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manufacturing.
Although the initial prototype worked well, there were
some basic design changeswhich had to be incorporated
in order to both improve the quality of the measured data
and make the sensor operational in remote areas. Some of
these changes were basic, involving power supply (from
AC to DC operation), packaging and removal of a built it
temperature sensor. The temperature measurement was
required to adjust the velocity of sound for ambient tem-
perature. It was difficult to build a reasonable radiation
screen for the temperature sensor as part of the overall
sensor. Furthermore, at most automatic stations where
snow depth measurements are required, an air tempera-
ture measurement is usually available.
The first sensor designed and manufactured by CSCC
had the model designation CSMAL01. Only a limited
number of these sensors were built. They had the disad-
vantage of having the built in temperature sensor with a
radiation shield, the power consumption was high and
the sensor enclosure was inadequatefor high humidityen-
vironments. The sensor subsequentlyhadtwo major design
changes,resultinginmodel designationUDG01 (Ultrasonic
Depth Gauge) and most recently the SR50 (Sonic Ranger).
In this presentation, only these two models will be
discussed.

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UDG01 SENSOR

This was the sensor resulting from the first major redesign
of the ultrasonic sensor. The built in temperature sensor
was removedas wellas its associatedradiationshield. This
allowed a streamlining of the sensor packaging. Figure 1
is a graph showing the raw snow depth data for a sensor
located on the Agassiz Ice Cap, on the northern region of
Ellesmere Island. The data are daily readings from May
1988 to April 1989. There are periods when the sensor
was not capable of making a proper reading and the
resulting data value was zero. This would occur if the
sensor was making a reading during a snow fall event or
during periods of blowing snow. Under those circum-
stances, the sensor would receivemultiple echoes and not
be able to make a single determination. There is also a
four month period when the sensor was totally encrusted
with hoar frost and could not make a reading. This is a
common problem with the site and it equally affected the
performance of the anemometer and the temperature ra-
diation shield. Figure 2, is for the same data set but with
all the incorrect readings removed.
Figure 3 is snow depth data for the same site but for
several years. The 1993-1994 season is incomplete be-
cause of missing data due to a severed communications
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