Effects of climate change on high Alpine mountain environments: Evolution of mountaineering routes in the Mont Blanc massif (Western Alps) over half a century

In high alpine environments, glacial shrinkage and permafrost warming due to climate change have significant consequences on mountaineering routes. Few research projects have studied the relationship between climate change and mountaineering; this study attempts to characterize and explain the evolu...

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Main Authors: Jacques Mourey, Mélanie Marcuzzi, Ludovic Ravanel, François Pallandre
Format: Article
Language:English
Published: Taylor & Francis Group 2019-01-01
Series:Arctic, Antarctic, and Alpine Research
Subjects:
Online Access:http://dx.doi.org/10.1080/15230430.2019.1612216
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spelling doaj-0f893c8627e249ad96ca9a03fb342e212020-11-25T01:20:10ZengTaylor & Francis GroupArctic, Antarctic, and Alpine Research1523-04301938-42462019-01-0151117618910.1080/15230430.2019.16122161612216Effects of climate change on high Alpine mountain environments: Evolution of mountaineering routes in the Mont Blanc massif (Western Alps) over half a centuryJacques Mourey0Mélanie Marcuzzi1Ludovic Ravanel2François Pallandre3Université Grenoble Alpes, Université Savoie Mont BlancUniversité Grenoble Alpes, Université Savoie Mont BlancUniversité Grenoble Alpes, Université Savoie Mont BlancÉcole Nationale des Sports de Montagne/École Nationale de Ski et d’AlpinismeIn high alpine environments, glacial shrinkage and permafrost warming due to climate change have significant consequences on mountaineering routes. Few research projects have studied the relationship between climate change and mountaineering; this study attempts to characterize and explain the evolution over the past 40 years of the routes described in The Mont Blanc Massif: The 100 Finest Routes, Gaston Rébuffat’s emblematic guidebook, published in 1973.The main elements studied were the geomorphic and cryospheric changes at work and their impacts on the itinerary’s climbing parameters, determining the manner and possibility for an itinerary to be climbed. Thirty-one interviews, and comparison with other guidebooks, led to the identification of 25 geomorphic and cryospheric changes related to climate change that are affecting mountaineering itineraries. On average, an itinerary has been affected by nine changes. Among the 95 itineraries studied, 93 have been affected by the effects of climate change – 26 of them have been greatly affected; and three no longer exist. Moreover, periods during which these itineraries can be climbed in good conditions in summer have tended to become less predictable and periods of optimal conditions have shifted toward spring and fall, because the itineraries have become more dangerous and technically more challenging.http://dx.doi.org/10.1080/15230430.2019.1612216mountaineeringhigh mountain itinerariesclimate change effectsmont blanc massif
collection DOAJ
language English
format Article
sources DOAJ
author Jacques Mourey
Mélanie Marcuzzi
Ludovic Ravanel
François Pallandre
spellingShingle Jacques Mourey
Mélanie Marcuzzi
Ludovic Ravanel
François Pallandre
Effects of climate change on high Alpine mountain environments: Evolution of mountaineering routes in the Mont Blanc massif (Western Alps) over half a century
Arctic, Antarctic, and Alpine Research
mountaineering
high mountain itineraries
climate change effects
mont blanc massif
author_facet Jacques Mourey
Mélanie Marcuzzi
Ludovic Ravanel
François Pallandre
author_sort Jacques Mourey
title Effects of climate change on high Alpine mountain environments: Evolution of mountaineering routes in the Mont Blanc massif (Western Alps) over half a century
title_short Effects of climate change on high Alpine mountain environments: Evolution of mountaineering routes in the Mont Blanc massif (Western Alps) over half a century
title_full Effects of climate change on high Alpine mountain environments: Evolution of mountaineering routes in the Mont Blanc massif (Western Alps) over half a century
title_fullStr Effects of climate change on high Alpine mountain environments: Evolution of mountaineering routes in the Mont Blanc massif (Western Alps) over half a century
title_full_unstemmed Effects of climate change on high Alpine mountain environments: Evolution of mountaineering routes in the Mont Blanc massif (Western Alps) over half a century
title_sort effects of climate change on high alpine mountain environments: evolution of mountaineering routes in the mont blanc massif (western alps) over half a century
publisher Taylor & Francis Group
series Arctic, Antarctic, and Alpine Research
issn 1523-0430
1938-4246
publishDate 2019-01-01
description In high alpine environments, glacial shrinkage and permafrost warming due to climate change have significant consequences on mountaineering routes. Few research projects have studied the relationship between climate change and mountaineering; this study attempts to characterize and explain the evolution over the past 40 years of the routes described in The Mont Blanc Massif: The 100 Finest Routes, Gaston Rébuffat’s emblematic guidebook, published in 1973.The main elements studied were the geomorphic and cryospheric changes at work and their impacts on the itinerary’s climbing parameters, determining the manner and possibility for an itinerary to be climbed. Thirty-one interviews, and comparison with other guidebooks, led to the identification of 25 geomorphic and cryospheric changes related to climate change that are affecting mountaineering itineraries. On average, an itinerary has been affected by nine changes. Among the 95 itineraries studied, 93 have been affected by the effects of climate change – 26 of them have been greatly affected; and three no longer exist. Moreover, periods during which these itineraries can be climbed in good conditions in summer have tended to become less predictable and periods of optimal conditions have shifted toward spring and fall, because the itineraries have become more dangerous and technically more challenging.
topic mountaineering
high mountain itineraries
climate change effects
mont blanc massif
url http://dx.doi.org/10.1080/15230430.2019.1612216
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