Is the noble gas‐based rate of ocean warming during the Younger Dryas overestimated?
Noble gases in ice cores enable reconstructions of past mean ocean temperature. A recent result from the clathrate‐containing WAIS Divide Ice Core showed tight covariation between ocean and Antarctic temperatures throughout the last deglaciation, except for the Younger Dryas interval. In the beginni...
Published in: | Geophysical Research Letters |
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Main Authors: | , , , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
American Geophysical Union
2019
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Subjects: | |
Online Access: | https://nrl.northumbria.ac.uk/id/eprint/39343/ https://doi.org/10.1029/2019GL082971 https://nrl.northumbria.ac.uk/id/eprint/39343/16/Shackleton_et_al-2019-Geophysical_Research_Letters.pdf https://nrl.northumbria.ac.uk/id/eprint/39343/8/Shackleton_et_al-2019-Geophysical_Research_Letters.pdf https://nrl.northumbria.ac.uk/id/eprint/39343/1/Shackleton%20et%20al%20-%20Is%20the%20noble%20gas-based%20rate%20of%20ocean%20warming%20during%20the%20Younger%20Dryas%20overestimated%20AAM.pdf |