Effects of Tibetan Plateau Growth, Paratethys Sea Retreat and Global Cooling on the East Asian Climate by the Early Miocene
Effects of Tibetan Plateau Growth, Paratethys Sea Retreat and Global Cooling on the East Asian Climate by the Early Miocene
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中新世早期青藏高原生长、副特提斯海退缩和全球变冷对东亚气候的影响
DOI：
10.1029/2021gc009655
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发表时间：
2021-05
影响因子：
3.5
通讯作者：
Zhang Chunxia
中科院分区：
文献类型：
--
作者：
Zhang Ran;Jiang Dabang;Zhang Zhongshi;Zhang Chunxia
古植物学和沉积学记录表明，到中新世早期，中国东部已经发生了明显的气候和环境转变。这些转变是由古地理和全球气候变化驱动的，但这些变化在亚洲气候中各自的作用仍不清楚。在这里，我们使用低分辨率的挪威地球系统模型和社区大气模型版本4来比较青藏高原（TP）增长、副特提斯海退缩和全球变冷对中新世早期发生的东亚气候变化的影响。模拟结果表明，这三个因素对华东地区的气候影响明显不同。其中，TP增长增加了华东地区的年降水量，而副甲提斯海退缩和全球变冷则普遍减少了华东地区的年降水量。此外，研究的三个因素均导致了亚洲内陆的干旱化。考虑到地质记录显示，中新世早期中国东部地区降水量增加、植被从干旱/半干旱向湿润转变以及植物多样性较高，因此TP的生长在这些方面发挥了重要作用。
Paleobotanical and sedimentological records indicate that marked climatic and environmental transitions had taken place in East China by the early Miocene. These transitions were driven by paleogeographic and global climatic shifts, but the respective roles of these shifts in the Asian climate remain unclear. Here, we use the low‐resolution Norwegian Earth System Model and Community Atmosphere Model version 4 to compare the effects of Tibetan Plateau (TP) growth, Paratethys Sea retreat and global cooling on the East Asian climate change that occurred by the early Miocene. The modeling results indicate that these three factors had clearly different climatic effects in East China. In particular, TP growth increased annual precipitation in East China, while Paratethys Sea retreat and global cooling generally decreased annual precipitation in East China. In addition, the three factors studied all drove aridification in inland Asia. Considering the increased precipitation, arid/semiarid‐to‐humid shift in vegetation and high plant diversity present in East China by the early Miocene, as shown in geological records, TP growth thus played a major role in these respects.
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DOI：
10.1002/2015jd024370
发表时间：
2016-05
期刊：
Journal of Geophysical Research: Atmospheres
影响因子：
--
作者：
G. Roe;Q. Ding;D. Battisti;P. Molnar;M. Clark;C. Garzione
通讯作者：
G. Roe;Q. Ding;D. Battisti;P. Molnar;M. Clark;C. Garzione
晚渐新世-中新世中纬度干旱化和亚洲内陆风型
影响因子：
5.8
作者：
Sun, Jimin;Ye, Jie;Meng, Jin
通讯作者：
Meng, Jin
影响因子：
5.3
作者：
D. Zoura;D. J. Hill;A. Dolan;S. Hunter;Z. Tang;A. Haywood
通讯作者：
D. Zoura;D. J. Hill;A. Dolan;S. Hunter;Z. Tang;A. Haywood
气温波动和东亚季风推动了中国南方喀斯特生态系统的植物多样化
影响因子：
4.9
作者：
Kong, Hanghui;Condamine, Fabien L.;Kang, Ming
通讯作者：
Kang, Ming
影响因子：
5.3
作者：
Ran Zhang;D. Jiang;G. Ramstein;Zhongshi Zhang;P. Lippert;Entao Yu
通讯作者：
Ran Zhang;D. Jiang;G. Ramstein;Zhongshi Zhang;P. Lippert;Entao Yu