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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 />

areas, roads and other places where more frequent avalanches are acceptable than around<br />

settlements. The hazard mapping process for ski areas is in many ways different from e.g.<br />

hazard mapping for settlements. Due to the proximity of avalanche starting z<strong>on</strong>es to<br />

c<strong>on</strong>structi<strong>on</strong>s and ski-paths, smaller release areas and more frequent events in known<br />

avalanche paths have to be c<strong>on</strong>sidered. The primary result of exploratory simulati<strong>on</strong>s of small<br />

to medium-size Icelandic avalanches is that they can be simulated with reas<strong>on</strong>able realism<br />

with samosAT.<br />

This approach is based <strong>on</strong> a classificati<strong>on</strong> of the release areas with respect to their physical<br />

properties such as inclinati<strong>on</strong>, aspect and shape. The release areas are assigned a single<br />

number referred to as the starting z<strong>on</strong>e index and are thereby ranked by their likelihood of<br />

releasing an avalanche with a comparatively large run-out. It is not the goal to fully automate<br />

the hazard z<strong>on</strong>ing process. The method is rather an attempt to provide some overview of the<br />

avalanche c<strong>on</strong>diti<strong>on</strong>s of the area under scope and establish a basis for further analysis.<br />

3.3 Design of deflecting dams<br />

The effects of deflecting dams can by assessed with two-dimensi<strong>on</strong>al avalanche models by<br />

simulating the flow of an avalanche with given parameters using digital terrain model that<br />

includes the structure of c<strong>on</strong>siderati<strong>on</strong> and compare it to equivalent simulati<strong>on</strong> <strong>on</strong> untouched<br />

ground. The run-out index scale is useful to determine an appropriate design avalanche and to<br />

simulate the performance of the structure as the events gradually become larger.<br />

Figure 4 Distributi<strong>on</strong> of 2D run-out indices around the opening of the Hnífsdalur-Bolungarvík<br />

tunnel with (blue curves) and without (purple curves) the deflecting dam.<br />

The extent of the January 2005 avalanche is shown as a red curve.<br />

The samosAT has been run to c<strong>on</strong>strain the design of a deflecting dam in relati<strong>on</strong> to a c<strong>on</strong>structi<strong>on</strong><br />

of a road tunnel c<strong>on</strong>necting Hnífsdalur and Bolungarvík in the northwestern part of<br />

Iceland. The planned locati<strong>on</strong> of <strong>on</strong>e of the openings of the tunnel is in an area with well<br />

known history of avalanches. An avalanche recorded in January 2005 was chosen as a<br />

reference event. It reached the 2D run-out index 13 and has an estimated return period of<br />

approximately 15 years.<br />

Gíslas<strong>on</strong> 167

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