North Greenland ice islands
Abstract Large tabular icebergs derived from the glaciers which drain the north fringe of Greenland's Inland Iceoccur in many North Greenland fjords. Many have undulating surface topography resembling that of the ice islands calved from Ellesmere Island ice shelves. Semi-permanent sea ice in No...
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Cambridge University Press (CUP)
1989
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Online Access: | http://dx.doi.org/10.1017/s0032247400010809 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0032247400010809 |
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crcambridgeupr:10.1017/s0032247400010809 2024-09-15T17:53:28+00:00 North Greenland ice islands Higgins, A. K. 1989 http://dx.doi.org/10.1017/s0032247400010809 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0032247400010809 en eng Cambridge University Press (CUP) https://www.cambridge.org/core/terms Polar Record volume 25, issue 154, page 207-212 ISSN 0032-2474 1475-3057 journal-article 1989 crcambridgeupr https://doi.org/10.1017/s0032247400010809 2024-07-31T04:04:47Z Abstract Large tabular icebergs derived from the glaciers which drain the north fringe of Greenland's Inland Iceoccur in many North Greenland fjords. Many have undulating surface topography resembling that of the ice islands calved from Ellesmere Island ice shelves. Semi-permanent sea ice in North Greenland fjords often prevents the escape of bergs, except in exceptional summers several decades apart, when the fjord ice melts completely and some bergs may reach the Arctic Ocean. Other possible sources for ice islands are small ice shelves and local glaciers along the north coast of Greenland. Article in Journal/Newspaper Arctic Ocean Ellesmere Island Greenland Ice Shelves Iceberg* North Greenland Polar Record Sea ice Cambridge University Press Polar Record 25 154 207 212 |
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Open Polar |
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Cambridge University Press |
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crcambridgeupr |
language |
English |
description |
Abstract Large tabular icebergs derived from the glaciers which drain the north fringe of Greenland's Inland Iceoccur in many North Greenland fjords. Many have undulating surface topography resembling that of the ice islands calved from Ellesmere Island ice shelves. Semi-permanent sea ice in North Greenland fjords often prevents the escape of bergs, except in exceptional summers several decades apart, when the fjord ice melts completely and some bergs may reach the Arctic Ocean. Other possible sources for ice islands are small ice shelves and local glaciers along the north coast of Greenland. |
format |
Article in Journal/Newspaper |
author |
Higgins, A. K. |
spellingShingle |
Higgins, A. K. North Greenland ice islands |
author_facet |
Higgins, A. K. |
author_sort |
Higgins, A. K. |
title |
North Greenland ice islands |
title_short |
North Greenland ice islands |
title_full |
North Greenland ice islands |
title_fullStr |
North Greenland ice islands |
title_full_unstemmed |
North Greenland ice islands |
title_sort |
north greenland ice islands |
publisher |
Cambridge University Press (CUP) |
publishDate |
1989 |
url |
http://dx.doi.org/10.1017/s0032247400010809 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0032247400010809 |
genre |
Arctic Ocean Ellesmere Island Greenland Ice Shelves Iceberg* North Greenland Polar Record Sea ice |
genre_facet |
Arctic Ocean Ellesmere Island Greenland Ice Shelves Iceberg* North Greenland Polar Record Sea ice |
op_source |
Polar Record volume 25, issue 154, page 207-212 ISSN 0032-2474 1475-3057 |
op_rights |
https://www.cambridge.org/core/terms |
op_doi |
https://doi.org/10.1017/s0032247400010809 |
container_title |
Polar Record |
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25 |
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154 |
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207 |
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212 |
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1810295578303660032 |