Fei Wang

Dr. Fei Wang

The State Key Laboratory of Soil Erosion and Dryland Farming on Loess Plateau, Institute of Soil and Water Conservation, Northwest A&F University, Yangling, China
orcid

Research Focus & Metrics

Academic Career Length

22Years (2005-Present)

(Calculated once Scilit publication data is synced: current year − year of first publication + 1)

Representative Publications

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13 August 2013 in Land Degradation & Development
Verified
Journal Article
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GZGuangju Zhao
Guangju Zhao
XMXingmin Mu
Xingmin Mu
ZWZ. Wen
Z. Wen
Fei WangFei Wang
Fei Wang
PGP. Gao
P. Gao

1 September 2015 in Agricultural and Forest Meteorology
Verified
Journal Article
Closed access
WSWenyi Sun
Wenyi Sun
XSXiaoyan Song
Xiaoyan Song
XMXingmin Mu
Xingmin Mu
PGPeng Gao
Peng Gao
Fei WangFei Wang
Fei Wang
GZGuangju Zhao
Guangju Zhao

1 June 2021 in Science of The Total Environment
Verified
Journal Article
Closed access
WGWenyan Ge
Wenyan Ge
LDLiqiang Deng
Liqiang Deng
Fei WangFei Wang
Fei Wang
JHJianqiao Han
Jianqiao Han

1 November 2014 in Journal of Hydrology
Verified
Journal Article
Closed access
GZGuangju Zhao
Guangju Zhao
PTPeng Tian
Peng Tian
XMXingmin Mu
Xingmin Mu
JJJuying Jiao
Juying Jiao
Fei WangFei Wang
Fei Wang
PGPeng Gao
Peng Gao

3 January 2011 in Hydrology and Earth System Sciences
Verified
Journal Article
Open access
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Peng GaoPeng Gao
Peng Gao
XMX.-M. Mu
X.-M. Mu
Fei WangFei Wang
Fei Wang
RLR. Li
R. Li
The changes in streamflow and sediment discharge in the middle reaches of the Yellow River are a focus. In this paper, based on the precipitation, streamflow and sediment discharge series data (1950–2008), the streamflow and sediment discharge variation and its impact on precipitation/response to human activities have been analysis. The results show that significant decreasing trends in annual streamflow and sediment discharge have existed since the late 1950s in the middle reaches of the Yellow River (P = 0.01). Change-point analyses further revealed that transition years existed and that abrupt decline in streamflow and sediment discharge began in 1985 and 1981, respectively, in the middle reaches of the Yellow River (P = 0.05). Adoption of conservation measures in the 1980s and 1990s corroborates the identified transition years. Double-mass curves of precipitation vs. streamflow (sediment) for the periods before and after the transition year show remarkable decreases in proportionality of streamflow (sediment) generation. Compared with the period before the transition year, cumulative streamflow and cumulative sediment discharge reduced respectively by 17.8% and 28% during 1985–2008, which was caused by human intervention, in the middle reaches of the Yellow River. It is, therefore, concluded that human activities occupied a dominant position and played a major role in the streamflow and sediment discharge reduction in the middle reaches of the Yellow River.

1 February 2021 in Science of The Total Environment
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Journal Article
Closed access
Shangyu ShiShangyu Shi
Shangyu Shi
JYJingjie Yu
Jingjie Yu
Fei WangFei Wang
Fei Wang
PWPing Wang
Ping Wang
YZYichi Zhang
Yichi Zhang
KJKai Jin
Kai Jin