干旱区生态环境知识资源中心(Arid): Runoff variation and its response to climate change in Huolin River catchment, Northeast China

Arid

DOI	10.1007/s11629-021-6858-4
	Runoff variation and its response to climate change in Huolin River catchment, Northeast China
	Dan Dan; Chun Xi; Shi Lei; Xia Ying-ying; Zhou Hai-jun; Wan Zhi-qiang
通讯作者	Chun, X (corresponding author), Inner Mongolia Normal Univ, Inner Mongolia Restorat Engn Lab Wetland Ecoenvir, Hohhot 010022, Peoples R China. ; Chun, X (corresponding author), Inner Mongolia Normal Univ, Key Lab Mongolian Plateaus Climate Syst, Hohhot 010022, Peoples R China.
来源期刊	JOURNAL OF MOUNTAIN SCIENCE
ISSN	1672-6316
EISSN	1993-0321
出版年	2021
英文摘要	The Huolin River catchment (HRC) is located in the semi-arid region of Northeast China, which is very sensitive to climate change. The runoff in HRC is closely related to the recovery of local vegetation in the Greater Khingan Mountains and the survival of downstream wetlands. Dramatic runoff fluctuations and increasing no-flow days confirmed the water crisis in this area. Hence, it is extremely urgent to study the current situation and characteristics of runoff. In this study, hydrological and meteorological data of HRC during 1956-2018 were analyzed to elucidate the processes, characteristics, trends of the river runoff and revealed its response to climate change. The Mann-Kendall test and linear regression method showed that runoff in the HRC demonstrated a downward trend over the study period with a marked annual variation. The runoff in the high flow years was 100 times that of the low flow years, showing a typical continental climatic river characteristic. There are two runoff peak flows in the intra-annual runoff distribution in March and July, whereas two runoff valleys occurred around May and September to February. The runoff positively correlates with precipitation in summer and temperature in early spring. Snowmelt influenced by rising temperatures in April and precipitation in July is the main driving factor for the two peaks flow. Evaporation rose with precipitation decline and temperature increased, which may influence the runoff decrease. The annual runoff is well synchronized with the annual precipitation, and precipitation change is the main driving factor of variation and abrupt change points of annual runoff in the catchment. This study would be beneficial for water resource management in developing adaptation strategies to offset the negative impact of climate change in HRC.
英文关键词	Precipitation-runoff system Mann-Kendall test Abrupt change Regional response Semi-arid area
类型	Article
语种	英语
收录类别	SCI-E
WOS记录号	WOS:000717932900001
WOS关键词	ASIAN SUMMER MONSOON ; YELLOW-RIVER ; WATER-RESOURCES ; YANGTZE-RIVER ; ABRUPT CHANGE ; EAST CHINA ; STREAMFLOW ; VARIABILITY ; PRECIPITATION ; IMPACTS
WOS类目	Environmental Sciences
WOS研究方向	Environmental Sciences & Ecology
资源类型	期刊论文
条目标识符	http://119.78.100.177/qdio/handle/2XILL650/367669
作者单位	[Dan Dan; Chun Xi; Shi Lei; Xia Ying-ying; Zhou Hai-jun; Wan Zhi-qiang] Inner Mongolia Normal Univ, Inner Mongolia Restorat Engn Lab Wetland Ecoenvir, Hohhot 010022, Peoples R China; [Dan Dan; Chun Xi; Shi Lei; Xia Ying-ying; Zhou Hai-jun; Wan Zhi-qiang] Inner Mongolia Normal Univ, Key Lab Mongolian Plateaus Climate Syst, Hohhot 010022, Peoples R China; [Dan Dan; Shi Lei; Xia Ying-ying; Zhou Hai-jun; Wan Zhi-qiang] Inner Mongolia Normal Univ, Coll Geog Sci, Hohhot 010022, Peoples R China
推荐引用方式 GB/T 7714	Dan Dan,Chun Xi,Shi Lei,et al. Runoff variation and its response to climate change in Huolin River catchment, Northeast China[J],2021.
APA	Dan Dan,Chun Xi,Shi Lei,Xia Ying-ying,Zhou Hai-jun,&Wan Zhi-qiang.(2021).Runoff variation and its response to climate change in Huolin River catchment, Northeast China.JOURNAL OF MOUNTAIN SCIENCE.
MLA	Dan Dan,et al."Runoff variation and its response to climate change in Huolin River catchment, Northeast China".JOURNAL OF MOUNTAIN SCIENCE (2021).