IEEE Geoscience and Remote Sensing Magazine - March 2020 - 58

Benchmarks
>1 m/y
>10 m/y
<1 m/y
<10 cm/y

Main Scarp

Secondary Scarp
Topographic
Station + Radar

0

100

200 (m)

FIGURE 20. A plan of the depletion zone, which shows the landslide main scarps and the locations of the radar and topographic systems [2].

Topographic Station

Track

Transmitting Antenna

Radar Receiving Antenna

FIGURE 21. A field setup of the instrumentation at the test site and

details of the motorized sled, including its antennas [2].
spatial correlation during the whole experiment duration
was good. However, critical time intervals still exist, particularly around midday, when the temperature is very high
(therefore, the tolerance on meteorological errors is lower)
and wind typically blows stronger.
LANDSLIDE MONITORING
The Tessina landslide, located in the northeastern Italian
Alps near the city of Belluno, was first triggered in October
1960. It is a complex landslide with a source area affected
58

by rototranslational slides, which develop downhill into a
mudflow through a steep channel. The landslide developed
in the Tessina valley between the altitudes of 1,220 and
625 m, with a total longitudinal extension of nearly 3 km,
a maximum width of roughly 500 m, and a total volume of
approximately 7 million  m 3 . The mudflow skimmed over
the village of Funes and stretched downhill as far as the village of Lamosano.
The GB-SAR apparatus used in this application is the
portable device LiSA. The measurement campaign on the
Tessina landslide was carried out between 25 September
and 13 October 2000. The instrumentation was installed
at an elevation of 997.3 m in a stable area on the opposite slope in front of the depletion zone, which was completely visible at an average distance of 500 m, as shown
in Figure 20.
The arrangement of the instrumentation in the field is
presented in Figure 21. The rail was mounted on a concrete
wall, and the electronic apparatuses for acquisition and visualization were placed in an existing building.
Figure 22 shows the scenario observed by the radar
instrument, which corresponds to the upper part of the
landslide (the zone of depletion and part of the upper accumulation zone). Each white dot in the figure indicates a
benchmark, position of which is measured with millimetric
IEEE GEOSCIENCE AND REMOTE SENSING MAGAZINE

MARCH 2020



IEEE Geoscience and Remote Sensing Magazine - March 2020

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