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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 3 The mountain Brellur above Patreksfjörður with its flat and extensive<br />

mountaintop. The Urðir area is located <strong>on</strong> the left side of the photo where there is<br />

a gap in the residential area (photo: Kristín Martha Hák<strong>on</strong>ardóttir).<br />

The mountaintop acts as a huge catchment area for snow drift. Northeasterly winds, which<br />

seem to be dominating in the area according to available data <strong>on</strong> weather c<strong>on</strong>diti<strong>on</strong>s, can<br />

cause str<strong>on</strong>g snow drift into the starting z<strong>on</strong>e and the formati<strong>on</strong> of big cornices (Margreth,<br />

2006). <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 avalanches in<br />

the area and the break up of cornices, as those shown in Figure 4, is known to have initiated<br />

some of the largest avalanches in the area (Jóhanness<strong>on</strong> and others, 1996). Installati<strong>on</strong> of<br />

snow fences and wind baffles is therefore c<strong>on</strong>sidered to be an effective way of reducing the<br />

risk of avalanches at the Urðir area in Patreksfjörður.<br />

Figure 4: Cornices in the cliffs in the avalanche starting z<strong>on</strong>e in Patreksfjörður in 1995. The<br />

height of the cornices is estimated 5−10 m (photo: courtesy of Þröstur Reyniss<strong>on</strong>).<br />

Margreth (2006) designed a scheme combining snow fences and wind baffles for the Urðir<br />

area in an appraisal study for avalanche defences for the Urðir and Klif areas in Patreksfjörður.<br />

The proposed snow drift measures are shown in Figure 5. They c<strong>on</strong>sist of 25−30 wind<br />

baffles to break up cornice formati<strong>on</strong> and 1700 m of snow fences positi<strong>on</strong>ed normal to the<br />

prevailing wind directi<strong>on</strong> in multiple rows. The wind directi<strong>on</strong>, wind speed and the local snow<br />

distributi<strong>on</strong> need to be analysed in advance for an effective applicati<strong>on</strong> of the snow drift<br />

measures, followed by testing the functi<strong>on</strong> of a small porti<strong>on</strong> of snow fences and wind baffles<br />

prior to the final c<strong>on</strong>structi<strong>on</strong>.<br />

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

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