Dru Posted July 23, 2004 Posted July 23, 2004 Impacts Gruber, S., M. Hoelzle and W. Haeberli. 2004. Permafrost thaw and destabilization of Alpine rock walls in the hot summer of 2003. GRL 31, L13504, doi: 10.1029/2004GL020051, 2004. Gruber et al. consider whether the unusual summer of 2003 in Europe is an indicator of things to come under climate change. The summer of 2003 was ~3°C warmer in Switzerland than the 1961-90 average and this coincided with exceptional rock fall activity, especially at high elevations and on north-facing slopes. In the absence of unusual precipitation or other possible effects on slope stability, the authors hypothesize that rapid degradation of mountain permafrost is the likely cause. They investigated this hypothesis using observations of air and near surface temperature in steep rock faces in an energy balance model to simulate summer thaw for the period 1982-2002 and compared it to 2003 rates. The modelled thaw of 2003 exceeded the maximum of the previous 21 years. , Authors conclude that these findings are cause for concern with respect to future warming, suggesting that the locations, magnitudes and frequencies of rock wall instabilities are likely to expand beyond the ranges of historic variability. This instability has implications for infrastructure, tourism and public safety in alpine ranges. Better buy a new helmet... Quote
Stemalot Posted July 23, 2004 Posted July 23, 2004 yes...it's about time you up grade the ugly old thing! Quote
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