anddatais accessedby radiotelemetry. widespread avalanching.
A solar panel was pointed at 25 degrees aspect due to the On February 20, 1996 an explosive charge(2kg / PETN)
terrain and tilted slightly toward the ground so that the tied to a bamboo pole was detonated 1 meter above the
energy from the snow reflectivitywould chargethe battery. new snow surface to create an airblast in Harold's slide
A program was downloaded to the datalogger via RF path at 1200 hours. The elastic response of the snowpack
telemetry to monitor the sensors every 15 seconds. Also, due to the explosive charge was capturedby the C&G sen-
capabilities at the site allow for real time monitoring. The sors. This is evident with an increase in creep rate or
programretrieved themaximum and minimum angles and deflection of the sensor. This rapid increase was followed
calculated the averageover a fifteen minute interval. The by a slow stabilization of the snow. This is evident by the
angle of the sensor moving back toward normal. In start-
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