Floating Glacial Ice Caps in the Arctic Ocean
Two arguments are presented, one in favor of the existence of thicker ice in the Arctic Ocean during glacial time, and the other in favor of a full-fledged Arctic ice cap. The first is based on the Greenland air temperature record obtained from isotopic studies of the Camp Century ice core. The seco...
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American Association for the Advancement of Science (AAAS)
1975
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Online Access: | http://dx.doi.org/10.1126/science.188.4193.1116 https://www.science.org/doi/pdf/10.1126/science.188.4193.1116 |
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craaas:10.1126/science.188.4193.1116 2024-06-09T07:42:55+00:00 Floating Glacial Ice Caps in the Arctic Ocean Broecker, Wallace S. 1975 http://dx.doi.org/10.1126/science.188.4193.1116 https://www.science.org/doi/pdf/10.1126/science.188.4193.1116 en eng American Association for the Advancement of Science (AAAS) Science volume 188, issue 4193, page 1116-1118 ISSN 0036-8075 1095-9203 journal-article 1975 craaas https://doi.org/10.1126/science.188.4193.1116 2024-05-16T12:54:46Z Two arguments are presented, one in favor of the existence of thicker ice in the Arctic Ocean during glacial time, and the other in favor of a full-fledged Arctic ice cap. The first is based on the Greenland air temperature record obtained from isotopic studies of the Camp Century ice core. The second is based on the oxygen isotope record of benthic foraminifera from a deep Pacific Ocean core. Article in Journal/Newspaper Arctic Arctic Ocean Foraminifera* Greenland Ice cap ice core AAAS Resource Center (American Association for the Advancement of Science) Arctic Arctic Ocean Greenland Pacific Science 188 4193 1116 1118 |
institution |
Open Polar |
collection |
AAAS Resource Center (American Association for the Advancement of Science) |
op_collection_id |
craaas |
language |
English |
description |
Two arguments are presented, one in favor of the existence of thicker ice in the Arctic Ocean during glacial time, and the other in favor of a full-fledged Arctic ice cap. The first is based on the Greenland air temperature record obtained from isotopic studies of the Camp Century ice core. The second is based on the oxygen isotope record of benthic foraminifera from a deep Pacific Ocean core. |
format |
Article in Journal/Newspaper |
author |
Broecker, Wallace S. |
spellingShingle |
Broecker, Wallace S. Floating Glacial Ice Caps in the Arctic Ocean |
author_facet |
Broecker, Wallace S. |
author_sort |
Broecker, Wallace S. |
title |
Floating Glacial Ice Caps in the Arctic Ocean |
title_short |
Floating Glacial Ice Caps in the Arctic Ocean |
title_full |
Floating Glacial Ice Caps in the Arctic Ocean |
title_fullStr |
Floating Glacial Ice Caps in the Arctic Ocean |
title_full_unstemmed |
Floating Glacial Ice Caps in the Arctic Ocean |
title_sort |
floating glacial ice caps in the arctic ocean |
publisher |
American Association for the Advancement of Science (AAAS) |
publishDate |
1975 |
url |
http://dx.doi.org/10.1126/science.188.4193.1116 https://www.science.org/doi/pdf/10.1126/science.188.4193.1116 |
geographic |
Arctic Arctic Ocean Greenland Pacific |
geographic_facet |
Arctic Arctic Ocean Greenland Pacific |
genre |
Arctic Arctic Ocean Foraminifera* Greenland Ice cap ice core |
genre_facet |
Arctic Arctic Ocean Foraminifera* Greenland Ice cap ice core |
op_source |
Science volume 188, issue 4193, page 1116-1118 ISSN 0036-8075 1095-9203 |
op_doi |
https://doi.org/10.1126/science.188.4193.1116 |
container_title |
Science |
container_volume |
188 |
container_issue |
4193 |
container_start_page |
1116 |
op_container_end_page |
1118 |
_version_ |
1801371623493730304 |