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...

Full description

Bibliographic Details
Main Authors: Wendleder, Anna, Gnatzy, Gregor, Schmitt, Andreas, Abdullahi, Sahra
Format: Conference Object
Language:unknown
Published: 2021
Subjects:
Online Access:https://elib.dlr.de/141673/
_version_ 1835014814404968448
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/