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Hydrology and Earth System Sciences An interactive open-access journal of the European Geosciences Union
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Volume 22, issue 12
Hydrol. Earth Syst. Sci., 22, 6415-6434, 2018
https://doi.org/10.5194/hess-22-6415-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
Hydrol. Earth Syst. Sci., 22, 6415-6434, 2018
https://doi.org/10.5194/hess-22-6415-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.

Research article 10 Dec 2018

Research article | 10 Dec 2018

Redressing the balance: quantifying net intercatchment groundwater flows

Laurène Bouaziz et al.
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Cited articles  
Ajami, H., Troch, P. A., Maddock, T., Meixner, T., and Eastoe, C.: Quantifying mountain block recharge by means of catchment-scale storage-discharge relationships, Water Resour. Res., 47, W04504, https://doi.org/10.1029/2010WR009598., 2011.
Ameli, A., Gabrielli, C., Morgenstern, U., and McDonnell, J.: Groundwater subsidy from headwaters to their parent water watershed: A combined field-modeling approach, Water Resour. Res., 54, 5110–5125, https://doi.org/10.1029/2017WR022356, 2018.
Ameli, A. A., Beven, K., Erlandsson, M., Creed, I. F., McDonnell, J. J., and Bishop, K.: Primary weathering rates, water transit times, and concentration-discharge relations: A theoretical analysis for the critical zone, Water Resour. Res., 53, 942–960, 2017.
Andréassian, V. and Perrin, C.: On the ambiguous interpretation of the Turc-Budyko nondimensional graph, Water Resour. Res., 48, W10601, https://doi.org/10.1029/2012WR012532, 2012.
Banque Hydro: ©Ministère de l'Ecologie, du Développement Durable et de l'Energie, available at: http://hydro.eaufrance.fr/ (last access: 15 May 2017), 2015.
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We quantify net intercatchment groundwater flows in the Meuse basin in a complementary three-step approach through (1) water budget accounting, (2) testing a set of conceptual hydrological models and (3) evaluating against remote sensing actual evaporation data. We show that net intercatchment groundwater flows can make up as much as 25 % of mean annual precipitation in the headwaters and should therefore be accounted for in conceptual models to prevent overestimating actual evaporation rates.
We quantify net intercatchment groundwater flows in the Meuse basin in a complementary...
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