Water stable isotope record of ice core WAIS divide
Changes in atmospheric circulation over the past five decades have enhanced the wind-driven inflow of warm ocean water onto the Antarctic continental shelf, where it melts ice shelves from below. Atmospheric circulation changes have also caused rapid warming over the West Antarctic Ice Sheet, and co...
Main Authors: | , , , , , , , , , , , , , , , , , , , , , , |
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Format: | Dataset |
Language: | English |
Published: |
PANGAEA
2018
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Subjects: | |
Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.886046 https://doi.org/10.1594/PANGAEA.886046 |