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International Symposium on Mitigative Measures against Snow ...

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<str<strong>on</strong>g>Internati<strong>on</strong>al</str<strong>on</strong>g> <str<strong>on</strong>g>Symposium</str<strong>on</strong>g> <strong>on</strong> <strong>Mitigative</strong> <strong>Measures</strong> <strong>against</strong> <strong>Snow</strong> Avalanches<br />

Egilsstaðir, Iceland, March 11–14, 2008<br />

Figure 2 Overview of the snow net test site “Hafelekar”.<br />

2.1.1 Measurements <strong>on</strong> the snow nets<br />

Figure 3 shows the measuring equipment installed <strong>on</strong> the snow nets. Measuring instruments<br />

were <strong>on</strong>ly installed <strong>on</strong> <strong>on</strong>e half of each net type. The axial and transverse forces in the base<br />

point of the posts are measured with a load measuring pin of the type Magtrol LB236. For the<br />

measurement of the tensi<strong>on</strong> forces in the anchors and all wire ropes, a special sensor<br />

c<strong>on</strong>taining HBM KMR200 or KMR300 has been designed at the BFW. The inclinati<strong>on</strong> of the<br />

supporting net and the posts is recorded by a biaxial inclinosensor HLPlanar NS-25/E2. The<br />

data is recorded every thirty minutes with Campbell data loggers that are fixed <strong>on</strong> the posts.<br />

Every four hours the measured values are directly transferred to an internet platform and<br />

automatically edited in a graphical way.<br />

2.1.2 Measurements <strong>on</strong> the snow cover<br />

During field visits the snow distributi<strong>on</strong>, snow depth and snow density were measured.<br />

Besides the manual observati<strong>on</strong> the temporal variati<strong>on</strong> of snow depth was documented with a<br />

terrestrial laser scanner (Riegl company, LPM-i2k). Laser ranging is based <strong>on</strong> measuring the<br />

time-of-flight of a short laser signal from the instruments’ transmitter to the target and back to<br />

the receiver. A detailed descripti<strong>on</strong> of the laser scanner is given by Wiatr (2007). In order to<br />

positi<strong>on</strong> the laser scanner five reflectors (tiepoints) have been installed within the test site.<br />

Due to the high reflectivity this points appear as bright spots in the laser scan image, so the<br />

exact coordinates of the laser scanner can be determined. The laser output is an irregular<br />

scatter-plot, therefore data is transformed to a regular grid with the Nearest Neighbour<br />

interpolati<strong>on</strong>. To verify the results of the laser measurements, which means the difference<br />

between summer and winter DEM (digital elevati<strong>on</strong> model), snow depth was measured with<br />

probing at several positi<strong>on</strong>s within the test site.<br />

42 <strong>Snow</strong> loads <strong>on</strong> defensive snow net systems

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