气候变化领域集成服务门户(CCPortal): Central Asian river streamflows have not continued to increase during the recent warming hiatus

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DOI	10.1016/j.atmosres.2020.105124
	Central Asian river streamflows have not continued to increase during the recent warming hiatus
	Chen F.; Chen Y.; Bakhtiyorov Z.; Zhang H.; Man W.; Chen F.
发表日期	2020
ISSN	0169-8095
卷号	246
英文摘要	The recent warming hiatus started around 1998; however, how Central Asian river streamflows have responded to this warming slowdown remains unclear. Based on the instrumental streamflow records of eight rivers in Central Asian, we showed that the Central Asian streamflow variation is due to the change in precipitation/drought resulting from sea surface temperature changes in the eastern tropical Pacific Ocean and that equatorial eastern Pacific surface cooling has been the main driver of the slowdown in streamflow increase in Central Asia over the past two decades. Temperature is also likely an important driver of streamflow variation on the Pamirs Plateau during the warm season; however, the linkage between temperature and streamflow is not stable due in part to the precipitation-induced cooling. Central Asian river streamflow is very sensitive to variations in climate factors, and the influences of climate change on streamflow should be considered continuously by water resource managers. © 2020 Elsevier B.V.
英文关键词	Central Asia; ENSO; Streamflow variation; Warming hiatus
语种	英语
scopus关键词	Climate change; Oceanography; Rivers; Submarine geophysics; Climate factors; Eastern pacific; Eastern tropical pacific; Resource managers; Sea-surface temperature change; Streamflow records; Streamflow variations; Surface cooling; Stream flow; cooling; drought; global warming; precipitation (climatology); river flow; sea surface temperature; streamflow; Central Asia; Pacific Ocean; Pacific Ocean (East); Pacific Ocean (Tropical)
来源期刊	Atmospheric Research
文献类型	期刊论文
条目标识符	http://gcip.llas.ac.cn/handle/2XKMVOVA/141793
作者单位	Yunnan Key Laboratory of International Rivers and Transboundary Eco-Security, Institute of International Rivers and Eco-Security, Yunnan University, Kunming, 650504, China; Key Laboratory of Tree-ring Physical and Chemical Research, Institute of Desert Meteorology, China Meteorological Administration, Urumqi, 830002, China; Khujand Science Center Academy of Sciences of the Republic of Tajikistan, Khujand, 735700, Tajikistan; LASG, Institute of Atmospheric Physics, Chinese Academy of Sciences (CAS), Beijing, 100029, China; Key Laboratory of Alpine Ecology, CAS Center for Excellence in Tibetan Plateau Earth Sciences and Institute of Tibetan Plateau Research, Chinese Academy of Sciences (CAS), Beijing, 100101, China; Key Laboratory of Western China's Environmental Systems (Ministry of Education), College of Earth and Environmental Sciences, Lanzhou University, Lanzhou, 730000, China
推荐引用方式 GB/T 7714	Chen F.,Chen Y.,Bakhtiyorov Z.,et al. Central Asian river streamflows have not continued to increase during the recent warming hiatus[J],2020,246.
APA	Chen F.,Chen Y.,Bakhtiyorov Z.,Zhang H.,Man W.,&Chen F..(2020).Central Asian river streamflows have not continued to increase during the recent warming hiatus.Atmospheric Research,246.
MLA	Chen F.,et al."Central Asian river streamflows have not continued to increase during the recent warming hiatus".Atmospheric Research 246(2020).