Articles | Volume 26, issue 15
https://doi.org/10.5194/hess-26-4169-2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/hess-26-4169-2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Evaluating downscaling methods of GRACE (Gravity Recovery and Climate Experiment) data: a case study over a fractured crystalline aquifer in southern India
Claire Pascal
CORRESPONDING AUTHOR
Centre d'Étude Spatiale de la BIOsphère, CESBIO-UPS-CNRS-IRD-CNES-INRAE, 18 av. Ed. Belin, Toulouse CEDEX 9, 31401, France
Sylvain Ferrant
Centre d'Étude Spatiale de la BIOsphère, CESBIO-UPS-CNRS-IRD-CNES-INRAE, 18 av. Ed. Belin, Toulouse CEDEX 9, 31401, France
Adrien Selles
Bureau de Recherches Géologiques et Minières (BRGM), Université de Montpellier, 1039 rue de Pinville, Montpellier, 34000, France
Jean-Christophe Maréchal
Bureau de Recherches Géologiques et Minières (BRGM), Université de Montpellier, 1039 rue de Pinville, Montpellier, 34000, France
Abhilash Paswan
National Geophysical Research Institute, CSIR, Hyderabad, India
Olivier Merlin
Centre d'Étude Spatiale de la BIOsphère, CESBIO-UPS-CNRS-IRD-CNES-INRAE, 18 av. Ed. Belin, Toulouse CEDEX 9, 31401, France
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Victoria Vanthof, Sylvain Ferrant, Romain Walcker, and Richard Kelly
Int. Arch. Photogramm. Remote Sens. Spatial Inf. Sci., XLVIII-3-2024, 565–570, https://doi.org/10.5194/isprs-archives-XLVIII-3-2024-565-2024, https://doi.org/10.5194/isprs-archives-XLVIII-3-2024-565-2024, 2024
Pierre Laluet, Luis Olivera-Guerra, Víctor Altés, Vincent Rivalland, Alexis Jeantet, Julien Tournebize, Omar Cenobio-Cruz, Anaïs Barella-Ortiz, Pere Quintana-Seguí, Josep Maria Villar, and Olivier Merlin
Hydrol. Earth Syst. Sci., 28, 3695–3716, https://doi.org/10.5194/hess-28-3695-2024, https://doi.org/10.5194/hess-28-3695-2024, 2024
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Monitoring agricultural drainage flow in irrigated areas is key to water and soil management. In this paper, four simple drainage models are evaluated on two irrigated sub-basins where drainage flow is measured daily. The evaluation of their precision shows that they simulate drainage very well when calibrated with drainage data and that one of them is slightly better. The evaluation of their accuracy shows that only one model can provide rough drainage estimates without calibration data.
Yassine Khardi, Guillaume Lacombe, Benoit Dewandel, Abdelilah Taky, Jean-Christophe Maréchal, Ali Hammani, and Sami Bouarfa
Proc. IAHS, 385, 47–52, https://doi.org/10.5194/piahs-385-47-2024, https://doi.org/10.5194/piahs-385-47-2024, 2024
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A 6400 m3 on-farm storage basin was built along a wadi in pre-Saharan Morocco to store floodwater for date palm irrigation. Its effect on the water table is confirmed by monitoring surface and groundwater levels and modeling the spatiotemporal variability of the recorded flood-induced piezometric mound. We show that beneficial replenishment of the water table is localized (radius < 360 m) and decreases over time due to the basin siltation reducing its storage capacity and permeability.
Bouchra Ait Hssaine, Olivier Merlin, Jamal Ezzahar, Nitu Ojha, Salah Er-Raki, and Said Khabba
Hydrol. Earth Syst. Sci., 24, 1781–1803, https://doi.org/10.5194/hess-24-1781-2020, https://doi.org/10.5194/hess-24-1781-2020, 2020
S. Ferrant, A. Selles, M. Le Page, A. AlBitar, S. Mermoz, S. Gascoin, A. Bouvet, S. Ahmed, and Y. Kerr
Int. Arch. Photogramm. Remote Sens. Spatial Inf. Sci., XLII-3-W6, 285–292, https://doi.org/10.5194/isprs-archives-XLII-3-W6-285-2019, https://doi.org/10.5194/isprs-archives-XLII-3-W6-285-2019, 2019
J. Chirouze, G. Boulet, L. Jarlan, R. Fieuzal, J. C. Rodriguez, J. Ezzahar, S. Er-Raki, G. Bigeard, O. Merlin, J. Garatuza-Payan, C. Watts, and G. Chehbouni
Hydrol. Earth Syst. Sci., 18, 1165–1188, https://doi.org/10.5194/hess-18-1165-2014, https://doi.org/10.5194/hess-18-1165-2014, 2014
T. Reimann, M. Giese, T. Geyer, R. Liedl, J. C. Maréchal, and W. B. Shoemaker
Hydrol. Earth Syst. Sci., 18, 227–241, https://doi.org/10.5194/hess-18-227-2014, https://doi.org/10.5194/hess-18-227-2014, 2014
O. Merlin
Hydrol. Earth Syst. Sci., 17, 3623–3637, https://doi.org/10.5194/hess-17-3623-2013, https://doi.org/10.5194/hess-17-3623-2013, 2013
Related subject area
Subject: Groundwater hydrology | Techniques and Approaches: Remote Sensing and GIS
Influence of intensive agriculture and geological heterogeneity on the recharge of an arid aquifer system (Saq–Ram, Arabian Peninsula) inferred from GRACE data
Preprocessing approaches in machine-learning-based groundwater potential mapping: an application to the Koulikoro and Bamako regions, Mali
Applicability of Landsat 8 thermal infrared sensor for identifying submarine groundwater discharge springs in the Mediterranean Sea basin
Unsaturated zone model complexity for the assimilation of evapotranspiration rates in groundwater modelling
Technical note: Water table mapping accounting for river–aquifer connectivity and human pressure
Estimating long-term groundwater storage and its controlling factors in Alberta, Canada
Recent changes in terrestrial water storage in the Upper Nile Basin: an evaluation of commonly used gridded GRACE products
Mapping irrigation potential from renewable groundwater in Africa – a quantitative hydrological approach
How to identify groundwater-caused thermal anomalies in lakes based on multi-temporal satellite data in semi-arid regions
Statistical analysis to characterize transport of nutrients in groundwater near an abandoned feedlot
Hydrogeological settings of a volcanic island (San Cristóbal, Galapagos) from joint interpretation of airborne electromagnetics and geomorphological observations
Shallow groundwater effect on land surface temperature and surface energy balance under bare soil conditions: modeling and description
Reconnoitering the effect of shallow groundwater on land surface temperature and surface energy balance using MODIS and SEBS
Derivation of groundwater flow-paths based on semi-automatic extraction of lineaments from remote sensing data
Groundwater use for irrigation – a global inventory
Pierre Seraphin, Julio Gonçalvès, Bruno Hamelin, Thomas Stieglitz, and Pierre Deschamps
Hydrol. Earth Syst. Sci., 26, 5757–5771, https://doi.org/10.5194/hess-26-5757-2022, https://doi.org/10.5194/hess-26-5757-2022, 2022
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This study assesses the detailed water budget of the Saq–Ram Aquifer System using satellite gravity data. Spatial heterogeneities regarding the groundwater recharge were identified: (i) irrigation excess is great enough to artificially recharge the aquifer; and (ii) volcanic lava deposits, which cover 8% of the domain, contribute to more than 50% of the total natural recharge. This indicates a major control of geological context on arid aquifer recharge, which has been poorly discussed hitherto.
Víctor Gómez-Escalonilla, Pedro Martínez-Santos, and Miguel Martín-Loeches
Hydrol. Earth Syst. Sci., 26, 221–243, https://doi.org/10.5194/hess-26-221-2022, https://doi.org/10.5194/hess-26-221-2022, 2022
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Many communities in the Sahel rely solely on groundwater. We develop a machine learning technique to map areas of groundwater potential. Algorithms are trained to detect areas where there is a confluence of factors that facilitate groundwater occurrence. Our contribution focuses on using variable scaling to minimize expert bias and on testing our results beyond standard metrics. This approach is illustrated through its application to two administrative regions of Mali.
Sònia Jou-Claus, Albert Folch, and Jordi Garcia-Orellana
Hydrol. Earth Syst. Sci., 25, 4789–4805, https://doi.org/10.5194/hess-25-4789-2021, https://doi.org/10.5194/hess-25-4789-2021, 2021
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Satellite thermal infrared (TIR) remote sensing is a useful method for identifying coastal springs in karst aquifers both locally and regionally. The limiting factors include technical limitations, geological and hydrogeological characteristics, environmental and marine conditions, and coastal geomorphology. Also, it can serve as a tool to use for a first screening of the coastal water surface temperature to identify possible thermal anomalies that will help narrow the sampling survey.
Simone Gelsinari, Valentijn R. N. Pauwels, Edoardo Daly, Jos van Dam, Remko Uijlenhoet, Nicholas Fewster-Young, and Rebecca Doble
Hydrol. Earth Syst. Sci., 25, 2261–2277, https://doi.org/10.5194/hess-25-2261-2021, https://doi.org/10.5194/hess-25-2261-2021, 2021
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Estimates of recharge to groundwater are often driven by biophysical processes occurring in the soil column and, particularly in remote areas, are also always affected by uncertainty. Using data assimilation techniques to merge remotely sensed observations with outputs of numerical models is one way to reduce this uncertainty. Here, we show the benefits of using such a technique with satellite evapotranspiration rates and coupled hydrogeological models applied to a semi-arid site in Australia.
Mathias Maillot, Nicolas Flipo, Agnès Rivière, Nicolas Desassis, Didier Renard, Patrick Goblet, and Marc Vincent
Hydrol. Earth Syst. Sci., 23, 4835–4849, https://doi.org/10.5194/hess-23-4835-2019, https://doi.org/10.5194/hess-23-4835-2019, 2019
Soumendra N. Bhanja, Xiaokun Zhang, and Junye Wang
Hydrol. Earth Syst. Sci., 22, 6241–6255, https://doi.org/10.5194/hess-22-6241-2018, https://doi.org/10.5194/hess-22-6241-2018, 2018
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The paper presents groundwater storage conditions in all the major river basins across Alberta, Canada. We used remote-sensing data and investigate their performance using available ground-based data of groundwater level monitoring, storage coefficients, aquifer thickness, and surface water measurements. The water available for groundwater recharge has been studied in detail. Separate approaches have been followed for confined and unconfined aquifers for estimating groundwater storage.
Mohammad Shamsudduha, Richard G. Taylor, Darren Jones, Laurent Longuevergne, Michael Owor, and Callist Tindimugaya
Hydrol. Earth Syst. Sci., 21, 4533–4549, https://doi.org/10.5194/hess-21-4533-2017, https://doi.org/10.5194/hess-21-4533-2017, 2017
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This study tests the phase and amplitude of GRACE TWS signals in the Upper Nile Basin from five commonly used gridded products (NASA's GRCTellus: CSR, JPL, GFZ; JPL-Mascons; GRGS) using in situ data and soil moisture from the Global Land Data Assimilation System. Resolution of changes in groundwater storage (ΔGWS) from GRACE is greatly constrained by the uncertain simulated soil moisture storage and the low amplitude in ΔGWS observed in deeply weathered crystalline rocks in the Upper Nile Basin.
Y. Altchenko and K. G. Villholth
Hydrol. Earth Syst. Sci., 19, 1055–1067, https://doi.org/10.5194/hess-19-1055-2015, https://doi.org/10.5194/hess-19-1055-2015, 2015
U. Mallast, R. Gloaguen, J. Friesen, T. Rödiger, S. Geyer, R. Merz, and C. Siebert
Hydrol. Earth Syst. Sci., 18, 2773–2787, https://doi.org/10.5194/hess-18-2773-2014, https://doi.org/10.5194/hess-18-2773-2014, 2014
P. Gbolo and P. Gerla
Hydrol. Earth Syst. Sci., 17, 4897–4906, https://doi.org/10.5194/hess-17-4897-2013, https://doi.org/10.5194/hess-17-4897-2013, 2013
A. Pryet, N. d'Ozouville, S. Violette, B. Deffontaines, and E. Auken
Hydrol. Earth Syst. Sci., 16, 4571–4579, https://doi.org/10.5194/hess-16-4571-2012, https://doi.org/10.5194/hess-16-4571-2012, 2012
F. Alkhaier, G. N. Flerchinger, and Z. Su
Hydrol. Earth Syst. Sci., 16, 1817–1831, https://doi.org/10.5194/hess-16-1817-2012, https://doi.org/10.5194/hess-16-1817-2012, 2012
F. Alkhaier, Z. Su, and G. N. Flerchinger
Hydrol. Earth Syst. Sci., 16, 1833–1844, https://doi.org/10.5194/hess-16-1833-2012, https://doi.org/10.5194/hess-16-1833-2012, 2012
U. Mallast, R. Gloaguen, S. Geyer, T. Rödiger, and C. Siebert
Hydrol. Earth Syst. Sci., 15, 2665–2678, https://doi.org/10.5194/hess-15-2665-2011, https://doi.org/10.5194/hess-15-2665-2011, 2011
S. Siebert, J. Burke, J. M. Faures, K. Frenken, J. Hoogeveen, P. Döll, and F. T. Portmann
Hydrol. Earth Syst. Sci., 14, 1863–1880, https://doi.org/10.5194/hess-14-1863-2010, https://doi.org/10.5194/hess-14-1863-2010, 2010
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Short summary
This paper presents a new validation method for the downscaling of GRACE (Gravity Recovery and Climate Experiment) data. It measures the improvement of the downscaled data against the low-resolution data in both temporal and, for the first time, spatial domains. This validation method offers a standardized and comprehensive framework to interpret spatially and temporally the quality of the downscaled products, supporting future efforts in GRACE downscaling methods.
This paper presents a new validation method for the downscaling of GRACE (Gravity Recovery and...