The end of the ice age
Methane-gas hydrates may have contributed to the rapid rise in atmospheric CH 4 , CO 2 , and global temperatures at the end of the last major glaciation about 13 500 years ago. Given suitable orbital conditions and insolation at high latitude, a small triggering event, such as the release of one or...
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1990
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Online Access: | http://dx.doi.org/10.1139/e90-012 http://www.nrcresearchpress.com/doi/pdf/10.1139/e90-012 |
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crcansciencepubl:10.1139/e90-012 2024-04-28T08:09:36+00:00 The end of the ice age Nisbet, E. G. 1990 http://dx.doi.org/10.1139/e90-012 http://www.nrcresearchpress.com/doi/pdf/10.1139/e90-012 en eng Canadian Science Publishing http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining Canadian Journal of Earth Sciences volume 27, issue 1, page 148-157 ISSN 0008-4077 1480-3313 General Earth and Planetary Sciences journal-article 1990 crcansciencepubl https://doi.org/10.1139/e90-012 2024-04-02T06:55:52Z Methane-gas hydrates may have contributed to the rapid rise in atmospheric CH 4 , CO 2 , and global temperatures at the end of the last major glaciation about 13 500 years ago. Given suitable orbital conditions and insolation at high latitude, a small triggering event, such as the release of one or more Arctic gas pools, may have initiated massive release of methane from hydrate under ice and in permafrost. The consequent greenhouse warming would have provided strong positive feedback, amplifying emission. This warming, driven by CH 4 , may have induced the release of CO 2 from the oceans to the biosphere, stabilizing the interglacial carbon cycle. Article in Journal/Newspaper Arctic Ice permafrost Canadian Science Publishing Canadian Journal of Earth Sciences 27 1 148 157 |
institution |
Open Polar |
collection |
Canadian Science Publishing |
op_collection_id |
crcansciencepubl |
language |
English |
topic |
General Earth and Planetary Sciences |
spellingShingle |
General Earth and Planetary Sciences Nisbet, E. G. The end of the ice age |
topic_facet |
General Earth and Planetary Sciences |
description |
Methane-gas hydrates may have contributed to the rapid rise in atmospheric CH 4 , CO 2 , and global temperatures at the end of the last major glaciation about 13 500 years ago. Given suitable orbital conditions and insolation at high latitude, a small triggering event, such as the release of one or more Arctic gas pools, may have initiated massive release of methane from hydrate under ice and in permafrost. The consequent greenhouse warming would have provided strong positive feedback, amplifying emission. This warming, driven by CH 4 , may have induced the release of CO 2 from the oceans to the biosphere, stabilizing the interglacial carbon cycle. |
format |
Article in Journal/Newspaper |
author |
Nisbet, E. G. |
author_facet |
Nisbet, E. G. |
author_sort |
Nisbet, E. G. |
title |
The end of the ice age |
title_short |
The end of the ice age |
title_full |
The end of the ice age |
title_fullStr |
The end of the ice age |
title_full_unstemmed |
The end of the ice age |
title_sort |
end of the ice age |
publisher |
Canadian Science Publishing |
publishDate |
1990 |
url |
http://dx.doi.org/10.1139/e90-012 http://www.nrcresearchpress.com/doi/pdf/10.1139/e90-012 |
genre |
Arctic Ice permafrost |
genre_facet |
Arctic Ice permafrost |
op_source |
Canadian Journal of Earth Sciences volume 27, issue 1, page 148-157 ISSN 0008-4077 1480-3313 |
op_rights |
http://www.nrcresearchpress.com/page/about/CorporateTextAndDataMining |
op_doi |
https://doi.org/10.1139/e90-012 |
container_title |
Canadian Journal of Earth Sciences |
container_volume |
27 |
container_issue |
1 |
container_start_page |
148 |
op_container_end_page |
157 |
_version_ |
1797577894110691328 |