UAV-based remote sensing of immediate changes in geomorphology following a glacial lake outburst flood at the Zackenberg river, northeast Greenland

Two detailed geomorphological maps (1:2000) depicting landscape changes as a result of a glacial lake outburst flood were produced for the 2.1-km-long section of the Zackenberg river, NE Greenland. The maps document the riverscape before the flood (5 August 2017) and immediately after the flood (8 A...

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Main Authors: Aleksandra M. Tomczyk, Marek W. Ewertowski
Format: Article
Language:English
Published: Taylor & Francis Group 2020-01-01
Series:Journal of Maps
Subjects:
gis
Online Access:http://dx.doi.org/10.1080/17445647.2020.1749146
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spelling doaj-ad9b32a483cd4d6981701791a051000e2021-07-06T12:16:07ZengTaylor & Francis GroupJournal of Maps1744-56472020-01-011618610010.1080/17445647.2020.17491461749146UAV-based remote sensing of immediate changes in geomorphology following a glacial lake outburst flood at the Zackenberg river, northeast GreenlandAleksandra M. Tomczyk0Marek W. Ewertowski1Faculty of Geographical and Geological Sciences, Adam Mickiewicz UniversityFaculty of Geographical and Geological Sciences, Adam Mickiewicz UniversityTwo detailed geomorphological maps (1:2000) depicting landscape changes as a result of a glacial lake outburst flood were produced for the 2.1-km-long section of the Zackenberg river, NE Greenland. The maps document the riverscape before the flood (5 August 2017) and immediately after the flood (8 August 2017), illustrating changes to the riverbanks and morphology of the channel. A series of additional maps (1:800) represent case studies of different types of riverbank responses, emphasising the importance of the lateral thermo-erosion and bank collapsing as significant immediate effects of the flood. The average channel width increased from 40.75 m pre-flood to 44.59 m post-flood, whereas the length of active riverbanks decreased from 1729 to 1657 m. The new deposits related to 2017 flood covered 93,702 m2. The developed maps demonstrated the applicability of small Unmanned Aerial Vehicles (UAVs) for investigating the direct effects of floods, even in the harsh Arctic environment.http://dx.doi.org/10.1080/17445647.2020.1749146dronegismappingbank erosionarctic
collection DOAJ
language English
format Article
sources DOAJ
author Aleksandra M. Tomczyk
Marek W. Ewertowski
spellingShingle Aleksandra M. Tomczyk
Marek W. Ewertowski
UAV-based remote sensing of immediate changes in geomorphology following a glacial lake outburst flood at the Zackenberg river, northeast Greenland
Journal of Maps
drone
gis
mapping
bank erosion
arctic
author_facet Aleksandra M. Tomczyk
Marek W. Ewertowski
author_sort Aleksandra M. Tomczyk
title UAV-based remote sensing of immediate changes in geomorphology following a glacial lake outburst flood at the Zackenberg river, northeast Greenland
title_short UAV-based remote sensing of immediate changes in geomorphology following a glacial lake outburst flood at the Zackenberg river, northeast Greenland
title_full UAV-based remote sensing of immediate changes in geomorphology following a glacial lake outburst flood at the Zackenberg river, northeast Greenland
title_fullStr UAV-based remote sensing of immediate changes in geomorphology following a glacial lake outburst flood at the Zackenberg river, northeast Greenland
title_full_unstemmed UAV-based remote sensing of immediate changes in geomorphology following a glacial lake outburst flood at the Zackenberg river, northeast Greenland
title_sort uav-based remote sensing of immediate changes in geomorphology following a glacial lake outburst flood at the zackenberg river, northeast greenland
publisher Taylor & Francis Group
series Journal of Maps
issn 1744-5647
publishDate 2020-01-01
description Two detailed geomorphological maps (1:2000) depicting landscape changes as a result of a glacial lake outburst flood were produced for the 2.1-km-long section of the Zackenberg river, NE Greenland. The maps document the riverscape before the flood (5 August 2017) and immediately after the flood (8 August 2017), illustrating changes to the riverbanks and morphology of the channel. A series of additional maps (1:800) represent case studies of different types of riverbank responses, emphasising the importance of the lateral thermo-erosion and bank collapsing as significant immediate effects of the flood. The average channel width increased from 40.75 m pre-flood to 44.59 m post-flood, whereas the length of active riverbanks decreased from 1729 to 1657 m. The new deposits related to 2017 flood covered 93,702 m2. The developed maps demonstrated the applicability of small Unmanned Aerial Vehicles (UAVs) for investigating the direct effects of floods, even in the harsh Arctic environment.
topic drone
gis
mapping
bank erosion
arctic
url http://dx.doi.org/10.1080/17445647.2020.1749146
work_keys_str_mv AT aleksandramtomczyk uavbasedremotesensingofimmediatechangesingeomorphologyfollowingaglaciallakeoutburstfloodatthezackenbergrivernortheastgreenland
AT marekwewertowski uavbasedremotesensingofimmediatechangesingeomorphologyfollowingaglaciallakeoutburstfloodatthezackenbergrivernortheastgreenland
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