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• W3145965170 abstract "The response of high latitude periglacial environments to climate change is very particular for two main reasons: the rise in temperature is more pronounced than another bioclimatic zones, and the presence of permanently frozen ground. Permafrost determines a very particular hydrological functioning. In areas where permafrost is thick and continuous, it can be considered to act as an impermeable barrier blocking water infiltration. The specificity of surface hydrological functioning partly explains the extent of wetlands in periglacial regions. This chapter provides the response of Arctic fluvial hydrosystems to ongoing climate change. Rivers in the periglacial region freeze for several months in winter. River ice depends mainly on air temperatures, but also on the presence and thickness of snow, which has an insulating effect. Riverbeds play an important economic role, and navigation is at the forefront of this. The safety of navigation depends on water levels." @default.
• W3145965170 created "2021-04-13" @default.
• W3145965170 creator A5087460831 @default.
• W3145965170 date "2021-03-26" @default.
• W3145965170 modified "2023-10-12" @default.
• W3145965170 title "The Impacts of Climate Change on the Hydrological Dynamics of High Latitude Periglacial Environments" @default.
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• W3145965170 doi "https://doi.org/10.1002/9781119817925.ch7" @default.
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