Temporal evolution of crack propagation propensity in snow in relation to slab and weak layer properties

If a weak snow layer below a cohesive slab is present in the snow cover, unstable snow conditions can prevail for days or even weeks. We monitored the temporal evolution of a weak layer of faceted crystals as well as the overlaying slab layers at the location of an automatic weather station in the S...

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Detaylı Bibliyografya
Asıl Yazarlar: J. Schweizer, B. Reuter, A. van Herwijnen, B. Richter, J. Gaume
Materyal Türü: Makale
Dil:English
Baskı/Yayın Bilgisi: Copernicus Publications 2016-11-01
Seri Bilgileri:The Cryosphere
Online Erişim:http://www.the-cryosphere.net/10/2637/2016/tc-10-2637-2016.pdf