• Sorted by Date • Sorted by Last Name of First Author •
Lu, Zhong, Li, Kuo, Zhang, Jinliang, Lei, Guoping, Yu, Ziyang, and Li, Chaoqun, 2023. Mechanisms influencing changes in water cycle processes in the changing environment of the Songnen Plain, China. Science of the Total Environment, 905:166916, doi:10.1016/j.scitotenv.2023.166916.
• from the NASA Astrophysics Data System • by the DOI System •
@ARTICLE{2023ScTEn.90566916L,
author = {{Lu}, Zhong and {Li}, Kuo and {Zhang}, Jinliang and {Lei}, Guoping and {Yu}, Ziyang and {Li}, Chaoqun},
title = "{Mechanisms influencing changes in water cycle processes in the changing environment of the Songnen Plain, China}",
journal = {Science of the Total Environment},
keywords = {Water cycle processes, Mechanisms of influence, Coupled surface-groundwater models, GRACE and GLDAS data, Songnen Plain},
year = 2023,
month = dec,
volume = {905},
eid = {166916},
pages = {166916},
abstract = "{The process of the land-surface water cycle has undergone substantial
changes as a result of climate change and human activities.
Disclosing the evolution of the water cycle and its mechanisms
in a changing environment is a challenging and hot issue in
hydrological science research, which is essential for regional
ecological protection and sustainable development. Based on the
MIKE SHE/MIKE 11 model, multi-source data are used to simulate
the water cycle change process in the Songnen Plain from 1980 to
2020. The study indicates that groundwater data inverted by
GRACE and GLDAS data is relatively accurate, which effectively
reflects the process of groundwater storage change in particular
regions. Moreover, the surface-groundwater coupling model
employs strongly correlated inverse groundwater data to simulate
the water cycle change process in the Songnen Plain, yielding
highly accurate simulation results. In terms of the impact of
climate change and human activities on the water cycle process,
climate change is the primary cause of changes in the regional
water cycle, with contributions to actual evapotranspiration,
surface runoff, and groundwater level of 77.04 \%, 70.88 \%, and
67.86 \%, respectively. Nonetheless, as human activities
intensify, their impact on the water cycle process progressively
increases. From the perspective of the mechanism of water cycle
change, the decrease in wetland area, the expansion of urban
areas, and the increase in urban water demand are the primary
causes of regional water cycle change between 1995 and 2010. The
establishment of water conservation facilities and the dramatic
increase in paddy field area are the primary causes of the water
cycle change between 2011 and 2020. This study combines multi-
source remote sensing data with hydrological models to simulate
medium- and large-scale water cycle processes, providing new
concepts and methods for examining water cycle processes in
water-scarce areas.}",
doi = {10.1016/j.scitotenv.2023.166916},
adsurl = {https://ui.adsabs.harvard.edu/abs/2023ScTEn.90566916L},
adsnote = {Provided by the SAO/NASA Astrophysics Data System}
}
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