• Sorted by Date • Sorted by Last Name of First Author •
Guo, Hai, Zhan, Chesheng, Zhang, Haoyue, Hu, Shi, and Li, Zhonghe, 2024. Development of anthropogenic water regulation for Community integrated Earth System model (CIESM). Journal of Hydrology, 635:131192, doi:10.1016/j.jhydrol.2024.131192.
• from the NASA Astrophysics Data System • by the DOI System •
@ARTICLE{2024JHyd..63531192G,
author = {{Guo}, Hai and {Zhan}, Chesheng and {Zhang}, Haoyue and {Hu}, Shi and {Li}, Zhonghe},
title = "{Development of anthropogenic water regulation for Community integrated Earth System model (CIESM)}",
journal = {Journal of Hydrology},
keywords = {Anthropogenic water regulation, CIESM, Water cycle, Model improvement},
year = 2024,
month = may,
volume = {635},
eid = {131192},
pages = {131192},
abstract = "{This study examines the impact of anthropogenic water regulation (AWR)
on hydroclimatic systems by incorporating an AWR module into the
Community Integrated Earth System Model (CIESM), validated
against GRACE satellite data. This approach assesses the
influence of human activities, including irrigation and
groundwater extraction, on global and regional hydrology and
climate. Key findings include: Implementation of the AWR module
significantly improves terrestrial water storage (TWS)
simulation accuracy in CIESM. The correlation coefficient for
global-scale TWS improved from 0.33 in the control (CTRL) to
0.89 in the experiment (EXP). Notably, the model's performance
enhanced in Northern India and the North China Plain, while the
Central United States showed limited improvement. AWR markedly
alters the global water cycle, evidenced by substantial
increases in soil moisture (about 0.04 to 0.02 m3/m3) and
evapotranspiration. These changes have led to increased latent
heat flux (around 5 W/m<SUP loc=``post''>2</SUP>) and a decrease
in temperature by 0.1 {\textdegree}C to 1 {\textdegree}C in
heavily irrigated regions. The study highlights the role of AWR
in modifying the energy balance, particularly in agricultural
areas where irrigation exerts a significant cooling effect.
Despite its potential, the study identifies considerable
uncertainties in coupling AWR within the CIESM model, related to
inherent model limitations, incomplete water intake data,
variable groundwater levels, and simplifications in water
transfer parameters. Future research should aim to refine these
aspects, focusing on enhancing the physical mechanisms and
performance of AWR modules in hydroclimatic simulations. In
conclusion, this research underscores the substantial
modifications in hydrological and climatic conditions due to
human activities. The improved AWR scheme within CIESM provides
valuable insights for understanding and predicting climate
change impacts on water resources, demonstrating its utility in
simulating complex hydroclimatic changes at both global and
regional scales.}",
doi = {10.1016/j.jhydrol.2024.131192},
adsurl = {https://ui.adsabs.harvard.edu/abs/2024JHyd..63531192G},
adsnote = {Provided by the SAO/NASA Astrophysics Data System}
}
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