Decoupled Hydroclimate of Central and Southwestern Iran Controlled by the Strength of Southerly‐Westerly Jets During Marine Isotope Stage 3

Decoupled Hydroclimate of Central and Southwestern Iran Controlled by the Strength of Southerly‐Westerly Jets During Marine Isotope Stage 3

Abstract The regional impact of abrupt glacial climate variability remains poorly constrained for arid southwestern Asia, particularly winter dynamics during Marine Isotope Stage 3, due to limited paleoarchives in the Middle East. Here, we present continuous speleothem records of δ18O and δ13C with...

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Bibliographic Details
Main Authors: M. Soleimani, J. L. Baker, A. Nadimi, Y. Dublyansky, G. Koltai, C. Spötl
Format: Article
Language:English
Published: Wiley 2024-07-01
Series:Geophysical Research Letters
Subjects:
paleoclimate
speleothem
Iran
Marine Isotope Stage 3
Heinrich event 4
westerlies
Online Access:https://doi.org/10.1029/2024GL109797
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https://doi.org/10.1029/2024GL109797

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