Does δ 18 O of O 2 record meridional shifts in tropical rainfall?
Marine sediments, speleothems, paleo-lake elevations, and ice core methane and δ 18 O of O 2 ( δ 18 O atm ) records provide ample evidence for repeated abrupt meridional shifts in tropical rainfall belts throughout the last glacial cycle. To improve understanding of the impact of abrupt events on th...
Published in: | Climate of the Past |
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Main Authors: | , , , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Copernicus Publications
2017
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Subjects: | |
Online Access: | https://doi.org/10.5194/cp-13-1323-2017 https://doaj.org/article/0fc8364e88cf45339195d1a55cff4ba3 |