Your search found 8 records
1 Wang, P. P.; Zheng, C.. 1998. An efficient approach for successively perturbed groundwater models. Advances in Water Resources, 21(6):499-508.
(Location: IWMI-HQ Call no: PER Record No: H022466)
2 Wang, M.; Zheng, C.. 1998. Ground water management optimization using genetic algorithms and simulated annealing: Formulation and comparison. Journal of the American Water Resources Association, 34(3):519-530.
(Location: IWMI-HQ Call no: PER Record No: H023013)
3 Sun, M.; Zheng, C.. 1999. Long-term groundwater management by a modflow based dynamic optimization tool. Journal of the American Water Resources Association, 35(1):99-111.
(Location: IWMI-HQ Call no: PER Record No: H024432)
4 Barry, D. A.; Prommer, H.; Miller, C. T.; Engesgaard, P.; Brun, A.; Zheng, C.. 2002. Modelling the fate of oxidisable organic contaminants in groundwater. Advances in Water Resources, 25(8-12):945-983.
(Location: IWMI-HQ Call no: PER Record No: H030937)
5 Wang, P. P.; Zheng, C.; Gorelick, S. M. 2005. A general approach to advective3-dispersive transport with multirate mass transfer. Advances in Water Resources, 28(1):33-42.
(Location: IWMI-HQ Call no: PER Record No: H036663)
6 Kendy, E.; Wang, J.; Molden, David; Zheng, C.; Liu, C.; Steenhuis, T. S. 2007. Can urbanization solve inter-sector water conflicts?: Insight from a case study in Hebei Province, North China Plain. Water Policy, 9(Supplement 1):75-93.
Urbanization ; Water supply ; Groundwater ; Artificial recharge ; Water reuse ; Irrigated farming ; Water balance ; Land use ; Water budget ; Water transfer ; Water conservation ; Water use efficiency / China / Hebei Province / North China Plain / Luancheng Coynty / Shijiazhuang City / Yangze River
(Location: IWMI HQ Call no: PER Record No: H040297)
7 Clark, M. P.; Luce, C. H.; AghaKouchak, A.; Berghuijs, W.; David, C. H.; Duan, Q.; Ge, S.; van Meerveld, I.; Zheng, C.; Parlange, M. B.; Tyler, S. W. 2021. Open science: open data, open models, …and open publications? Water Resources Research, 57(4):e2020WR029480. [doi: https://doi.org/10.1029/2020WR029480]
Open science ; Open data ; Open access ; Models ; Publications ; Journals ; Funding ; Costs ; Access to information ; Institutions ; Research
(Location: IWMI HQ Call no: e-copy only Record No: H050359)
(0.19 MB)
This commentary explores the challenges and opportunities associated with a possible transition of Water Resources Research to a publication model where all articles are freely available upon publication (“Gold” open access). It provides a review of the status of open access publishing models, a summary of community input, and a path forward for AGU leadership. The decision to convert to open access is framed by a mix of finances and values. On the one hand, the challenge is to define who pays, and how, and what we can do to improve the affordability of publishing. On the other hand, the challenge is to increase the extent to which science is open and accessible. The next steps for the community include an incisive analysis of the financial feasibility of different cost models, and weighing the financial burden for open access against the desire to further advance open science.
8 Yao, Y.; Zheng, C.; Andrews, C. B.; Scanlon, B. R.; Kuang, X.; Zeng, Z.; Jeong, S.-J.; Lancia, M.; Wu, Y.; Li, G. 2021. Role of groundwater in sustaining northern Himalayan rivers. Geophysical Research Letters, 48(10):e2020GL092354. [doi: https://doi.org/10.1029/2020GL092354]
Groundwater flow ; Rivers ; Sustainability ; Stream flow ; Groundwater recharge ; Discharges ; Hydrology ; Precipitation ; Highlands ; Models / China / Himalayan Rivers / Yarlung Zangbo Basin
(Location: IWMI HQ Call no: e-copy only Record No: H050400)
https://agupubs.onlinelibrary.wiley.com/doi/epdf/10.1029/2020GL092354
https://vlibrary.iwmi.org/pdf/H050400.pdf
https://vlibrary.iwmi.org/pdf/H050400.pdf
(4.10 MB) (4.10 MB)
The Himalayas are critical for supplying water for ~2 billion people who live downstream, and available water is highly sensitive to climate change. The role of the groundwater system in sustaining the northern Himalayan rivers remains unknown, and this compromises Asia's future water sustainability. Here, we quantify the spatiotemporal contribution of groundwater to river flows in the Yarlung Zangbo Basin (upper reaches of Brahmaputra). Our results show that the groundwater recharge represents ~23% of mean annual precipitation, translating into ~30 km3/yr of baseflow, which contributes ~55% of the total river discharge in the upstream reaches to ~27% in the downstream reaches. The percentage of groundwater contribution is inversely related to topographic steepness and total precipitation, with the steepest topography and highest precipitation in the eastern Himalayas. This study fills a knowledge gap on groundwater in the Himalayas and is a foundation for projecting water changes under climatic warming.
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