Design of a scanning laser meter for monitoring the spatio-temporal evolution of snow depth and its application in the Alps and in Antarctica
Although both the temporal and spatial variations of the snow depth are usually of interest for numerous applications, available measurement techniques are either space-oriented (e.g. terrestrial laser scans) or time-oriented (e.g. ultrasonic ranging probe). Because of snow heterogeneity, measuring...
Main Authors: | , , , |
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Format: | Article |
Language: | English |
Published: |
Copernicus Publications
2016-07-01
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Series: | The Cryosphere |
Online Access: | http://www.the-cryosphere.net/10/1495/2016/tc-10-1495-2016.pdf |
Summary: | Although both the temporal and spatial variations of the snow depth are usually of interest for numerous
applications, available measurement techniques are either space-oriented
(e.g. terrestrial laser scans) or time-oriented (e.g. ultrasonic ranging
probe). Because of snow heterogeneity, measuring depth in a single point is
insufficient to provide accurate and representative estimates. We present a
cost-effective automatic instrument to acquire spatio-temporal variations of
snow depth. The device comprises a laser meter mounted on a 2-axis stage and
can scan ≈ 200 000 points over an area of 100–200 m<sup>2</sup> in
4 h. Two instruments, installed in Antarctica (Dome C) and the French
Alps (Col de Porte), have been operating continuously and unattended over
2015 with a success rate of 65 and 90 % respectively. The precision of
single point measurements and long-term stability were evaluated to be about
1 cm and the accuracy to be 5 cm or better. The spatial
variability in the scanned area reached 7–10 cm (root mean square)
at both sites, which means that the number of measurements is sufficient to
average out the spatial variability and yield precise mean snow depth. With
such high precision, it was possible for the first time at Dome C
to (1) observe a 3-month period of regular and slow increase of snow depth
without apparent link to snowfalls and (2) highlight that most of the annual
accumulation stems from a single event although several snowfall and strong
wind events were predicted by the ERA-Interim reanalysis. Finally the paper
discusses the benefit of laser scanning compared to multiplying single-point
sensors in the context of monitoring snow depth. |
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ISSN: | 1994-0416 1994-0424 |