Evolution of supraglacial lakes on the Greenland Ice sheet
Polar Regions pass through dramatic changes caused by ongoing climate warming. In many areas, rapid glaciers surface velocity has been observed provoked by supraglacial lakes if their water is able to drain to the ground. This study analyses the evolution of supraglacial lakes on the western margin...
Main Authors: | , , , |
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Format: | Conference Object |
Language: | unknown |
Published: |
2021
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Subjects: | |
Online Access: | https://elib.dlr.de/141673/ |
_version_ | 1835014814404968448 |
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author | Wendleder, Anna Gnatzy, Gregor Schmitt, Andreas Abdullahi, Sahra |
author_facet | Wendleder, Anna Gnatzy, Gregor Schmitt, Andreas Abdullahi, Sahra |
author_sort | Wendleder, Anna |
collection | Unknown |
description | Polar Regions pass through dramatic changes caused by ongoing climate warming. In many areas, rapid glaciers surface velocity has been observed provoked by supraglacial lakes if their water is able to drain to the ground. This study analyses the evolution of supraglacial lakes on the western margin of Greenland near Kangerlussuaq based on a Sentinel-1 data time series from May to December 2017. Additionally, the TanDEM-X Digital Elevation Model is used for the determination of the altitude of the supraglacial lakes. The automatic detection of supraglacial lakes in SAR images is limited due to the very similar backscatter profile of water surfaces and wet glacier areas. Hence, we manually determined the lake boundaries and were able to date the onset, the maximum water level, and the drainage or freeze, respectively. We concluded that the time span between the onset and the maximal water level was two weeks for most of the lakes. Though, lakes above 1200 m a.s.l. freeze rather than draining out. |
format | Conference Object |
genre | glacier Greenland Ice Sheet Kangerlussuaq |
genre_facet | glacier Greenland Ice Sheet Kangerlussuaq |
geographic | Greenland Kangerlussuaq |
geographic_facet | Greenland Kangerlussuaq |
id | ftdlr:oai:elib.dlr.de:141673 |
institution | Open Polar |
language | unknown |
long_lat | ENVELOPE(-55.633,-55.633,72.633,72.633) |
op_collection_id | ftdlr |
op_relation | Wendleder, Anna und Gnatzy, Gregor und Schmitt, Andreas und Abdullahi, Sahra (2021) Evolution of supraglacial lakes on the Greenland Ice sheet. In: 13th European Conference on Synthetic Aperture Radar, EUSAR 2021. EUSAR 2021, 2021-03-29 - 2021-04-01, Online Event. ISBN 978-380075457-1. ISSN 2197-4403. |
publishDate | 2021 |
record_format | openpolar |
spelling | ftdlr:oai:elib.dlr.de:141673 2025-06-15T14:27:42+00:00 Evolution of supraglacial lakes on the Greenland Ice sheet Wendleder, Anna Gnatzy, Gregor Schmitt, Andreas Abdullahi, Sahra 2021-03 https://elib.dlr.de/141673/ unknown Wendleder, Anna und Gnatzy, Gregor und Schmitt, Andreas und Abdullahi, Sahra (2021) Evolution of supraglacial lakes on the Greenland Ice sheet. In: 13th European Conference on Synthetic Aperture Radar, EUSAR 2021. EUSAR 2021, 2021-03-29 - 2021-04-01, Online Event. ISBN 978-380075457-1. ISSN 2197-4403. Dynamik der Landoberfläche Konferenzbeitrag NonPeerReviewed 2021 ftdlr 2025-06-04T04:58:04Z Polar Regions pass through dramatic changes caused by ongoing climate warming. In many areas, rapid glaciers surface velocity has been observed provoked by supraglacial lakes if their water is able to drain to the ground. This study analyses the evolution of supraglacial lakes on the western margin of Greenland near Kangerlussuaq based on a Sentinel-1 data time series from May to December 2017. Additionally, the TanDEM-X Digital Elevation Model is used for the determination of the altitude of the supraglacial lakes. The automatic detection of supraglacial lakes in SAR images is limited due to the very similar backscatter profile of water surfaces and wet glacier areas. Hence, we manually determined the lake boundaries and were able to date the onset, the maximum water level, and the drainage or freeze, respectively. We concluded that the time span between the onset and the maximal water level was two weeks for most of the lakes. Though, lakes above 1200 m a.s.l. freeze rather than draining out. Conference Object glacier Greenland Ice Sheet Kangerlussuaq Unknown Greenland Kangerlussuaq ENVELOPE(-55.633,-55.633,72.633,72.633) |
spellingShingle | Dynamik der Landoberfläche Wendleder, Anna Gnatzy, Gregor Schmitt, Andreas Abdullahi, Sahra Evolution of supraglacial lakes on the Greenland Ice sheet |
title | Evolution of supraglacial lakes on the Greenland Ice sheet |
title_full | Evolution of supraglacial lakes on the Greenland Ice sheet |
title_fullStr | Evolution of supraglacial lakes on the Greenland Ice sheet |
title_full_unstemmed | Evolution of supraglacial lakes on the Greenland Ice sheet |
title_short | Evolution of supraglacial lakes on the Greenland Ice sheet |
title_sort | evolution of supraglacial lakes on the greenland ice sheet |
topic | Dynamik der Landoberfläche |
topic_facet | Dynamik der Landoberfläche |
url | https://elib.dlr.de/141673/ |