全新世长江中下游地区降水变化及其驱动机制

徐家豪; 张志平; 陈钧伟; 孙炜毅; 申忠伟; 贾鑫

doi:10.3799/dqkx.2023.214

Volume 50 Issue 2

Feb. 2025

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Article Navigation > Earth Science > 2025 > 50(2): 699-717

Xu Jiahao, Zhang Zhiping, Chen Junwei, Sun Weiyi, Shen Zhongwei, Jia Xin, 2025. Holocene Precipitation Change in the Middle and Lower Reaches of the Yangtze River and Its Forcing Mechanisms. Earth Science, 50(2): 699-717. doi: 10.3799/dqkx.2023.214

Citation:

Xu Jiahao, Zhang Zhiping, Chen Junwei, Sun Weiyi, Shen Zhongwei, Jia Xin, 2025. Holocene Precipitation Change in the Middle and Lower Reaches of the Yangtze River and Its Forcing Mechanisms. Earth Science, 50(2): 699-717. doi: 10.3799/dqkx.2023.214

Citation:

Xu Jiahao, Zhang Zhiping, Chen Junwei, Sun Weiyi, Shen Zhongwei, Jia Xin, 2025. Holocene Precipitation Change in the Middle and Lower Reaches of the Yangtze River and Its Forcing Mechanisms. Earth Science, 50(2): 699-717. doi: 10.3799/dqkx.2023.214

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Holocene Precipitation Change in the Middle and Lower Reaches of the Yangtze River and Its Forcing Mechanisms

doi: 10.3799/dqkx.2023.214

Xu Jiahao^{1, 2
,
,},
Zhang Zhiping^{1, 2
,
,
,},
Chen Junwei^{1, 2},
Sun Weiyi^{1, 3},
Shen Zhongwei⁴,
Jia Xin^{1, 2}

1.
School of Geography, Nanjing Normal University, Nanjing 210023, China
2.
Institute of Environmental Archaeology, Nanjing Normal University, Nanjing 210023, China
3.
Key Laboratory of Virtual Geographic Environment(Ministry of Education), Nanjing Normal University, Nanjing 210023, China
4.
School of Geographical Sciences, Hunan Normal University, Changsha 410081, China

Received Date: 2023-11-25
Available Online: 2025-02-26
Publish Date: 2025-02-25

Abstract

Abstract

In order to reconcile the contradictions among the Holocene precipitation records retrieved from different nature archives in the middle and lower reaches of the Yangtze River (MLRYR), this study analyzed 12 Holocene precipitation records in the middle reaches of the Yangtze River and 18 Holocene precipitation records in the lower reaches of the Yangtze River. The results show that the precipitation in the MLRYR has gradually increased since the onset of the Holocene, and then decreased after the middle Holocene. During the late Holocene, the precipitation evolution pattern in the MLRYR was decoupled: the precipitation in the middle reaches of the Yangtze River increased again, while the precipitation in the lower reaches of the Yangtze River tended to decrease with fluctuations. In terms of mechanisms, the Holocene precipitation evolution in the MLRYR was generally controlled by the Northern Hemisphere summer insolation (NHSI). During the late Holocene, the ENSO activity increased significantly, and the position of the Asian westerly jet was shifted to the south, superimposed on the anomalies of the Indian summer monsoon circulation, which not only led to the deviation of the precipitation pattern in the MLRYR from the variation trend of NHSI, but also resulted in the formation of a more wet climate in the middle reaches of the Yangtze River relative to the lower reaches of the Yangtze River.
- Holocene,
- Middle and lower reaches of the Yangtze River,
- East Asian summer monsoon,
- precipitation changes,
- forcing mechanisms,
- geomorphology

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References(131)

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Holocene Precipitation Change in the Middle and Lower Reaches of the Yangtze River and Its Forcing Mechanisms

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