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- W3141576035 abstract "Periglacial areas are subject to paraperiglacial erosion crises caused by the melting of the permafrost, which are geomorphologically materialized by large scale ground deformations, affecting loose formations such as rocky substrates, slope areas as well as flat areas. In the context of current climate change, knowledge of periglacial processes and the degradation of permafrost are challenges for a global understanding of our planet, the consequences of which do not solely affect periglacial areas. These periglacial spaces are characterized by low temperatures and are often associated with areas of permafrost. This chapter explores the present and past spatial extent of periglacial environments. The processes and forms associated with the paraperiglacial dynamics can be analyzed as a cascading paraperiglacial geosystem. Gravity dynamics increase with global warming and the melting of permafrost walls; they may even affect outdoor tourism activities, particularly mountaineering or the practice of downhill skiing." @default.
- W3141576035 created "2021-04-13" @default.
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- W3141576035 date "2021-03-26" @default.
- W3141576035 modified "2023-10-12" @default.
- W3141576035 title "Spatial Impacts of Climate Change on Periglacial Environments" @default.
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- W3141576035 doi "https://doi.org/10.1002/9781119817925.ch6" @default.
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