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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 />

<strong>Snow</strong> drift measures as protecti<strong>on</strong> <strong>against</strong> snow avalanches in<br />

Iceland<br />

Kristín Martha Hák<strong>on</strong>ardóttir 1* , Stefan Margreth 2 , Gunnar Guðni Tómass<strong>on</strong> 4 , Hallgrímur<br />

Daði Indriðas<strong>on</strong> 1 and Skúli Þórðars<strong>on</strong> 3<br />

1 VST C<strong>on</strong>sulting Engineers Ltd., Ármúli 4, IS-104 Reykjavík, ICELAND<br />

2 WSL. Institut fur Schnee- und Lawinenforschung, Fluelastr. 11, CH-7260 Davos Dorf, SWITZERLAND<br />

3 Vegsýn, Reykjavíkurvegur 60, 220 Hafnarfjörður, ICELAND<br />

4 Reykjavík University, Kringlan 1, 103 Reykjavík, ICELAND<br />

*Corresp<strong>on</strong>ding author, e-mail: kmh (at) vst.is<br />

ABSTRACT<br />

<strong>Snow</strong> drift measures have been proposed as a part of a protecti<strong>on</strong> plan above the avalanche<br />

pr<strong>on</strong>e Urðir area in Patreksfjörður in western Iceland. The appraisal study was c<strong>on</strong>ducted by<br />

VST C<strong>on</strong>sulting engineers Ltd. in co-operati<strong>on</strong> with a specialist <strong>on</strong> snow drift measures at the<br />

SLF in Switzerland. <strong>Snow</strong> drift is the main reas<strong>on</strong> for snow accumulati<strong>on</strong> in starting z<strong>on</strong>es of<br />

avalanches in the area and the break up of cornices is known to have initiated some of the<br />

largest avalanches in the area. The flat mountain plateau above Patreksfjörður, coupled with<br />

the local weather c<strong>on</strong>diti<strong>on</strong>s lead to feasible c<strong>on</strong>diti<strong>on</strong>s for the c<strong>on</strong>structi<strong>on</strong> of snow fences in<br />

order to reduce snow drift into the avalanche starting z<strong>on</strong>e below the mountain plateau. Wind<br />

baffles at the edge of the plateau are additi<strong>on</strong>ally proposed to prevent the formati<strong>on</strong> of large<br />

c<strong>on</strong>tinuous cornices in the cliffs above the starting z<strong>on</strong>e. High wind speeds <strong>on</strong> mountaintops<br />

in Iceland pose a problem to the design of the structures. The snow drift measures are<br />

c<strong>on</strong>sidered to be extremely valuable to additi<strong>on</strong>ally reduce the avalanche risk in the complex<br />

situati<strong>on</strong> of c<strong>on</strong>structing suitable protecti<strong>on</strong> dams in the Urðir area. <strong>Snow</strong> drift measures have<br />

not yet been built as integrative avalanche protecti<strong>on</strong>s above inhabited areas in Iceland and<br />

experience <strong>on</strong> optimal design and durability is thus lacking.<br />

1. INTRODUCTION<br />

The avalanche situati<strong>on</strong> in the Urðir area above Patreksfjörður is severe. The risk associated<br />

with the avalanche path is <strong>on</strong>e of the highest of such paths in Iceland creating an<br />

approximately 200 m wide gap in the village where the older part is to the east and a newer<br />

residential area to the west of the path. Residential houses have been built increasingly closer<br />

to the avalanche path and the mountainside making it hard and complicated to protect the area<br />

sufficiently with dams. The plateau above the mountain acts as a large catchment area for<br />

snow drift which accumulates in the starting z<strong>on</strong>e below the plateau. The c<strong>on</strong>diti<strong>on</strong>s at the<br />

mountaintop are favourable for c<strong>on</strong>structing snow fences to prevent snow from drifting into<br />

the starting z<strong>on</strong>e.<br />

<strong>Snow</strong> drift measures have not been built in Iceland yet as snow avalanche defence measures<br />

above inhabited areas, they are however widely used as such elsewhere, e.g. in the Alps. The<br />

climatic c<strong>on</strong>diti<strong>on</strong>s in Iceland differ somewhat from the Alps, especially regarding higher<br />

wind speeds <strong>on</strong> mountain tops. The high wind speeds could pose problems to durability and<br />

effectiveness of the structures.<br />

Hák<strong>on</strong>ardóttir, Margreth, Tómass<strong>on</strong>, Indriðas<strong>on</strong> and Þórðars<strong>on</strong> 85

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