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	Detecting hydrological consistency between soil moisture and precipitation and changes of soil moisture in summer over the Tibetan Plateau
	Meng, X.1,6; Li, R.2; Luan, L.1,3; Lyu, S.4,5; Zhang, T.1; Ao, Y.1; Han, B.1; Zhao, L.1; Ma, Y.1,3
刊名	CLIMATE DYNAMICS
	2018-12-01
卷号	51期号:11-12页码:4157-4168
关键词	Hydrological consistency ESA soil moisture product Soil moisture Precipitation Trends Tibetan Plateau
ISSN号	0930-7575
DOI	10.1007/s00382-017-3646-5
通讯作者	Meng, X.(mxh@lzb.ac.cn)
英文摘要	As the first purely multi-decadal satellite-based soil moisture product that spans over 35years (from November 1978 to December 2013) on a daily basis designed for climate application, the applicability of the European Space Agency (ESA) soil moisture product, including the hydrological consistency between the product and the observed precipitation and the product continuity on the Tibetan Plateau (TP) were investigated. The results show that there is significant degree between the ESA soil moisture product and the observed precipitation. The positive anomaly of the ESA soil moisture product can reflect the occurrences of precipitation, but the precipitation may not definitely lead to soil moisture anomaly, which largely depends on the precipitation amounts. For climate application, large number of missing gaps was shown on the west of the TP, where it is considered that the retrieval algorithms are largely affected by the permafrost covered in this region, leaving the ESA soil moisture product for further improvement. In application, the ESA soil moisture product was used to study the response of surface soil moisture to climate change on the TP. With the rapid warming and the overall wetting of the TP, soil moisture increases on the central of the TP with the increase of precipitation, and decreases in the southeast TP with the precipitation deduction. However, it decreases in the west TP, where it was probably influenced by both the insignificant precipitation changes and the significant increase of evaporation.
收录类别	SCI ; ISTP
WOS关键词	ATMOSPHERE INTERACTIONS ; CLIMATE-CHANGE ; MANN-KENDALL ; HEAT-SOURCE ; TREND ; PERMAFROST ; VEGETATION ; SATELLITE ; WATER ; PART
WOS研究方向	Meteorology & Atmospheric Sciences
WOS类目	Meteorology & Atmospheric Sciences
语种	英语
出版者	SPRINGER
WOS记录号	WOS:000451725600014
内容类型	期刊论文
URI标识	http://www.corc.org.cn/handle/1471x/2558251
专题	寒区旱区环境与工程研究所
通讯作者	Meng, X.
作者单位	1.Chinese Acad Sci, Northwest Inst Ecoenvironm & Resources, Key Lab Land Surface Proc & Climate Change Cold &, Lanzhou 730000, Peoples R China 2.Neimenggu Meteorol Ctr, Neimenggu 010051, Peoples R China 3.Univ Chinese Acad Sci, Beijing 100049, Peoples R China 4.Chengdu Univ Informat Technol, Sch Atmospher Sci, Plateau Atmosphere & Environm Key Lab Sichuan Pro, Chengdu 610225, Sichuan, Peoples R China 5.Nanjing Univ Informat Sci & Technol, Collaborat Innovat Ctr Forecast & Evaluat Meteoro, Nanjing 210044, Jiangsu, Peoples R China 6.Chinese Acad Sci, Northwest Inst Ecoenvironm & Resources, Zoige Plateau Wetlands Ecosyst Res Stn, 320 Donggang West Rd, Lanzhou 730000, Peoples R China
推荐引用方式 GB/T 7714	Meng, X.,Li, R.,Luan, L.,et al. Detecting hydrological consistency between soil moisture and precipitation and changes of soil moisture in summer over the Tibetan Plateau[J]. CLIMATE DYNAMICS,2018,51(11-12):4157-4168.
APA	Meng, X..,Li, R..,Luan, L..,Lyu, S..,Zhang, T..,...&Ma, Y..(2018).Detecting hydrological consistency between soil moisture and precipitation and changes of soil moisture in summer over the Tibetan Plateau.CLIMATE DYNAMICS,51(11-12),4157-4168.
MLA	Meng, X.,et al."Detecting hydrological consistency between soil moisture and precipitation and changes of soil moisture in summer over the Tibetan Plateau".CLIMATE DYNAMICS 51.11-12(2018):4157-4168.

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