Investigating methods for identifying paleo surge-type glaciers or highly dynamical ice flows in Trygghamn, west Spitsbergen

Surge-type glaciers exhibit a cyclic behaviour with an ice mass increase in the reservoir area during the inactive, quiescent phase and a rapid transportation of ice during the active, surge phase. In order to interpret the effects of climate change correctly it is important to distinguish between a...

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Bibliographic Details
Main Author: Wallin, Åsa
Format: Bachelor Thesis
Language:English
Published: Stockholms universitet, Institutionen för naturgeografi 2016
Subjects:
Online Access:http://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-131801
Description
Summary:Surge-type glaciers exhibit a cyclic behaviour with an ice mass increase in the reservoir area during the inactive, quiescent phase and a rapid transportation of ice during the active, surge phase. In order to interpret the effects of climate change correctly it is important to distinguish between advances of surge-type glaciers and those of ‘normal’ glaciers, caused by climatic fluctuations. This is particularly important for the Arctic, which is predicted to experience the highest increase in temperature on the planet. The dynamic and mechanism of surge-type glaciers can be used for understanding both modern and past ice sheet dynamic instabilities, threshold behavior and contribution to sea level rise. They are also suggested to be analogues for land-terminating paleo ice streams and surging ice sheet lobes, which makes them highly valuable as research objects. Though in order to understand their behavior, it is important to be able to identify them. In literature the number for surge-type glaciers on Svalbard varies between 13 and 90 %, thus it is important to work out methods, other than physical observations, for identification. Aerial photographs are a powerful tool for the identification and mapping of landforms and ice structures and for reconstructing glacier distribution. Though for mapping of ice facies and structures within the glaciers, which provide important information regarding the glaciers past dynamics, and is an important part of the identification, fieldwork is essential. Fieldwork is also much needed in order to interpret the landforms and their genesis correctly. It is suggested that the use of multiple methods for identifying surges, or highly dynamical ice flows, will improve the result and the reliability will increase. In this thesis two different methods, structural glaciology and glacial geomorphology, have been used for interpreting the past behaviour of the four glaciers in Trygghamna, west Spitsbergen. Structural glaciology provides a way to determine the dynamic of surge-type ...