Assessment of Morphology Changes of the End Moraine of the Werenskiold Glacier (SW Spitsbergen) Using Active and Passive Remote Sensing Techniques

Wedel Jarlsberg Land in Svalbard is a region with a varied periglacial landscape. In the mountains and in the valleys, the climate is polar with permafrost. During the summer, the near-surface ground layer thaws. The Werenskiold Glacier, together with its end moraine, are located in the central part...

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Bibliographic Details
Published in:Remote Sensing
Main Authors: Tadeusz Głowacki, Damian Kasza
Format: Article in Journal/Newspaper
Language:English
Published: MDPI AG 2021
Subjects:
Q
Ice
Online Access:https://doi.org/10.3390/rs13112134
https://doaj.org/article/f54c20d151a74726ae6cac3b0d956fe1