Articles | Volume 20, issue 7
https://doi.org/10.5194/cp-20-1615-2024
https://doi.org/10.5194/cp-20-1615-2024
Research article
 | 
25 Jul 2024
Research article |  | 25 Jul 2024

Response of coastal California hydroclimate to the Paleocene–Eocene Thermal Maximum

Xiaodong Zhang, Brett J. Tipple, Jiang Zhu, William D. Rush, Christian A. Shields, Joseph B. Novak, and James C. Zachos

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Latest update: 25 Dec 2024
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Short summary
This study is motivated by the current anthropogenic-warming-forced transition in regional hydroclimate. We use observations and model simulations during the Paleocene–Eocene Thermal Maximum (PETM) to constrain the regional/local hydroclimate response. Our findings, based on multiple observational evidence within the context of model output, suggest a transition toward greater aridity and precipitation extremes in central California during the PETM.