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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 />

3. APPLICATION OF TWO-DIMENSIONAL SIMULATIONS<br />

3.1 Hazard z<strong>on</strong>ing of settled areas<br />

As menti<strong>on</strong>ed earlier, the SAMOS model has been used in the hazard z<strong>on</strong>ing process,<br />

described by Jónass<strong>on</strong> and others (1999) and Arnalds and others (2004), for several Icelandic<br />

villages since the year 2000. The two-dimensi<strong>on</strong>al simulati<strong>on</strong> results have proved to be<br />

valuable for showing the directi<strong>on</strong> of the main avalanche t<strong>on</strong>gues from the starting areas, in<br />

particular the influence of ridges and gullies and to estimate the shortening of avalanche runout<br />

due to lateral spreading . The use of the 2D run-out index scale and the parameter axis has<br />

already been implemented to this process in a recent project (Jóhanness<strong>on</strong> and others, 2007).<br />

Figure 3 Comparis<strong>on</strong> of 1D and 2D run-out indices based <strong>on</strong> simulati<strong>on</strong>s with a modified<br />

PCM flow-line model and samosAT, respectively.<br />

As shown in Figure 3, the 1D and 2D run-out indices coincide in middle of the avalanche path<br />

of Seljalandsdalur/Tungudalur, N-W Iceland, where it is rather unc<strong>on</strong>fined and the flow-lines<br />

are roughly parallel, whereas a difference is evident where the landscape is more complex.<br />

This informati<strong>on</strong> can be useful when hazard z<strong>on</strong>es are delineated and make it possible to<br />

better c<strong>on</strong>sider the effect of ridges, gullies and curves in the path.<br />

Hazard maps have already been issued for the most vulnerable villages of Iceland. The maps<br />

are c<strong>on</strong>stantly reviewed, especially in c<strong>on</strong>necti<strong>on</strong> to the c<strong>on</strong>structi<strong>on</strong> of defence structures.<br />

Furthermore, the avalanche hazard is yet to be assessed in many rural areas. Two-dimensi<strong>on</strong>al<br />

avalanche simulati<strong>on</strong>s and 2D run-out indices will be of good use in that process since twodimensi<strong>on</strong>al<br />

avalanche models can provide a good overview and comparis<strong>on</strong> of avalanche<br />

c<strong>on</strong>diti<strong>on</strong>s from <strong>on</strong>e place to another.<br />

3.2 Hazard z<strong>on</strong>ing of unsettled areas<br />

The IMO is developing a methodology to be used for the hazard mapping of public ski areas<br />

in Iceland. Two-dimensi<strong>on</strong>al avalanche simulati<strong>on</strong>s will be important for this work and a first<br />

proposal of guidelines for systematic simulati<strong>on</strong> for avalanche paths in Icelandic ski areas has<br />

been issued (Gíslas<strong>on</strong>, 2007). This methodology could possibly apply for other recreati<strong>on</strong>al<br />

166 Applicati<strong>on</strong> of two-dimensi<strong>on</strong>al avalanche model simulati<strong>on</strong>s at the IMO

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