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...

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Bibliographic Details
Published in:Climate of the Past
Main Authors: A. M. Seltzer, C. Buizert, D. Baggenstos, E. J. Brook, J. Ahn, J.-W. Yang, J. P. Severinghaus
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2017
Subjects:
Online Access:https://doi.org/10.5194/cp-13-1323-2017
https://doaj.org/article/0fc8364e88cf45339195d1a55cff4ba3