The impact of hillslope groundwater dynamics and landscape functioning in event-flow generation: a field study in the Rietholzbach catchment, Switzerland

A reliable prediction of hydrograph responses in mountainous headwater catchments requires a mechanistic understanding of the coupled hydro-climatic processes in these regions. This study shows that only a small fraction of the total area in a pre-Alpine headwater catchment actively regulates stream...

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Vydané v:	Hydrogeology journal Ročník 23; číslo 5; s. 935 - 948
Hlavní autori:	von Freyberg, Jana, Rao, P. Suresh C., Radny, Dirk, Schirmer, Mario
Médium:	Journal Article
Jazyk:	English
Vydavateľské údaje:	Berlin/Heidelberg Springer Berlin Heidelberg 01.08.2015 Springer Nature B.V
Predmet:	Aquatic Pollution aquifers Base flow Catchment areas Catchments Discharge Earth and Environmental Science Earth Sciences Environmental impact Field study Geology Geophysics/Geodesy Groundwater Groundwater discharge Groundwater flow Groundwater recharge Headwaters Hydrogeology hydrograph Hydrographs Hydrology Hydrology/Water Resources Landscape Landscape ecology Landscapes Mathematical models Mountains prediction rain riparian areas Riparian land River discharge River flow rivers Stream discharge Stream flow subsurface flow Surface runoff Switzerland time series analysis Waste Water Technology Water Management Water Pollution Control Water Quality/Water Pollution watersheds Switzerland Switzerland, St. Gall, Rietholzbach Rainfall/runoff Groundwater recharge/water budget Minimalistic model Mountainous catchments Switzerland
ISSN:	1431-2174, 1435-0157
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Abstract	A reliable prediction of hydrograph responses in mountainous headwater catchments requires a mechanistic understanding of the coupled hydro-climatic processes in these regions. This study shows that only a small fraction of the total area in a pre-Alpine headwater catchment actively regulates streamflow responses to hydro-climatic forcing, which facilitates the application of a parsimonious framework for hydrograph time-series prediction. Based on landscape analysis and hydrometric data from the Upper Rietholzbach catchment (URHB, 0.94 km 2 , northeast Switzerland), a conceptual model was established. Here, the rainfall-event-driven contribution of surface runoff and subsurface flow (event flow) accounts for around 50 % of total river discharge. The event-flow hydrograph is generated from approximately 25 % of the entire area consisting of riparian zones (8 %) and adjacent hillslopes (17 %), each with characteristic streamflow-generating mechanisms. Baseflow generation is attributed to deep groundwater discharge from a fractured-rock aquifer covering ∼75 % of the catchment area. A minimalistic model, that represents event flow as depletion of two parallel linear reservoirs, verified the conceptual model of the URHB with adequate hydrograph simulations ( R 2 = 0.67, Nash-Sutcliffe efficiency (NSE) = 0.64). Hereby, the expansion of the event-flow contributing areas was found to be particularly significant during long and high-intensity rainfall events. These findings provide a generalized approach for the large-scale characterization of groundwater recharge and hydrological behavior of mountainous catchments with similar landscape properties.
AbstractList	A reliable prediction of hydrograph responses in mountainous headwater catchments requires a mechanistic understanding of the coupled hydro-climatic processes in these regions. This study shows that only a small fraction of the total area in a pre-Alpine headwater catchment actively regulates streamflow responses to hydro-climatic forcing, which facilitates the application of a parsimonious framework for hydrograph time-series prediction. Based on landscape analysis and hydrometric data from the Upper Rietholzbach catchment (URHB, 0.94 km super(2), northeast Switzerland), a conceptual model was established. Here, the rainfall-event-driven contribution of surface runoff and subsurface flow (event flow) accounts for around 50 % of total river discharge. The event-flow hydrograph is generated from approximately 25 % of the entire area consisting of riparian zones (8 %) and adjacent hillslopes (17 %), each with characteristic streamflow-generating mechanisms. Baseflow generation is attributed to deep groundwater discharge from a fractured-rock aquifer covering 75 % of the catchment area. A minimalistic model, that represents event flow as depletion of two parallel linear reservoirs, verified the conceptual model of the URHB with adequate hydrograph simulations (R super(2)=0.67, Nash-Sutcliffe efficiency (NSE)=0.64). Hereby, the expansion of the event-flow contributing areas was found to be particularly significant during long and high-intensity rainfall events. These findings provide a generalized approach for the large-scale characterization of groundwater recharge and hydrological behavior of mountainous catchments with similar landscape properties.Original Abstract: Une prediction fiable des reponses hydrologiques dans les bassins versants amont de montagne necessite une apprehension mecaniste des processus couples hydroclimatiques dans ces regions. La presente etude montre que seule une petite fraction de la surface totale d'un bassin versant amont des Prealpes regule activement les reponses de l'ecoulement au forcage hydro-climatique, ce qui rend possible l'utilisation d'un cadre parcimonieux pour la prediction des chroniques hydrologiques. Sur la base d'une analyse du paysage et des donnees hydrometriques relatives au bassin versant du Haut Rietholzbach (HRHB, 0.94 km super(2), Nord Est de la Suisse) un modele conceptuel a ete elabore. Ici la contribution du ruissellement de surface et de l'ecoulement de subsurface (l'evenement hydrologique), induite par un evenement pluvieux, atteint environ 50 % du debit total de la riviere. L'hydrogramme en reponse a un evenement pluvieux est genere par environ 25 % de la surface totale, qui comprend les zones riveraines du cours d'eau (8 %) et les versants adjacents (17 %), chacun ayant des mecanismes specifiques de generation de l'ecoulement. La generation de l'ecoulement de base est attribuee a la decharge des eaux souterraines profondes depuis un aquifere de roches fracturees couvrant a peu pres 75 % du bassin versant. Un modele minimaliste, qui represente l'evenement hydrologique comme la vidange de deux reservoirs en parallele a reponse lineaire, conforte le modele conceptuel du HRHB, avec des simulations hydrologiques satisfaisantes (R super(2)=0.67, coefficient d'efficacite Nash-Sutcliffe (CENS)=0.64). En l'espece, l'extension des zones contribuant a la reponse hydrologique a un evenement pluvieux s'est trouvee etre particulierement importante pendant les evenements pluvieux de longue duree et de forte intensite. Ces conclusions conduisent a une approche generalisee de la caracterisation a grande echelle de la recharge des eaux souterraines et du comportement hydrologique des bassins versants de montagne presentant des proprietes paysageres similaires. A reliable prediction of hydrograph responses in mountainous headwater catchments requires a mechanistic understanding of the coupled hydro-climatic processes in these regions. This study shows that only a small fraction of the total area in a pre-Alpine headwater catchment actively regulates streamflow responses to hydro-climatic forcing, which facilitates the application of a parsimonious framework for hydrograph time-series prediction. Based on landscape analysis and hydrometric data from the Upper Rietholzbach catchment (URHB, 0.94 km 2 , northeast Switzerland), a conceptual model was established. Here, the rainfall-event-driven contribution of surface runoff and subsurface flow (event flow) accounts for around 50 % of total river discharge. The event-flow hydrograph is generated from approximately 25 % of the entire area consisting of riparian zones (8 %) and adjacent hillslopes (17 %), each with characteristic streamflow-generating mechanisms. Baseflow generation is attributed to deep groundwater discharge from a fractured-rock aquifer covering ∼75 % of the catchment area. A minimalistic model, that represents event flow as depletion of two parallel linear reservoirs, verified the conceptual model of the URHB with adequate hydrograph simulations ( R 2 = 0.67, Nash-Sutcliffe efficiency (NSE) = 0.64). Hereby, the expansion of the event-flow contributing areas was found to be particularly significant during long and high-intensity rainfall events. These findings provide a generalized approach for the large-scale characterization of groundwater recharge and hydrological behavior of mountainous catchments with similar landscape properties. A reliable prediction of hydrograph responses in mountainous headwater catchments requires a mechanistic understanding of the coupled hydro-climatic processes in these regions. This study shows that only a small fraction of the total area in a pre-Alpine headwater catchment actively regulates streamflow responses to hydro-climatic forcing, which facilitates the application of a parsimonious framework for hydrograph time-series prediction. Based on landscape analysis and hydrometric data from the Upper Rietholzbach catchment (URHB, 0.94 km^sup 2^, northeast Switzerland), a conceptual model was established. Here, the rainfall-event-driven contribution of surface runoff and subsurface flow (event flow) accounts for around 50 % of total river discharge. The event-flow hydrograph is generated from approximately 25 % of the entire area consisting of riparian zones (8 %) and adjacent hillslopes (17 %), each with characteristic streamflow-generating mechanisms. Baseflow generation is attributed to deep groundwater discharge from a fractured-rock aquifer covering 75 % of the catchment area. A minimalistic model, that represents event flow as depletion of two parallel linear reservoirs, verified the conceptual model of the URHB with adequate hydrograph simulations (R ^sup 2^=0.67, Nash-Sutcliffe efficiency (NSE)=0.64). Hereby, the expansion of the event-flow contributing areas was found to be particularly significant during long and high-intensity rainfall events. These findings provide a generalized approach for the large-scale characterization of groundwater recharge and hydrological behavior of mountainous catchments with similar landscape properties. A reliable prediction of hydrograph responses in mountainous headwater catchments requires a mechanistic understanding of the coupled hydro-climatic processes in these regions. This study shows that only a small fraction of the total area in a pre-Alpine headwater catchment actively regulates streamflow responses to hydro-climatic forcing, which facilitates the application of a parsimonious framework for hydrograph time-series prediction. Based on landscape analysis and hydrometric data from the Upper Rietholzbach catchment (URHB, 0.94 km², northeast Switzerland), a conceptual model was established. Here, the rainfall-event-driven contribution of surface runoff and subsurface flow (event flow) accounts for around 50 % of total river discharge. The event-flow hydrograph is generated from approximately 25 % of the entire area consisting of riparian zones (8 %) and adjacent hillslopes (17 %), each with characteristic streamflow-generating mechanisms. Baseflow generation is attributed to deep groundwater discharge from a fractured-rock aquifer covering ∼75 % of the catchment area. A minimalistic model, that represents event flow as depletion of two parallel linear reservoirs, verified the conceptual model of the URHB with adequate hydrograph simulations (R ² = 0.67, Nash-Sutcliffe efficiency (NSE) = 0.64). Hereby, the expansion of the event-flow contributing areas was found to be particularly significant during long and high-intensity rainfall events. These findings provide a generalized approach for the large-scale characterization of groundwater recharge and hydrological behavior of mountainous catchments with similar landscape properties.
Author	Rao, P. Suresh C. von Freyberg, Jana Schirmer, Mario Radny, Dirk
Author_xml	– sequence: 1 givenname: Jana surname: von Freyberg fullname: von Freyberg, Jana email: jana.vonfreyberg@usys.ethz.ch organization: Department of Environmental Systems Science, Swiss Federal Institute of Technology Zürich, Department of Water Resources and Drinking Water, Eawag Swiss Federal Institute of Aquatic Science and Technology, Centre for Hydrogeology and Geothermics (CHYN), University of Neuchâtel – sequence: 2 givenname: P. Suresh C. surname: Rao fullname: Rao, P. Suresh C. organization: Lyles School of Civil Engineering & Agronomy Department, Purdue University – sequence: 3 givenname: Dirk surname: Radny fullname: Radny, Dirk organization: Department of Water Resources and Drinking Water, Eawag Swiss Federal Institute of Aquatic Science and Technology – sequence: 4 givenname: Mario surname: Schirmer fullname: Schirmer, Mario organization: Department of Water Resources and Drinking Water, Eawag Swiss Federal Institute of Aquatic Science and Technology, Centre for Hydrogeology and Geothermics (CHYN), University of Neuchâtel
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CitedBy_id	crossref_primary_10_5194_hess_22_3841_2018 crossref_primary_10_1016_j_earscirev_2017_10_010 crossref_primary_10_1002_hyp_13878 crossref_primary_10_1080_00207233_2017_1288059
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Mitteilungen der Versuchsanstalt für Wasserbau, Hydrologie und Glaziologie der ETH, Zürich, 51 pp McGlynnBLSeibertJDistributed assessment of contributing area and riparian buffering along stream networksWater Resour Res2003391082 RinaldoABevenKJBertuzzoENicotinaLDaviesJFioriARussoDBotterGCatchment travel time distributions and water flow in soilsWater Resour Res201147 Koenig P, Lang H, Schwarze R (1994) On the runoff formation in the small pre-alpine research basin Rietholzbach FRIEND: flow regimes from International Experimental and Network Data (Proceedings of the Braunschweig Conference, October 1993) IAHS Publ. no. 221, IAHS, Wall SI Seneviratne (1238_CR51) 2012; 48 RW Healy (1238_CR30) 2010 I Rodriguez-Iturbe (1238_CR49) 1999; 455 D Penna (1238_CR45) 2011; 15 W Balderer (1238_CR5) 1983; 34 HE Dahlke (1238_CR16) 2012; 138 RJ Nathan (1238_CR44) 1990; 26 1238_CR23 SK Carey (1238_CR14) 2010; 24 G Ali (1238_CR2) 2013; 27 SL Dingman (1238_CR17) 2002 K Beven (1238_CR9) 1979; 24 W Brutsaert (1238_CR13) 2005 S Bachmair (1238_CR3) 2011 T Vitvar (1238_CR56) 1997; 12 WJ Gburek (1238_CR22) 2002; 57 SW Lyon (1238_CR36) 2006; 42 E Zehe (1238_CR60) 2009; 13 JD Woodbury (1238_CR59) 2014; 50 H Bouwer (1238_CR12) 1976; 12 1238_CR35 1238_CR33 HE Dahlke (1238_CR15) 2009; 2 CB Graham (1238_CR26) 2010; 393 1238_CR39 NB Basu (1238_CR7) 2010; 46 K Beven (1238_CR8) 2001; 5 K Posavec (1238_CR47) 2010; 48 T Doppler (1238_CR18) 2012; 16 1238_CR31 T Ewen (1238_CR20) 2011; 62 H Mittelbach (1238_CR42) 2012; 430 JW Kirchner (1238_CR34) 2003; 17 T Dunne (1238_CR19) 1970; 6 M Sivapalan (1238_CR52) 2003; 17 AL James (1238_CR32) 2009; 377 G Botter (1238_CR11) 2007; 43 S Gharari (1238_CR24) 2011; 15 J Gurtz (1238_CR29) 2003; 17 1238_CR41 A Rinaldo (1238_CR48) 2011; 47 D Tetzlaff (1238_CR53) 2007; 21 GS McGrath (1238_CR40) 2007; 11 VK Gupta (1238_CR27) 1980; 16 W Balderer (1238_CR6) 1984; 36 J Gurtz (1238_CR28) 2003; 51 MLV Martina (1238_CR37) 2006; 42 BL McGlynn (1238_CR38) 2003; 39 HE Gall (1238_CR21) 2013; 28 DN Moriasi (1238_CR43) 2007; 50 1238_CR1 1238_CR58 SE Thompson (1238_CR55) 2011; 47 JR Philip (1238_CR46) 1957; 84 1238_CR4 1238_CR50 1238_CR10 M Ghasemizade (1238_CR25) 2013; 69 AJ Teuling (1238_CR54) 2010; 46 D Viviroli (1238_CR57) 2003; 23
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SubjectTerms	Aquatic Pollution aquifers Base flow Catchment areas Catchments Discharge Earth and Environmental Science Earth Sciences Environmental impact Field study Geology Geophysics/Geodesy Groundwater Groundwater discharge Groundwater flow Groundwater recharge Headwaters Hydrogeology hydrograph Hydrographs Hydrology Hydrology/Water Resources Landscape Landscape ecology Landscapes Mathematical models Mountains prediction rain riparian areas Riparian land River discharge River flow rivers Stream discharge Stream flow subsurface flow Surface runoff Switzerland time series analysis Waste Water Technology Water Management Water Pollution Control Water Quality/Water Pollution watersheds
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Title	The impact of hillslope groundwater dynamics and landscape functioning in event-flow generation: a field study in the Rietholzbach catchment, Switzerland
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