Articles | Volume 16, issue 1
https://doi.org/10.5194/gmd-16-353-2023
https://doi.org/10.5194/gmd-16-353-2023
Methods for assessment of models
 | 
13 Jan 2023
Methods for assessment of models |  | 13 Jan 2023

Regional coupled surface–subsurface hydrological model fitting based on a spatially distributed minimalist reduction of frequency domain discharge data

Nicolas Flipo, Nicolas Gallois, and Jonathan Schuite

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Cited articles

Abbott, M., Bathurst, J., Cunge, J., O'Connell, P., and Rasmussen, J.: An introduction to the European Hydrological System. 1. History and philosophy of a physically based distributed modelling system, J. Hydrol., 87, 45–59, 1986a. a
Abbott, M. B., Bathurst, J. C., Cunge, J. A., O'Connell, P. E., and Rasmussen, J.: An introduction to the European Hydrological System. 2. Structure of a physically based distributed modelling system, J. Hydrol., 87, 61–77, 1986b. a
Ashraf Vaghefi, S., Iravani, M., Sauchyn, D., Andreichuk, Y., Goss, G., and Faramarzi, M.: Regionalization and parameterization of a hydrologic model significantly affect the cascade of uncertainty in climate-impact projections, Clim. Dynam., 53, 2861–2886, https://doi.org/10.1007/s00382-019-04664-w, 2019. a
Baratelli, F., Flipo, N., and Moatar, F.: Estimation of distributed stream-aquifer exchanges at the regional scale using a distributed model: sensitivity to in-stream water level fluctuations, riverbed elevation and roughness, J. Hydrol., 542, 686–703, https://doi.org/10.1016/j.jhydrol.2016.09.041, 2016. a, b, c
Baratelli, F., Flipo, N., Rivière, A., and Biancamaria, S.: Retrieving river baseflow from SWOT spaceborne mission, Remote Sens. Environ., 218, 44–54, https://doi.org/10.1016/j.rse.2018.09.013, 2018. a
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Short summary
A new approach is proposed to fit hydrological or land surface models, which suffer from large uncertainties in terms of water partitioning between fast runoff and slow infiltration from small watersheds to regional or continental river basins. It is based on the analysis of hydrosystem behavior in the frequency domain, which serves as a basis for estimating water flows in the time domain with a physically based model. It opens the way to significant breakthroughs in hydrological modeling.