Origin and location of new Arctic islands and straits due to glacial recession

A total of 34 new islands (each 0.5 km^{2} or above) have appeared due to recession of Arctic glaciers under climate warming since the 1960s. Analysis of maps and satellite images of the Arctic coasts has been a basic method of recognizing these islands. Their origin is the final stage of a process...

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Published in:Ambio
Main Authors: Ziaja, Wiesław, Ostafin, Krzysztof
Format: Article in Journal/Newspaper
Language:English
Published: 2019
Subjects:
Online Access:https://ruj.uj.edu.pl/xmlui/handle/item/64719
https://doi.org/10.1007/s13280-018-1041-z
https://link.springer.com/article/10.1007/s13280-018-1041-z
id ftjagiellonuniir:oai:ruj.uj.edu.pl:item/64719
record_format openpolar
spelling ftjagiellonuniir:oai:ruj.uj.edu.pl:item/64719 2024-05-19T07:34:18+00:00 Origin and location of new Arctic islands and straits due to glacial recession Pochodzenie i położenie nowych wysp i cieśnin arktycznych z powodu recesji lodowców Ziaja, Wiesław Ostafin, Krzysztof 2019 https://ruj.uj.edu.pl/xmlui/handle/item/64719 https://doi.org/10.1007/s13280-018-1041-z https://link.springer.com/article/10.1007/s13280-018-1041-z eng eng AMBIO, T. 48, nr 1, s. 25-34 0044-7447 1654-7209 doi:10.1007/s13280-018-1041-z https://ruj.uj.edu.pl/xmlui/handle/item/64719 https://link.springer.com/article/10.1007/s13280-018-1041-z Udzielam licencji. Uznanie autorstwa 4.0 Międzynarodowa http://creativecommons.org/licenses/by/4.0/legalcode.pl zmiany klimatyczne recesja lodowców prognozy zmian nowe wyspy i cieśniny w Arktyce climate change glacial recession nearest future scenarios new Arctic islands and straits artykuł w czasopiśmie 2019 ftjagiellonuniir https://doi.org/10.1007/s13280-018-1041-z 2024-04-19T00:05:38Z A total of 34 new islands (each 0.5 km^{2} or above) have appeared due to recession of Arctic glaciers under climate warming since the 1960s. Analysis of maps and satellite images of the Arctic coasts has been a basic method of recognizing these islands. Their origin is the final stage of a process which began in the twentieth century. They appear only on the coasts where bedrock elevations above sea level are surrounded by depressions below this level, filled (at least from the landside) with glaciers. Their recession leads to flooding of the depressions by sea water, thus creating straits which separate the new islands from the mainland. Hence, such new islands appear only in Greenland and the European Arctic. Their ecosystems accommodate to new environmental conditions. In the near future, this process will be intensified in a situation of further warming. Article in Journal/Newspaper Arctic Climate change Greenland Jagiellonian University Repository Ambio 48 1 25 34
institution Open Polar
collection Jagiellonian University Repository
op_collection_id ftjagiellonuniir
language English
topic zmiany klimatyczne
recesja lodowców
prognozy zmian
nowe wyspy i cieśniny w Arktyce
climate change
glacial recession
nearest future scenarios
new Arctic islands and straits
spellingShingle zmiany klimatyczne
recesja lodowców
prognozy zmian
nowe wyspy i cieśniny w Arktyce
climate change
glacial recession
nearest future scenarios
new Arctic islands and straits
Ziaja, Wiesław
Ostafin, Krzysztof
Origin and location of new Arctic islands and straits due to glacial recession
topic_facet zmiany klimatyczne
recesja lodowców
prognozy zmian
nowe wyspy i cieśniny w Arktyce
climate change
glacial recession
nearest future scenarios
new Arctic islands and straits
description A total of 34 new islands (each 0.5 km^{2} or above) have appeared due to recession of Arctic glaciers under climate warming since the 1960s. Analysis of maps and satellite images of the Arctic coasts has been a basic method of recognizing these islands. Their origin is the final stage of a process which began in the twentieth century. They appear only on the coasts where bedrock elevations above sea level are surrounded by depressions below this level, filled (at least from the landside) with glaciers. Their recession leads to flooding of the depressions by sea water, thus creating straits which separate the new islands from the mainland. Hence, such new islands appear only in Greenland and the European Arctic. Their ecosystems accommodate to new environmental conditions. In the near future, this process will be intensified in a situation of further warming.
format Article in Journal/Newspaper
author Ziaja, Wiesław
Ostafin, Krzysztof
author_facet Ziaja, Wiesław
Ostafin, Krzysztof
author_sort Ziaja, Wiesław
title Origin and location of new Arctic islands and straits due to glacial recession
title_short Origin and location of new Arctic islands and straits due to glacial recession
title_full Origin and location of new Arctic islands and straits due to glacial recession
title_fullStr Origin and location of new Arctic islands and straits due to glacial recession
title_full_unstemmed Origin and location of new Arctic islands and straits due to glacial recession
title_sort origin and location of new arctic islands and straits due to glacial recession
publishDate 2019
url https://ruj.uj.edu.pl/xmlui/handle/item/64719
https://doi.org/10.1007/s13280-018-1041-z
https://link.springer.com/article/10.1007/s13280-018-1041-z
genre Arctic
Climate change
Greenland
genre_facet Arctic
Climate change
Greenland
op_relation AMBIO, T. 48, nr 1, s. 25-34
0044-7447
1654-7209
doi:10.1007/s13280-018-1041-z
https://ruj.uj.edu.pl/xmlui/handle/item/64719
https://link.springer.com/article/10.1007/s13280-018-1041-z
op_rights Udzielam licencji. Uznanie autorstwa 4.0 Międzynarodowa
http://creativecommons.org/licenses/by/4.0/legalcode.pl
op_doi https://doi.org/10.1007/s13280-018-1041-z
container_title Ambio
container_volume 48
container_issue 1
container_start_page 25
op_container_end_page 34
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