Articles | Volume 19, issue 7
https://doi.org/10.5194/hess-19-2971-2015
https://doi.org/10.5194/hess-19-2971-2015
Research article
 | 
01 Jul 2015
Research article |  | 01 Jul 2015

Analyses of uncertainties and scaling of groundwater level fluctuations

X. Y. Liang and Y.-K. Zhang

Related authors

On the coupled unsaturated–saturated flow process induced by vertical, horizontal, and slant wells in unconfined aquifers
Xiuyu Liang, Hongbin Zhan, You-Kuan Zhang, and Jin Liu
Hydrol. Earth Syst. Sci., 21, 1251–1262, https://doi.org/10.5194/hess-21-1251-2017,https://doi.org/10.5194/hess-21-1251-2017, 2017

Related subject area

Subject: Groundwater hydrology | Techniques and Approaches: Uncertainty analysis
Data-driven estimates for the geostatistical characterization of subsurface hydraulic properties
Falk Heße, Sebastian Müller, and Sabine Attinger
Hydrol. Earth Syst. Sci., 28, 357–374, https://doi.org/10.5194/hess-28-357-2024,https://doi.org/10.5194/hess-28-357-2024, 2024
Short summary
Hierarchical sensitivity analysis for a large-scale process-based hydrological model applied to an Amazonian watershed
Haifan Liu, Heng Dai, Jie Niu, Bill X. Hu, Dongwei Gui, Han Qiu, Ming Ye, Xingyuan Chen, Chuanhao Wu, Jin Zhang, and William Riley
Hydrol. Earth Syst. Sci., 24, 4971–4996, https://doi.org/10.5194/hess-24-4971-2020,https://doi.org/10.5194/hess-24-4971-2020, 2020
Short summary
Interpretation of multi-scale permeability data through an information theory perspective
Aronne Dell'Oca, Alberto Guadagnini, and Monica Riva
Hydrol. Earth Syst. Sci., 24, 3097–3109, https://doi.org/10.5194/hess-24-3097-2020,https://doi.org/10.5194/hess-24-3097-2020, 2020
Short summary
Spatially distributed sensitivity of simulated global groundwater heads and flows to hydraulic conductivity, groundwater recharge, and surface water body parameterization
Robert Reinecke, Laura Foglia, Steffen Mehl, Jonathan D. Herman, Alexander Wachholz, Tim Trautmann, and Petra Döll
Hydrol. Earth Syst. Sci., 23, 4561–4582, https://doi.org/10.5194/hess-23-4561-2019,https://doi.org/10.5194/hess-23-4561-2019, 2019
Short summary
Multi-model approach to quantify groundwater-level prediction uncertainty using an ensemble of global climate models and multiple abstraction scenarios
Syed M. Touhidul Mustafa, M. Moudud Hasan, Ajoy Kumar Saha, Rahena Parvin Rannu, Els Van Uytven, Patrick Willems, and Marijke Huysmans
Hydrol. Earth Syst. Sci., 23, 2279–2303, https://doi.org/10.5194/hess-23-2279-2019,https://doi.org/10.5194/hess-23-2279-2019, 2019
Short summary

Cited articles

Bear, J.: Dynamics of fluids in porous media, Environmental science series (New York, 1972), American Elsevier Pub. Co., New York, xvii, 764 pp., 1972.
Bloomfield, J. P. and Little, M. A.: Robust evidence for random fractal scaling of groundwater levels in unconfined aquifers, J. Hydrol., 393, 362–369, https://doi.org/10.1016/j.jhydrol.2010.08.031, 2010.
Dagan, G.: Flow and transport in porous formations, Springer-Verlag, Berlin, New York, xvii, 465 pp., 1989.
Gelhar, L. W.: Stochastic subsurface hydrology, Prentice-Hall, Englewood Cliffs, NJ, x, 390 pp., 1993.
Hantush, M. M. and Marino, M. A.: One-Dimensional Stochastic-Analysis in Leaky Aquifers Subject to Random Leakage, Water Resour. Res., 30, 549–558, https://doi.org/10.1029/93wr02887, 1994.
Download
Short summary
The error or uncertainty in head, obtained with an analytical or numerical solution, at an early time is mainly caused by the random initial condition. The error reduces with time, later reaching a constant error. The constant error at a later time is mainly due to the effects of the uncertain source/sink. The error caused by the uncertain boundary is limited to a narrow zone. Temporal scaling of head exists in most parts of a low permeable aquifer, mainly caused by recharge fluctuation.