Does δ18O of O2 record meridional shifts in tropical rainfall?

Marine sediments, speleothems, paleo-lake elevations, and ice core methane and δ18O of O2 (δ18Oatm) 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 the global...

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Bibliographic Details
Published in:Climate of the Past
Main Authors: Seltzer, Alan M., Buizert, Christo, Baggenstos, Daniel, Brook, Edward J., Ahn, Jinho, Yang, Ji-Woong, Severinghaus, Jeffrey P.
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2017
Subjects:
Online Access:https://doi.org/10.5194/cp-13-1323-2017
https://noa.gwlb.de/receive/cop_mods_00008424
https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00008381/cp-13-1323-2017.pdf
https://cp.copernicus.org/articles/13/1323/2017/cp-13-1323-2017.pdf