Global ocean cooling of 2.3°C during the Last Glacial Maximum
Quantitative constraints on past mean ocean temperature (MOT) critically inform our historical understanding of Earth's energy balance. A recently developed MOT proxy based on paleoatmospheric Xe, Kr, and N2 ratios in ice core air bubbles is a promising tool rooted in the temperature dependence...
| Main Authors: | , , , , |
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| Format: | Journal article |
| Language: | English |
| Published: |
American Geophysical Union
2024
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