HUSCAP logo Hokkaido Univ. logo

Hokkaido University Collection of Scholarly and Academic Papers >
Institute of Low Temperature Science >
Peer-reviewed Journal Articles, etc >

The influence of the presence and drainage of an ice-marginal lake on the flow of Gornergletscher, Switzerland

Files in This Item:
JoG56-196_278-286.pdf645.35 kBPDFView/Open
Please use this identifier to cite or link to this item:http://hdl.handle.net/2115/49862

Title: The influence of the presence and drainage of an ice-marginal lake on the flow of Gornergletscher, Switzerland
Authors: Riesen, Patrick Browse this author
Sugiyama, Shin Browse this author →KAKEN DB
Funk, Martin Browse this author
Issue Date: Jun-2010
Publisher: International Glaciological Society
Journal Title: Journal of Glaciology
Volume: 56
Issue: 196
Start Page: 278
End Page: 286
Publisher DOI: 10.3189/002214310791968575
Abstract: Gornergletscher, Switzerland, is located adjacent to the marginal lake Gornersee, which periodically drains. We measured glacier ice-flow velocities during two drainage events of the lake, in 2004 and 2006. The common feature of these events was that, during both, Gornersee filled to its maximum level and then overflowed. The events differed in that in 2004 Gornersee rapidly drained via a sudden subglacial connection, whereas in 2006 the lake water continued to overflow and slowly discharged into a nearby moulin. We analysed the changes in ice-flow velocities in the vicinity of Gornersee during the two drainage events, using a three-dimensional ice-flow model which is able to (1) simulate locally variable enhanced basal motion of the ice and (2) account for the load and release of water pressure exerted on the ice margin. We demonstrate that the key features of the observed flow changes can be reproduced adequately in the numerical model by considering these two effects as the main mechanisms. We interpret the 2006 flow changes to be dominated by the release of lake water pressure acting on the ice during the lake drainage. The 2004 ice-flow changes can be explained by enhanced basal motion, and the impact of the lake water pressure provides certain clues to some observations insufficiently explained by enhanced basal motion.
Rights: © 2010 International Glaciological Society
Relation: http://www.igsoc.org/
Type: article
URI: http://hdl.handle.net/2115/49862
Appears in Collections:低温科学研究所 (Institute of Low Temperature Science) > 雑誌発表論文等 (Peer-reviewed Journal Articles, etc)

Submitter: 杉山 慎

Export metadata:

OAI-PMH ( junii2 , jpcoar )

MathJax is now OFF:


 

 - Hokkaido University