Stable isotopes and chloride ion of precipitation events in the northeastern Tibetan Plateau, China

doi:10.1007/s11629-020-6574-5

IEECAS OpenIR > 黄土与第四纪地质国家重点实验室（2010~）

	Stable isotopes and chloride ion of precipitation events in the northeastern Tibetan Plateau, China
	Cui Bu-li 1,2,3; Li Dong-sheng 2; Jiang Bao-fu 2; Wang Ying 2; Wang Ya-xuan 2; Wang Long-sheng 2; Li Xiao-yan 1
通讯作者	Cui Bu-li(cuibuli@163.com)
	2021-04-01
发表期刊	JOURNAL OF MOUNTAIN SCIENCE
ISSN	1672-6316
卷号	18 期号:4 页码:834-846
摘要	Stable isotopes and chloride ion of precipitation are ideal environmental tracers to explain and reveal the formation and evolution mechanisms of water bodies. It is crucial to investigate the stable isotopes and chloride in precipitation events in the northeastern part of the Tibetan Plateau (NETP) due to the limitation of available data. This study sampled each event of precipitation during the period from July 2018 to June 2019 and the monthly dustfall in the NETP to investigate the temporal changes of stable isotopes and chloride in precipitation, and to reveal the moisture source of precipitation over the NETP using a back trajectory model. Results showed that the delta H-2 values of precipitation ranged from -183.51 parts per thousand to 17.75 parts per thousand, and the delta O-18 values ranged from -25.18 parts per thousand to 0.48 parts per thousand. The slope of the Local Meteoric Water Line was slightly lower than 8 due to the effect of below-cloud secondary evaporation on the precipitation process. Most d-excess values were higher than 10 parts per thousand because moisture recycled from the continent and Qinghai Lake surface mixed with precipitation. The chloride in precipitation accounted for 86.5% of the annual total deposition mass of chloride (1329.64 mg/m(2)), indicating that precipitation was the main source of chloride in the NETP. The temperature and amount effects of stable isotope in the precipitation were obvious in the NETP. The precipitation was predominantly derived from the Westerly Circulation from September through May and the East Asian Monsoon from June to August, with precipitation amounts of 246.5 mm and 178.0 mm, respectively, indicating that the precipitation over the NETP brought by the Westerly Circulation was more than that brought by the East Asian Monsoon. The air mass over the NETP transited in late May and early September, and a slight change in transition period would mainly be related to the intensity of the East Asian Monsoon, which is strongly influenced by El Nino-Southern Oscillation. These results provide not only baseline data for hydrological and climatological studies of the NETP but also valuable insights into the hydrological process in the inland arid area of Asia.
关键词	Stable isotope Chloride ion Precipitation Moisture source Northeastern Tibetan Plateau
DOI	10.1007/s11629-020-6574-5
收录类别	SCI ; SCI
语种	英语
WOS研究方向	Environmental Sciences & Ecology
WOS类目	Environmental Sciences
WOS记录号	WOS:000639495600002
出版者	SCIENCE PRESS
引用统计	被引频次：3[WOS] [WOS记录] [WOS相关记录]
文献类型	期刊论文
条目标识符	http://ir.ieecas.cn/handle/361006/16346
专题	黄土与第四纪地质国家重点实验室（2010~）
通讯作者	Cui Bu-li
作者单位	1.Beijing Normal Univ, State Key Lab Earth Surface Proc & Resource Ecol, Beijing 100875, Peoples R China 2.Ludong Univ, Sch Resources & Environm Engn, Yantai 264025, Peoples R China 3.Chinese Acad Sci, Inst Earth Environm, State Key Lab Loess & Quaternary Geol, Xian 710061, Peoples R China
推荐引用方式 GB/T 7714	Cui Bu-li,Li Dong-sheng,Jiang Bao-fu,et al. Stable isotopes and chloride ion of precipitation events in the northeastern Tibetan Plateau, China[J]. JOURNAL OF MOUNTAIN SCIENCE,2021,18(4):834-846.
APA	Cui Bu-li.,Li Dong-sheng.,Jiang Bao-fu.,Wang Ying.,Wang Ya-xuan.,...&Li Xiao-yan.(2021).Stable isotopes and chloride ion of precipitation events in the northeastern Tibetan Plateau, China.JOURNAL OF MOUNTAIN SCIENCE,18(4),834-846.
MLA	Cui Bu-li,et al."Stable isotopes and chloride ion of precipitation events in the northeastern Tibetan Plateau, China".JOURNAL OF MOUNTAIN SCIENCE 18.4(2021):834-846.