Severe Drought Conditions in Northern East Asia During the Early Pliocene Caused by Weakened Pacific Meridional Temperature Gradient
Severe Drought Conditions in Northern East Asia During the Early Pliocene Caused by Weakened Pacific Meridional Temperature Gradient
复制标题
太平洋经向温度梯度减弱导致上新世早期东亚北部严重干旱
DOI:
10.1029/2022gl098813
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发表时间:
2022-07
期刊:
影响因子:
--
通讯作者:
Hongxuan Lu
中科院分区:
文献类型:
--
作者:
Yanhong Zheng;Alexey V. Fedorov;Natalie J. Burls;Rui Zhang;Chris Brierley;Zhengkun Fang;Xuefeng Yu;Feng Xian;Hongxuan Lu
The evolution of hydroclimate in East Asia during the Pliocene—a potential analog of the future greenhouse climate—remains highly uncertain. Here we reconstruct changes in the hydroclimate of Northern China during this epoch. Our results reveal previously undocumented severe drought conditions that persisted through the early Pliocene with a significantly greater magnitude than suggested by other records. Using a broad hierarchy of climate simulations, we find that reduction in the Pacific meridional sea surface temperature (SST) gradient has particularly strong impacts on precipitation over Northern China, which suggests its key role in maintaining drought conditions during the early Pliocene. The weaker Pacific meridional SST gradient causes the weakening of the East Asian summer monsoon precipitation over this region via a reduction of atmospheric northward moisture transport from the ocean, which enhances aridity inland. Our results highlight the fundamental control of the tropical ocean on the extra-tropical hydrological cycle.
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影响因子:
5.3
作者:
Jiayi Lu;Huan Yang;M. Griffiths;N. Burls;G. Xiao;Jilong Yang;J. K. Wang;K. Johnson;S. Xie
通讯作者:
Jiayi Lu;Huan Yang;M. Griffiths;N. Burls;G. Xiao;Jilong Yang;J. K. Wang;K. Johnson;S. Xie
影响因子:
13.6
作者:
Tierney JE;Pausata FS;deMenocal PB
通讯作者:
deMenocal PB
影响因子:
4.9
作者:
Burls, N. J.;Fedorov, A. V.
通讯作者:
Fedorov, A. V.
影响因子:
64.8
作者:
Fedorov, A. V.;Brierley, C. M.;Ravelo, A. C.
通讯作者:
Ravelo, A. C.
影响因子:
56.9
作者:
M. Wara;A. Ravelo;M. Delaney
通讯作者:
M. Wara;A. Ravelo;M. Delaney