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Published in 2019 at "Boreas"
DOI: 10.1111/bor.12404
Abstract: Pronounced climatic warming associated with the Late Weichselian Pleniglacial‐to‐Lateglacial transition caused considerable environmental changes throughout the former periglacial zones (in Europe ~53°–46°N). During permafrost degradation and subsequent ground subsidence (i.e. thermokarst processes), the landscape changed…
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Keywords:
permafrost;
late weichselian;
thermokarst landscape;
central europe ... See more keywords