Improving the Spectral Analysis of Hydrological Signals to Efficiently Constrain Watershed Properties
Autor: | Agnès Rivière, Jonathan Schuite, Nicolas Massei, Fulvia Baratelli, Nicolas Flipo |
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Přispěvatelé: | Centre de Géosciences (GEOSCIENCES), MINES ParisTech - École nationale supérieure des mines de Paris, Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL), Morphodynamique Continentale et Côtière (M2C), Université de Caen Normandie (UNICAEN), Normandie Université (NU)-Normandie Université (NU)-Institut national des sciences de l'Univers (INSU - CNRS)-Université de Rouen Normandie (UNIROUEN), Normandie Université (NU)-Centre National de la Recherche Scientifique (CNRS) |
Jazyk: | angličtina |
Rok vydání: | 2019 |
Předmět: |
Watershed
010504 meteorology & atmospheric sciences Water flow 0208 environmental biotechnology Flow (psychology) data analysis Aquifer Soil science 02 engineering and technology 01 natural sciences Footprint Hydrology (agriculture) Vadose zone catchment [SDU.STU.HY]Sciences of the Universe [physics]/Earth Sciences/Hydrology 0105 earth and related environmental sciences Water Science and Technology watershed geography geography.geographical_feature_category Discharge 6. Clean water spectral analysis 020801 environmental engineering hydrosystem Environmental science transfer function |
Zdroj: | Water Resources Research Water Resources Research, American Geophysical Union, 2019, 55 (5), pp.4043-4065. ⟨10.1029/2018WR024579⟩ |
ISSN: | 0043-1397 1944-7973 |
DOI: | 10.1029/2018WR024579⟩ |
Popis: | (IF 4.14 [2018]; Q1); International audience; The footprint of catchment properties on water flow is reflected into hydrological signals, such as stream discharge. Here we demonstrate that it is possible to constrain catchment properties from the spectral analysis of hydrological signals but only when an appropriate transfer function (TF) is used for interpretation. We show that the appropriate theoretical TF, newly derived, is the only one to robustly describe a large diversity of experimental TFs that could be encountered in nature, because it entails the role of diffuse overflow and flow through the vadose zone, which have never been considered in spectral approaches before. The properties that may be estimated are the characteristic time scales of transfer in each compartment (surface, vadose zone, and aquifer) and the flow partitioning between surface and subsurface. We validate our approach by comparing the new and previous theoretical TFs to experimental TFs generated by a physically based distributed hydrological model, for a wide range of properties. The results confirm that without the use of the new TF, the interpretation of observed spectra may often lead to severe misestimations of catchment properties. The potential of the new TF to constrain catchment characteristics is exemplified by analyzing real hydrological signals from two watersheds with distinct behaviors. We finally discuss the broad implications of our findings and how they may contribute to a variety of topics in hydrology, thereby opening the way to a more widespread and robust use of spectral analysis to describe hydrosystems from effective rainfall, river discharge, and piezometric data. |
Databáze: | OpenAIRE |
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