Precipitation pattern of the mid-Holocene simulated by a high-resolution regional climate model
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- 作者：Entao Yu (1) (2)
Tao Wang (1) (2)
Yongqi Gao (1) (3)
Weiling Xiang (4) - 关键词：mid ; Holocene ; East China ; southern drought/northern flood
- 刊名：Advances in Atmospheric Sciences
- 出版年：2014
- 出版时间：July 2014
- 年：2014
- 卷：31
- 期：4
- 页码：962-971
- 全文大小：
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Tao Wang (1) (2)
Yongqi Gao (1) (3)
Weiling Xiang (4)
1. Nansen-Zhu International Research Centre, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing, 100029, China
2. Climate Change Research Center, Chinese Academy of Sciences, Beijing, 100029, China
3. Nansen Environmental and Remote Sensing Center, Bergen, Norway, 5006, China
4. State Key Laboratory of Atmospheric Boundary Layer Physics and Atmospheric Chemistry, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing, 100029, China - ISSN：1861-9533
文摘
Early proxy-based studies suggested that there potentially occurred a “southern drought/northern flood-(SDNF) over East China in the mid-Holocene (from roughly 7000 to 5000 years before present). In this study, we used both global and regional atmospheric circulation models to demonstrate that the SDNF—namely, the precipitation increases over North China and decreases over the the lower reaches of the Yangtze River Valley—could have taken place in the mid-Holocene. We found that the SDNF in the mid-Holocene was likely caused by the lower SST in the Pacific. The lowered SST and the higher air temperature over mainland China increased the land-sea thermal contrast and, as a result, strengthened the East Asian summer monsoon and enhanced the precipitation over North China.