Presentation Details
Multi-centennial climate oscillation caused by AMOC leads to the vicissitude of Tubo dynasty
ID：1152
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Updated Time：2025-01-05 10:30:41
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Poster Presentation
Start Time：2025-01-15 19:05（Asia/Shanghai）
Duration：15min
Session：S41 Session 41-The Atlantic Meridional Overturning Circulation Variability and Its Climatic Impacts »
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Abstract
The Tubo Dynasty (~600-900 AD) was the first regime in the history of the Tibetan Plateau with clear historical records. Previous studies have shown that the rise and fall of the Tubo Dynasty are closely related to the local climate cycle on multi-centennial time scale. In the transient experiment of EC-Earth 3 numerical model, we find that the change of the strength of thermohaline circulation (AMOC) may be the root cause of the multi-centennial oscillation of Tibetan Plateau climate. This research can greatly improve our understanding of how climate affects the evolution of human civilization and provide references for similar studies.
Keywords
AMOC, civilization, Tibetan Plateau
Speaker
Fengli An
Doctoral Student Fudan UniversitySubmission Author
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Important Date
-
Conference Date
Jan 13
2025
toJan 17
2025
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Sep 27 2024
Draft paper submission deadline
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Feb 17 2025
Registration deadline
Sponsored By
State Key Laboratory of Marine Environmental Science, Xiamen University
Organized By
State Key Laboratory of Marine Environmental Science, Xiamen University
Department of Earth Sciences, National Natural Science Foundation of China
Department of Earth Sciences, National Natural Science Foundation of China
Contact Information
- Kejing GU
- xm******@xmu.edu.cn
- +86*********
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