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I n s t r u m e n t s

a n d

M e t h o d s

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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 ofcable.Sincethe sensors were installedin January thecable
tilt.Once seven corresponding angles were known in thewas 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 forsensor #3 in the x-
2.5 Data retrieval
direction is:The data was downloaded from the dataloggervia RF te-
lemetry every week for analysis.During a storm cycle data
y=0.0054x+0.1543Eq.(3)wasdownloadedandanalyzedmorefrequently.This
where:allowed examination of snowpack strength andactivity on
y=voltagea real time basis.
x=angle of tilt of sensor3.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 ofsensors showed promise.The majorproblem was the in-
the three sensors a linear equation was derived in both thestallation 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
workingsensoronce thesystemwasoperational.Two
Once the C&G sensors are in placein the starting zone, theimportant results were obtained from the data.The elastic
data collectionstation was installed.The station consistedresponse of the snowpack to explosives and the increase
ofadatalogger,multiplexerand 12voltdcsolarpowerin creep rates due to loading were recorded that preceded
supply.Thestation anddatais accessedby radiotelemetry.widespread avalanching.
A solarpanel was pointed at 25 degrees aspect due to theOn February 20, 1996 an explosive charge(2kg / PETN)
terrain and tiltedslightlytowardthe ground sothatthetiedtoabamboopolewasdetonated 1meterabovethe
energy from the snow reflectivitywould chargethe battery.newsnowsurfacetocreate anairblastinHarold'sslide
AprogramwasdownloadedtothedataloggerviaRFpath at 1200 hours.The elastic response of the snowpack
telemetry to monitorthe 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.Thesors.Thisisevidentwithanincreaseincreep rateor
programretrieved themaximum and minimum angles anddeflection of the sensor.This rapid increase was followed
calculated the averageovera fifteen minute interval.Theby a slow stabilization of the snow.This is evident by the
angle of the sensormoving back toward normal.In start-

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Figure 1. Probe #1 r eflecting no creep movement.

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