Haijing Shi

Dr. Haijing Shi

orcid

Research Focus & Metrics

Academic Career Length

13Years (2014-Present)

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

Representative Publications

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1 February 2020 in Geomorphology
Verified
Journal Article
Closed access
YJYanmin Jiang
Yanmin Jiang
Haijing ShiHaijing Shi
Haijing Shi
ZWZhongming Wen
Zhongming Wen
MGMinghang Guo
Minghang Guo
JZJun Zhao
Jun Zhao
CZCheng Zheng
Cheng Zheng

1 August 2016 in CATENA
Verified
Journal Article
Closed access
MGMinghang Guo
Minghang Guo
Haijing ShiHaijing Shi
Haijing Shi
JZJun Zhao
Jun Zhao
PLPuling Liu
Puling Liu
DWDustin Welbourne
Dustin Welbourne
QLQi Lin
Qi Lin

1 December 2016 in Biological Conservation
Verified
Journal Article
Closed access
Haijing ShiHaijing Shi
Haijing Shi
Zhongming WenZhongming Wen
Zhongming Wen
DPDavid Paull
David Paull
MGMinghang Guo
Minghang Guo

1 December 2014 in Biological Conservation
Verified
Journal Article
Closed access
Haijing ShiHaijing Shi
Haijing Shi
DPDavid Paull
David Paull
ZWZhongming Wen
Zhongming Wen
LBLinda Broome
Linda Broome

7 November 2023 in Remote Sensing
Verified
Journal Article
Open access
PDF file
ZLZiqi Lin
Ziqi Lin
YLYangyang Liu
Yangyang Liu
Zhongming WenZhongming Wen
Zhongming Wen
XCXu Chen
Xu Chen
PHPeidong Han
Peidong Han
Haijing ShiHaijing Shi
Haijing Shi
Vegetation net primary productivity (NPP) serves as a crucial and intuitive indicator for assessing ecosystem health. However, the nonlinear dynamics and influencing factors operating at various time scales are not yet fully understood. Here, the ensemble empirical mode decomposition (EEMD) method was used to analyze the spatiotemporal patterns of NPP and its association with hydrothermal factors and anthropogenic activities across different temporal scales for the Yellow River Basin (YRB) from 2000 to 2020. The results indicate that: (1) the annual average NPP was 236.37 g C/m2 in the YRB and increased at rates of 4.64 g C/m2/a1 (R2 = 0.86, p < 0.01) during 2000 to 2020. Spatially, nonlinear analysis indicates that 72.77% of the study area exhibits a predominantly increasing trend in NPP, while 25.17% exhibits a reversing trend. (2) On a 3-year time scale, warming has resulted in an increase in NPP in the majority of areas of the study area (69.49%). As the time scale widens, the response of vegetation to climate change becomes more prominent; especially under the long-term trend, the percentage areas of the correlation between vegetation and precipitation and temperature increased with significance, reaching 48.21% and 11.57%, respectively. (3) Through comprehensive time analysis and multivariate regression analysis, it was confirmed that both human activities and climate factors had comparable impacts on vegetation growth. Among different vegetation types, climate was still the main factor affecting grassland NPP, and only 15.74% of grassland was affected by human activities. For shrubland, forest, and farmland, human activity was a dominating factor for vegetation NPP change. There are still few studies on vegetation change using nonlinear methods in the Yellow River Basin, and most studies have not considered the effect of time scale on vegetation evolution. The findings highlight the significance of multi-time scale analysis in understanding the vegetation dynamics and providing scientific guidance for future vegetation restoration and conservation efforts.

7 January 2015 in Austral Ecology
Verified
Journal Article
Closed access
PDF file
Haijing ShiHaijing Shi
Haijing Shi
DPDavid Paull
David Paull
LBLinda Broome
Linda Broome
HBHayley Bates
Hayley Bates