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The Polar Record Glacier

Bibliographic Data

ID9219441
AuthorsLiz Cruwys (University of Cambridge), Gareth Rees (0000-0003-2938-7491), W G Rees (0000-0001-6020-1232, University of Cambridge)
Year2001
Volume37
Issue201
Pages154-156
Publication date2001-04-01
Open AccessYes
TypeARTICLE
VenuePolar Record (JOURNAL)
Journal identifiersISSN: 0032-2474 • E-ISSN: 1475-3057
PublisherCambridge University Press (CUP) (PUBLISHER)
DOI10.1017/s0032247400026991
OpenAlexW1989114723
LanguageEN

The name for the Polar Record Glacier was approved in February 1952. At that time, the glacier was reported to possess an ice tongue that flowed into Sandefjord Ice Bay. In autumn 2000, AVHRR images were examined to assess whether the Polar Record ice tongue was still extant. It was found that there is an ice feature currently about 15 miles in length at the end of the glacier, although its orientation has changed since it was first surveyed in 1947. A fissure indicates that the tongue has calved to form an iceberg that is probably grounded

Antarctic sea ice · Bay · Biology · Cryosphere · Extant taxon · Feature (linguistics) · Geography · Glacier · Glacier morphology · Ice calving · Ice tongue · Iceberg · Physical geography · Polar · Sea ice · Tidewater glacier cycle · Climate change and permafrost · Cryospheric studies and observations · Geology · Oceanography · Paleontology · Polar Research and Ecology

Highly citedNo

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