Snow and Avalanches in a Climate Warming Context

We first show why current climate forecasting techniques, based on continuous extrapolations, are unreliable in the case of complex arrangements of interacting entities like the atmosphere–ocean system. By contrast, according to the well-established theory of dynamical systems, the observed present...

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Main Author: Louchet, Francois
Format: Book Part
Language:unknown
Published: Oxford University Press 2020
Subjects:
Ice
Online Access:http://dx.doi.org/10.1093/oso/9780198866930.003.0007
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spelling croxfordunivpr:10.1093/oso/9780198866930.003.0007 2023-05-15T16:37:40+02:00 Snow and Avalanches in a Climate Warming Context Louchet, Francois 2020 http://dx.doi.org/10.1093/oso/9780198866930.003.0007 unknown Oxford University Press Snow Avalanches page 57-60 book-chapter 2020 croxfordunivpr https://doi.org/10.1093/oso/9780198866930.003.0007 2022-08-05T10:28:24Z We first show why current climate forecasting techniques, based on continuous extrapolations, are unreliable in the case of complex arrangements of interacting entities like the atmosphere–ocean system. By contrast, according to the well-established theory of dynamical systems, the observed present increase of fluctuations (as heat waves, droughts, tornadoes, forest fires) is a warning signal for an impending discontinuous climate tipping. A comparison with paleoclimatic events suggests that the atmospheric temperature would be likely to increase in this case by 6–9 °C in the next few years. In the transient period, the succession of heavy snow-falls and thawing episodes would favor spontaneous full-depth avalanches with larger run-out distances. After tipping into a new equilibrium, significantly warmer temperatures would shift snow-covered areas towards higher altitudes, probably by more than 1000 m, resulting in closure of a number of ski resorts. Glacier retreat and permafrost thawing would also enhance both ice and rock-fall frequency. Book Part Ice permafrost Oxford University Press (via Crossref) 57 60
institution Open Polar
collection Oxford University Press (via Crossref)
op_collection_id croxfordunivpr
language unknown
description We first show why current climate forecasting techniques, based on continuous extrapolations, are unreliable in the case of complex arrangements of interacting entities like the atmosphere–ocean system. By contrast, according to the well-established theory of dynamical systems, the observed present increase of fluctuations (as heat waves, droughts, tornadoes, forest fires) is a warning signal for an impending discontinuous climate tipping. A comparison with paleoclimatic events suggests that the atmospheric temperature would be likely to increase in this case by 6–9 °C in the next few years. In the transient period, the succession of heavy snow-falls and thawing episodes would favor spontaneous full-depth avalanches with larger run-out distances. After tipping into a new equilibrium, significantly warmer temperatures would shift snow-covered areas towards higher altitudes, probably by more than 1000 m, resulting in closure of a number of ski resorts. Glacier retreat and permafrost thawing would also enhance both ice and rock-fall frequency.
format Book Part
author Louchet, Francois
spellingShingle Louchet, Francois
Snow and Avalanches in a Climate Warming Context
author_facet Louchet, Francois
author_sort Louchet, Francois
title Snow and Avalanches in a Climate Warming Context
title_short Snow and Avalanches in a Climate Warming Context
title_full Snow and Avalanches in a Climate Warming Context
title_fullStr Snow and Avalanches in a Climate Warming Context
title_full_unstemmed Snow and Avalanches in a Climate Warming Context
title_sort snow and avalanches in a climate warming context
publisher Oxford University Press
publishDate 2020
url http://dx.doi.org/10.1093/oso/9780198866930.003.0007
genre Ice
permafrost
genre_facet Ice
permafrost
op_source Snow Avalanches
page 57-60
op_doi https://doi.org/10.1093/oso/9780198866930.003.0007
container_start_page 57
op_container_end_page 60
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