Landscape–seascape dynamics in the isthmus between Sørkapp Land and the rest of Spitsbergen: Will a new big Arctic island form?

Transformation of the glaciated isthmus between Sørkapp Land and the rest of Spitsbergen since 1900 is described. The landscape–seascape dynamics depends on the glacial recession determined by climate warming after the Little Ice Age (i.e., since the beginning of the twentieth century, and especiall...

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Published in:AMBIO
Main Authors: Ziaja, Wieslaw, Ostafin, Krzysztof
Format: Text
Language:English
Published: Springer Netherlands 2014
Subjects:
Online Access:http://www.ncbi.nlm.nih.gov/pmc/articles/PMC4392015
http://www.ncbi.nlm.nih.gov/pubmed/25384599
https://doi.org/10.1007/s13280-014-0572-1
id ftpubmed:oai:pubmedcentral.nih.gov:4392015
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spelling ftpubmed:oai:pubmedcentral.nih.gov:4392015 2023-05-15T15:03:07+02:00 Landscape–seascape dynamics in the isthmus between Sørkapp Land and the rest of Spitsbergen: Will a new big Arctic island form? Ziaja, Wieslaw Ostafin, Krzysztof 2014-11-11 http://www.ncbi.nlm.nih.gov/pmc/articles/PMC4392015 http://www.ncbi.nlm.nih.gov/pubmed/25384599 https://doi.org/10.1007/s13280-014-0572-1 en eng Springer Netherlands http://www.ncbi.nlm.nih.gov/pmc/articles/PMC http://www.ncbi.nlm.nih.gov/pubmed/25384599 http://dx.doi.org/10.1007/s13280-014-0572-1 © The Author(s) 2014 Open AccessThis article is distributed under the terms of the Creative Commons Attribution License which permits any use, distribution, and reproduction in any medium, provided the original author(s) and the source are credited. CC-BY Report Text 2014 ftpubmed https://doi.org/10.1007/s13280-014-0572-1 2015-04-19T00:02:28Z Transformation of the glaciated isthmus between Sørkapp Land and the rest of Spitsbergen since 1900 is described. The landscape–seascape dynamics depends on the glacial recession determined by climate warming after the Little Ice Age (i.e., since the beginning of the twentieth century, and especially since the 1980s). The isthmus has been narrowed from 28 km in 1899–1900 to 6.2 km in 2013, and lowered by 60–200 m from 1936 to 2005. Two isthmus’ glaciers will have melted, given the current thermic conditions, by 2030–2035. It cannot be ruled out that Sørkapp Land will become an island after that period, because the altitude of the glaciers’ bedrock is close to the sea level. The disappearance of this huge ice mass, even without origin of a sound and island, will lead to a great transformation of the landscape and the ecosystem. Text Arctic Sørkapp Land Spitsbergen PubMed Central (PMC) Arctic Arctic Island ENVELOPE(-74.766,-74.766,62.234,62.234) Sørkapp Land ENVELOPE(16.523,16.523,76.801,76.801) AMBIO 44 4 332 342
institution Open Polar
collection PubMed Central (PMC)
op_collection_id ftpubmed
language English
topic Report
spellingShingle Report
Ziaja, Wieslaw
Ostafin, Krzysztof
Landscape–seascape dynamics in the isthmus between Sørkapp Land and the rest of Spitsbergen: Will a new big Arctic island form?
topic_facet Report
description Transformation of the glaciated isthmus between Sørkapp Land and the rest of Spitsbergen since 1900 is described. The landscape–seascape dynamics depends on the glacial recession determined by climate warming after the Little Ice Age (i.e., since the beginning of the twentieth century, and especially since the 1980s). The isthmus has been narrowed from 28 km in 1899–1900 to 6.2 km in 2013, and lowered by 60–200 m from 1936 to 2005. Two isthmus’ glaciers will have melted, given the current thermic conditions, by 2030–2035. It cannot be ruled out that Sørkapp Land will become an island after that period, because the altitude of the glaciers’ bedrock is close to the sea level. The disappearance of this huge ice mass, even without origin of a sound and island, will lead to a great transformation of the landscape and the ecosystem.
format Text
author Ziaja, Wieslaw
Ostafin, Krzysztof
author_facet Ziaja, Wieslaw
Ostafin, Krzysztof
author_sort Ziaja, Wieslaw
title Landscape–seascape dynamics in the isthmus between Sørkapp Land and the rest of Spitsbergen: Will a new big Arctic island form?
title_short Landscape–seascape dynamics in the isthmus between Sørkapp Land and the rest of Spitsbergen: Will a new big Arctic island form?
title_full Landscape–seascape dynamics in the isthmus between Sørkapp Land and the rest of Spitsbergen: Will a new big Arctic island form?
title_fullStr Landscape–seascape dynamics in the isthmus between Sørkapp Land and the rest of Spitsbergen: Will a new big Arctic island form?
title_full_unstemmed Landscape–seascape dynamics in the isthmus between Sørkapp Land and the rest of Spitsbergen: Will a new big Arctic island form?
title_sort landscape–seascape dynamics in the isthmus between sørkapp land and the rest of spitsbergen: will a new big arctic island form?
publisher Springer Netherlands
publishDate 2014
url http://www.ncbi.nlm.nih.gov/pmc/articles/PMC4392015
http://www.ncbi.nlm.nih.gov/pubmed/25384599
https://doi.org/10.1007/s13280-014-0572-1
long_lat ENVELOPE(-74.766,-74.766,62.234,62.234)
ENVELOPE(16.523,16.523,76.801,76.801)
geographic Arctic
Arctic Island
Sørkapp Land
geographic_facet Arctic
Arctic Island
Sørkapp Land
genre Arctic
Sørkapp Land
Spitsbergen
genre_facet Arctic
Sørkapp Land
Spitsbergen
op_relation http://www.ncbi.nlm.nih.gov/pmc/articles/PMC
http://www.ncbi.nlm.nih.gov/pubmed/25384599
http://dx.doi.org/10.1007/s13280-014-0572-1
op_rights © The Author(s) 2014
Open AccessThis article is distributed under the terms of the Creative Commons Attribution License which permits any use, distribution, and reproduction in any medium, provided the original author(s) and the source are credited.
op_rightsnorm CC-BY
op_doi https://doi.org/10.1007/s13280-014-0572-1
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