Terrestrial processes affecting unlithified coastal erosion disparities in central fjords of Svalbard
Terrestrial influences of coastal cliff morphology and hydrological impact on coastal erosion in unlithified cliff sediments in the inner fjords of Svalbard are assessed. Differential global positioning system measurements have been taken annually over the past two to four years at four field sites...
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Taylor & Francis Open
2015
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Online Access: | http://hdl.handle.net/11250/2462388 https://doi.org/10.3402/polar.v34.24122 |
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ftntnutrondheimi:oai:ntnuopen.ntnu.no:11250/2462388 2023-05-15T18:02:38+02:00 Terrestrial processes affecting unlithified coastal erosion disparities in central fjords of Svalbard Sessford, Evangeline Bæverfjord, Maj Gøril Glåmen Hormes, Anne 2015 http://hdl.handle.net/11250/2462388 https://doi.org/10.3402/polar.v34.24122 eng eng Taylor & Francis Open Polar Research. 2015, 34 . urn:issn:0800-0395 http://hdl.handle.net/11250/2462388 https://doi.org/10.3402/polar.v34.24122 cristin:1278186 Navngivelse-Ikkekommersiell 4.0 Internasjonal http://creativecommons.org/licenses/by-nc/4.0/deed.no CC-BY-NC 16 34 Polar Research Journal article Peer reviewed 2015 ftntnutrondheimi https://doi.org/10.3402/polar.v34.24122 2019-09-17T06:52:43Z Terrestrial influences of coastal cliff morphology and hydrological impact on coastal erosion in unlithified cliff sediments in the inner fjords of Svalbard are assessed. Differential global positioning system measurements have been taken annually over the past two to four years at four field sites in central Svalbard. Measurements were combined with aerial imagery using ArcGIS and the Digital Shoreline Analysis System to calculate rates of erosion in varying geomorphological cliff types. A total of 750 m of coast was divided into two main cliff types: ice-poor and ice-rich tundra cliffs and further divided based on their sediment depositional character and processes currently acting upon sediments. The results show that the most consistent erosion rates occur in the ice-poor cliffs (0.34 m/yr), whereas the most irregular and highest rates occur in ice-rich cliffs (0.47 m/yr). Throughout the study, no waves were observed to reach cliff toes, and therefore erosion rates are considered to reflect an effect of terrestrial processes, rather than wave action. Terrestrial hydrological processes are the driving factors for cliff erosion through winter precipitation for ice-poor cliffs and summer precipitation for ice-rich cliffs. Sediment removal from the base of the cliffs appears to be mainly conducted by sea ice and the ice foot during break up as waves did not reach the base of the studied cliffs during the observed period. publishedVersion Polar Research 201 © 2015 E.G. Sessford et al. This is an Open Access article distributed under the terms of the Creative Commons Attribution-NonCommercial 4.0 International License (http://creativecommons.org/licenses/by-nc/4.0/) Article in Journal/Newspaper Polar Research Sea ice Svalbard Tundra NTNU Open Archive (Norwegian University of Science and Technology) Svalbard Polar Research 34 1 24122 |
institution |
Open Polar |
collection |
NTNU Open Archive (Norwegian University of Science and Technology) |
op_collection_id |
ftntnutrondheimi |
language |
English |
description |
Terrestrial influences of coastal cliff morphology and hydrological impact on coastal erosion in unlithified cliff sediments in the inner fjords of Svalbard are assessed. Differential global positioning system measurements have been taken annually over the past two to four years at four field sites in central Svalbard. Measurements were combined with aerial imagery using ArcGIS and the Digital Shoreline Analysis System to calculate rates of erosion in varying geomorphological cliff types. A total of 750 m of coast was divided into two main cliff types: ice-poor and ice-rich tundra cliffs and further divided based on their sediment depositional character and processes currently acting upon sediments. The results show that the most consistent erosion rates occur in the ice-poor cliffs (0.34 m/yr), whereas the most irregular and highest rates occur in ice-rich cliffs (0.47 m/yr). Throughout the study, no waves were observed to reach cliff toes, and therefore erosion rates are considered to reflect an effect of terrestrial processes, rather than wave action. Terrestrial hydrological processes are the driving factors for cliff erosion through winter precipitation for ice-poor cliffs and summer precipitation for ice-rich cliffs. Sediment removal from the base of the cliffs appears to be mainly conducted by sea ice and the ice foot during break up as waves did not reach the base of the studied cliffs during the observed period. publishedVersion Polar Research 201 © 2015 E.G. Sessford et al. This is an Open Access article distributed under the terms of the Creative Commons Attribution-NonCommercial 4.0 International License (http://creativecommons.org/licenses/by-nc/4.0/) |
format |
Article in Journal/Newspaper |
author |
Sessford, Evangeline Bæverfjord, Maj Gøril Glåmen Hormes, Anne |
spellingShingle |
Sessford, Evangeline Bæverfjord, Maj Gøril Glåmen Hormes, Anne Terrestrial processes affecting unlithified coastal erosion disparities in central fjords of Svalbard |
author_facet |
Sessford, Evangeline Bæverfjord, Maj Gøril Glåmen Hormes, Anne |
author_sort |
Sessford, Evangeline |
title |
Terrestrial processes affecting unlithified coastal erosion disparities in central fjords of Svalbard |
title_short |
Terrestrial processes affecting unlithified coastal erosion disparities in central fjords of Svalbard |
title_full |
Terrestrial processes affecting unlithified coastal erosion disparities in central fjords of Svalbard |
title_fullStr |
Terrestrial processes affecting unlithified coastal erosion disparities in central fjords of Svalbard |
title_full_unstemmed |
Terrestrial processes affecting unlithified coastal erosion disparities in central fjords of Svalbard |
title_sort |
terrestrial processes affecting unlithified coastal erosion disparities in central fjords of svalbard |
publisher |
Taylor & Francis Open |
publishDate |
2015 |
url |
http://hdl.handle.net/11250/2462388 https://doi.org/10.3402/polar.v34.24122 |
geographic |
Svalbard |
geographic_facet |
Svalbard |
genre |
Polar Research Sea ice Svalbard Tundra |
genre_facet |
Polar Research Sea ice Svalbard Tundra |
op_source |
16 34 Polar Research |
op_relation |
Polar Research. 2015, 34 . urn:issn:0800-0395 http://hdl.handle.net/11250/2462388 https://doi.org/10.3402/polar.v34.24122 cristin:1278186 |
op_rights |
Navngivelse-Ikkekommersiell 4.0 Internasjonal http://creativecommons.org/licenses/by-nc/4.0/deed.no |
op_rightsnorm |
CC-BY-NC |
op_doi |
https://doi.org/10.3402/polar.v34.24122 |
container_title |
Polar Research |
container_volume |
34 |
container_issue |
1 |
container_start_page |
24122 |
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1766173022364893184 |