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: | , , , , |
---|---|
格式: | Journal article |
语言: | English |
出版: |
American Geophysical Union
2024
|