2018
DOI: 10.1007/s13280-018-1041-z
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Origin and location of new Arctic islands and straits due to glacial recession

Abstract: 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 re… Show more

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Cited by 12 publications
(23 citation statements)
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“…In 1995, one of the authors explored a new strait and island in Kongsfjorden, just after their formation. In 2005 and 2016, both authors carried out detailed landscape (including geomorphological) mapping of the coast near the glacial isthmus (formed of two glaciers under recession) being transformed into a new sound between the Sørkapp Land peninsula and the rest of Spitsbergen [5,8,19]. Table 1.…”
Section: Methodsmentioning
confidence: 99%
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“…In 1995, one of the authors explored a new strait and island in Kongsfjorden, just after their formation. In 2005 and 2016, both authors carried out detailed landscape (including geomorphological) mapping of the coast near the glacial isthmus (formed of two glaciers under recession) being transformed into a new sound between the Sørkapp Land peninsula and the rest of Spitsbergen [5,8,19]. Table 1.…”
Section: Methodsmentioning
confidence: 99%
“…The former Mesyatsev Headland-the northwesternmost part of Eva-Liv Island which is the northeasternmost part of the Franz Josef Land archipelago-was transformed into a small new island [8,18] after the formation of a new strait due to the recession of two ice sheets in the west of Eva-Liv Island. This must have happened before August 2nd, 1985.…”
Section: New Island-former Mesyatsev Headland Of Eva-liv Island-franzmentioning
confidence: 99%
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