Warming slowdown over the Tibetan plateau in recent decades

doi:10.1007/s00704-018-2435-3

	Warming slowdown over the Tibetan plateau in recent decades
	Liu, Yaojie 1,2; Zhang, Yangjian 1,2,3; Zhu, Juntao 1; Huang, Ke 1,2; Zu, Jiaxing 1,2; Chen, Ning 1,2; Cong, Nan 1; Stegehuis, Annemiek Irene 4
刊名	THEORETICAL AND APPLIED CLIMATOLOGY
	2019-02-01
卷号	135 期号:3-4 页码:1375-1385
关键词	Tibetan plateau Warming hiatus Land surface temperature MODIS Mann-Kendall
ISSN号	0177-798X
DOI	10.1007/s00704-018-2435-3
通讯作者	Zhang, Yangjian(zhangyj@igsnrr.ac.cn)
英文摘要	As the recent global warming hiatus and the warming on high elevations are attracting worldwide attention, this study examined the robustness of the warming slowdown over the Tibetan plateau (TP) and its related driving forces. By integrating multiple-source data from 1982 to 2015 and using trend analysis, we found that the mean temperature (T-mean), maximum temperature (T-max) and minimum temperature (T-min) showed a slowdown of the warming trend around 1998, during the period of the global warming hiatus. This was found over both the growing season (GS) and non-growing season (NGS) and suggested a robust warming hiatus over the TP. Due to the differences in trends of T-max and T-min, the trend of diurnal temperature range (DTR) also shifted after 1998, especially during the GS temperature. The warming rate was spatially heterogeneous. The northern TP (NTP) experienced more warming than the southern TP (STP) in all seasons from 1982 to 1998, while the pattern was reversed in the period from 1998 to 2015. Water vapour was found to be the main driving force for the trend in T-mean and T-min by influencing downward long wave radiation. Sunshine duration was the main driving force behind the trend in T-max and DTR through a change in downward shortwave radiation that altered the energy source of daytime temperature. Water vapour was the major driving force for temperature change over the NTP, while over the STP, sunshine duration dominated the temperature trend.
资助项目	Chinese National Key Program for Developing Basic Science[2013CB956302] ; Science and Technology Project of the Chinese Academy of Sciences[XDA05050400]
WOS关键词	ALTITUDINAL DEPENDENCE ; SURFACE-TEMPERATURE ; CLIMATE ; VARIABILITY ; IMPACTS
WOS研究方向	Meteorology & Atmospheric Sciences
语种	英语
出版者	SPRINGER WIEN
WOS记录号	WOS:000464905800038
资助机构	Chinese National Key Program for Developing Basic Science ; Science and Technology Project of the Chinese Academy of Sciences
内容类型	期刊论文
源URL	[http://ir.igsnrr.ac.cn/handle/311030/48036]
专题	中国科学院地理科学与资源研究所
通讯作者	Zhang, Yangjian
作者单位	1.Chinese Acad Sci, Inst Geog Sci & Nat Resources Res, Key Lab Ecosyst Network Observat & Modeling, Lhasa Plateau Ecosyst Res Stn, Beijing 100101, Peoples R China 2.Univ Chinese Acad Sci, Coll Resources & Environm, Beijing 100190, Peoples R China 3.Chinese Acad Sci, Ctr Excellence Tibetan Plateau Earth Sci, Beijing 100101, Peoples R China 4.Peking Univ, Sch Urban Planning & Design, Shenzhen Grad Sch, Shenzhen Key Lab Circular Econ, Shenzhen 518055, Peoples R China
推荐引用方式 GB/T 7714	Liu, Yaojie,Zhang, Yangjian,Zhu, Juntao,et al. Warming slowdown over the Tibetan plateau in recent decades[J]. THEORETICAL AND APPLIED CLIMATOLOGY,2019,135(3-4):1375-1385.
APA	Liu, Yaojie.,Zhang, Yangjian.,Zhu, Juntao.,Huang, Ke.,Zu, Jiaxing.,...&Stegehuis, Annemiek Irene.(2019).Warming slowdown over the Tibetan plateau in recent decades.THEORETICAL AND APPLIED CLIMATOLOGY,135(3-4),1375-1385.
MLA	Liu, Yaojie,et al."Warming slowdown over the Tibetan plateau in recent decades".THEORETICAL AND APPLIED CLIMATOLOGY 135.3-4(2019):1375-1385.