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  • About
  • The Global ETD Search service is a free service for researchers to find electronic theses and dissertations. This service is provided by the Networked Digital Library of Theses and Dissertations.
    Our metadata is collected from universities around the world. If you manage a university/consortium/country archive and want to be added, details can be found on the NDLTD website.
81

Gravimétrie et surveillance sismique pour la modélisation hydrologique en milieu karstique : application au bassin du Durzon (Larzac, France) / Gravimetry and ambient seismic noise monitoring for hydrological modeling : application to the Durzon karstic basin (Larzac, France)

Fores, Benjamin 24 November 2016 (has links)
Les aquifères karstiques représentent des ressources en eau essentielles dans de nombreuses régions du monde comme le bassin Méditerranéen. Cependant, de par les processus complexes de karstification, ces aquifères sont hétérogènes à de nombreuses échelles et vulnérables. Dans cette thèse, nous étudions le potentiel de la gravimétrie et du bruit sismique ambiant pour la modélisation hydrologique en milieu karstique.Le site dolomitique de l’observatoire « GEK », sur le bassin du Durzon dans le Larzac, est le site d’étude privilégié de ces travaux. Dans l’observatoire, un gravimètre supraconducteur dédié à l’hydrologie mesure depuis 2011 les variations de gravité en continu et à une très haute précision, pour la première fois sur un karst. Des modèles hydrologiques conceptuels ont été réalisés à partir de cette surveillance gravimétrique et ont permis de poser les bases de modèles physiques d’écoulements 1-D. En effet la gravimétrie, intégratrice, permet 1) de considérer l’épikarst localement hétérogène comme un milieu tabulaire équivalent et 2) de définir les types de transfert à l’œuvre sur le site. En particulier, l’absence de transfert rapide dans l’épikarst a été quantifiée avec précision pour la première fois à l’échelle du terrain (~100m). A l’aide de données météorologiques locales, un bilan de masse précis a permis de définir le flux en limite inférieure du modèle à 1 mm.jour-1. Ce flux s’est montré représentatif du débit de basses-eaux de la source drainant l’ensemble du bassin. Ce résultat suppose une homogénéité de l’épikarst dolomitique quasiment à l’échelle du bassin. Les paramètres des modèles physiques ont ensuite pu être calibrés à l’aide d’un an d’intercorrélation du bruit sismique ambiant entre deux stations. Les variations de vitesses de phase obtenues entre 6 et 8Hz nous ont servi de « chronomètre » pour suivre l’infiltration entre 30 et 60m de profondeur. La surveillance passive des variations de vitesses sismiques par intercorrélation du bruit sismique ambiant montre ainsi un fort potentiel pour l’étude des zones critiques profondes et complexes à l’échelle du terrain et peut combler la lacune instrumentale qui existe actuellement en hydrologie.Des campagnes répétées de mesures avec un gravimètre portable à ressort ont également mis en évidence le fonctionnement différent de deux épikarsts et leur variabilité à l’échelle de la centaine de mètres. Des mesures mensuelles autour de l’observatoire ont mis en évidence l’homogénéité spatiale de cet épikarst dolomitique : toutes les stations ont les mêmes variations temporelles de stock d’eau. Au contraire, des mesures saisonnières en surface et en profondeur le long de la galerie souterraine calcaire de l’abîme de Saint-Ferréol ont montré une variabilité spatiale forte du stockage ainsi que du transfert rapide. La lithologie de l’épikarst est donc suspectée de jouer un rôle dans sa capacité de stockage. Lors de ces campagnes, la faiblesse du signal recherché a nécessité une méthodologie précautionneuse et un effet de température sur les mesures des gravimètres relatifs à ressort a été observé sur le terrain et quantifié en laboratoire. / Karstic aquifers represent the most important fresh water reservoirs in many regions of the world like the Mediterranean Basin. However, because of complex processes of karstification, those aquifers are highly heterogeneous at all spatial scales and vulnerable to contamination. In this dissertation, we studied the potential of gravimetry and ambient seismic noise for hydrological modeling in karstic areas.The dolomitic area surrounding the “GEK” observatory in the Durzon catchment on the Larzac plateau, in France, is the preferred site for these studies. Inside the observatory, a superconducting gravimeter dedicated to hydrology has continuously measured gravity changes since 2011 with high precision, undertaken for the first time on a karst. From this gravity monitoring, we made conceptual hydrological models which laid the foundation of 1-D flow physical models. Indeed, gravimetry is an integrative hydro-geophysical method which allows 1) to consider the epikarst, locally heterogeneous as an equivalent tabular medium and 2) to define the types of transfer (fast & slow) occurring at the site. Especially, the lack of fast transfer through the GEK epikarst was precisely quantified for the first time at the field scale (~100m). Gravity-driven water mass balance with local meteorological data (evapotranspiration from a flux tower and precipitation) allowed setting the bottom outlet of the model to 1 mm.day-1. This flow has proved to be representative of the low-flow discharge at the only spring which represents all groundwater outflows from the catchment. This result supposes the homogeneity of the dolomitic epikarst almost at the basin scale. Model parameters were next calibrated using one year of ambient seismic noise monitored at two stations. Phase velocity changes obtained by cross-correlating the noise between 6 and 8 Hz were used as a ”timer” to follow the water infiltration between a depth of 30 and 60 meters. Thus, monitoring seismic velocity changes using ambient seismic noise demonstrates great potential for the study of deep and complex critical zones and could fill the instrumental gap currently existing in hydrology.Time-lapse gravity measurements with a spring-based portable gravimeter have also demonstrated the different behavior of two epikarsts and their variability at the scale of a few hundred meters. Monthly measurements around the observatory revealed the spatial homogeneity of this dolomitic epikarst: all the stations showed the same water storage changes. On the contrary, seasonal surface to depth gravity measurements along the underground passage of the Saint-Ferréol sinkhole, in limestone, have shown fast transfer and strong spatial variability of water storage. Lithology is then expected to play a part in the epikarst capacity to retain water. The precision needed to measure the weak hydrological induced signals during those surveys required robust methodology and an ambient temperature effect on measurements with spring-based gravimeter was observed in the field and quantified in the laboratory.
82

Hydrological modeling as a tool for sustainable water resources management: a case study of the Awash River Basin

Tessema, Selome M. January 2011 (has links)
The growing pressure on the world‘s fresh water resources is enforced by population growth that leads to conflicts between demands for different purposes. A main concern on water use is the conflict between the environment and other purposes like hydropower, irrigation for agriculture and domestic and industry water supply, where total flows are diverted without releasing water for ecological conservation. As a consequence, some of the common problems related to water faced by many countries are shortage, quality deterioration and flood impacts. Hence, utilization of integrated water resources management in a single system, which is built up by river basin, is an optimum way to handle the question of water. However, in many areas, when planning for balancing water demands major gaps exist on baseline knowledge of water resources. In order to bridge these gaps, hydro-logical models are among the available tools used to acquire adequate understanding of the characteristics of the river basin. Apart from forecasting and predicting the quantity and quality of water for decision makers, some models could also help in predicting the impacts of natural and anthropogenic changes on water resources and also in quantifying the spatial and temporal availability of the resources. However, main challenges lie in choosing and utilizing these models for a specific basin and managerial plan. In this study, an analysis of the different types of models and application of a selected model to characterize the Awash River basin, located in Ethiopia, is presented. The results from the modeling procedure and the performance of the model are discussed. The different possible sources of uncertainties in the modeling process are also discussed. The results indicate dissimilar predictions in using different methods; hence proper care must be taken in selecting and employing available methods for a specific watershed prior to presenting the results to decision makers. / QC 20110516
83

Modélisation hydrologique du bassin versant de l'oued Rheraya et sa contribution à la recharge de la nappe du Haouz (bassin du Tensift, Maroc) / Hydrological modeling of the Rheraya watershed and its contribution to the groundwater recharge of the Haouz aquifer (Tensift basin, Morocco)

Hajhouji, Youssef 20 October 2018 (has links)
La recharge de l'eau souterraine est un paramètre encore peu connu du bilan hydrologique. La connaissance des processus et l'estimation précise de la recharge de l'eau souterraine est une condition préalable à une gestion efficace et durable des eaux souterraines dans les régions arides et semi-arides. En plus la recharge de l'eau souterraine est considérée comme le paramètre le plus direct avec lequel le changement climatique peut affecter les ressources renouvelables des aquifères. Les présents travaux de thèse s'intéressent à la recharge de l'aquifère alluvial de la plaine du Haouz par les crues de l'oued Rheraya (rivière intermittente), qui descend des montagnes du Haut-Atlas et traverse la plaine du Haouz du sud vers le nord. Ces travaux ont deux objectifs principaux (i) d'abord simuler le régime hydrologique de l'oued Rheraya dont les crues sont à l'origine de la recharge de l'eau souterraine, et ensuite (ii) aborder la quantification de la recharge de l'eau souterraine du Haouz par ces crues dans la zone du piémont atlasique. La modélisation des débits de l'oued Rheraya dans le Haut-Atlas marocain (225 km², altitudes comprises entre 1030 m et 4165 m) est réalisée en prenant en compte la composante nivale. Pour cela, le modèle conceptuel global GR4J est appliqué sur la période 1989-2009 en y adjoignant le module CemaNeige qui simule la dynamique de la composante neigeuse de manière semi- distribuée. La fraction enneigée simulée se révèle corrélée avec celle extraite du produit neige MODIS durant la période 2000-2009 (R2 = 0,64). De plus, l'équivalent en eau de la neige simulé est cohérent avec celui mesuré par la station automatique au sommet de l'Oukaimeden durant la période 2004-2006 (R2 = 0,81). Enfin, nous obtenons une simulation des débits qui reproduit bien la très forte variabilité saisonnière et interannuelle. En conclusion, le régime hydrologique de l'oued Rheraya est pluvio-nival avec une distribution unimodale des débits dont le maximum en avril coïncide avec la fonte des neiges. L'étude de la recharge de l'eau souterraine est effectuée à travers l'analyse du suivi des fluctuations de l'eau souterraine sous le lit de l'oued Rheraya sur deux cycles hydrologiques 2014-2015 et 2015-2016.[...] / Groundwater recharge is a little known parameter in the water balance. Knowledge of processes and accurate estimation of groundwater recharge is a prerequisite for effective and sustainable management of groundwater resources. In addition, groundwater recharge is considered the most direct parameter by which climate change affects the renewable groundwater resources. The present PhD thesis focuses on the recharge of the alluvial aquifer of the Haouz plain by the floods of the Rheraya wadi (intermittent river), which descends from the High-Atlas Mountains and crosses the southern plain towards the North. This work has two main objectives: (i) simulating the hydrological regime of the Rheraya River whose floods are at the origin of the groundwater recharge, and (ii) Quantifying the groundwater recharge by the floods of the Rheraya in the zone of the High-Atlas piedmont. The runoff modeling of the Rheraya wadi in the High-Atlas (225 km², elevations ranging between 1030 and 4165 m.a.s.l.) takes into account the snow component. For this purpose, the GR4J conceptual and global model was applied over the period 1989- 2009, coupled with the CemaNeige module for semi-distributed snow dynamics. The daily snow coverage simulated by CemaNeige is in good agreement with that extracted from the MODIS snow product in the period 2000-2009 (R² = 0,64). In addition, the simulated daily snow water equivalent is consistent with that measured at the weather station of Oukaimeden (2004-2006, R² = 0,81). Finally, the runoff simulation reproduces quite well the strong seasonal and inter-annual variability. In conclusion, the hydrological regime of the Rheraya wadi is pluvio-nival with an unimodal distribution whose maximum in April is linked with snowmelt. The study of groundwater recharge is carried out through the analysis of the monitoring of groundwater fluctuations in the streambed of the Rheraya wadi, over two hydrological cycles 2014-2015 and 2015-2016.[...]
84

Estimation spatialisée de l'évapotranspiration réelle et des volumes d'irrigation à l'aide de modèles de bilans hydrique et énergétique forcés par des données de la télédétection optique (VIS/PIR/IRT) / Spatial estimation of actual evapotranspiration and irrigation volumes using water and energy balance models forced by optical remote sensing data (VIS/NIR/TIR)

Saadi, Sameh 16 February 2018 (has links)
La gestion efficace de l'eau dans les régions arides et semi-arides est un problème majeur, principalement dans les zones irriguées. La conception d'outils fournissant des estimations régionales des composantes du bilan hydrique peut aider à la gestion durable de la ressource en eau dans ces régions. La télédétection multi-capteurs a démontré un très fort potentiel pour le suivi des ressources hydriques agricoles à différentes échelles. Cette thèse vise à développer des techniques et des méthodes efficaces pour estimer les variables hydrologiques (évapotranspiration et les volumes d'irrigation) afin d'évaluer, dans l'espace (résolutions "métrique" et "kilométrique"), les besoins en eau des cultures du couvert végétal de la plaine de Kairouan (Tunisie centrale) ainsi que les volumes d'irrigation extraits de son aquifère surexploité. L'approche adoptée combine l'expérimentation, la modélisation et l'utilisation de données de télédétection multi-capteurs / multi-résolutions. Les deux types d'outils utilisés sont le modèle de bilan hydrique SAMIR et le modèle de bilan d'énergie SPARSE. Les variables estimées par SAMIR et SPARSE sont évaluées à l'aide des mesures terrain (mesures d'un scintillomètre XLAS) et des enquêtes de terrain (volumes d'irrigation observés). Les volumes d'irrigation saisonniers estimés par SAMIR sont acceptables, même si les résultats à des échelles de temps plus fines (mensuelles) doivent être améliorés. Ainsi, les paramètres de SAMIR, en particulier les paramètres non calibrés, sont revisités afin d'améliorer les performances de simulation de l'ET et des volumes d'irrigation. Les estimations des flux de chaleur sensible et latente par SPARSE sont en étroit accord avec celles obtenues à partir du XLAS. Cependant, l'extrapolation de l'évapotranspiration instantanée au pas de temps journalier est moins évidente. / In arid and semi-arid regions, efficient agricultural water management is a major issue, mainly in irrigated areas. The design of tools that provide an estimate of water balance components at the regional scale may help sustainable management of limited water resources in the water scarce regions. Remotely sensed Earth observation has become a major research field for agricultural water resources management. The main objective of this thesis is to develop and test efficient techniques and methods to estimate hydrological variables (Evapotranspiration (ET) and irrigation volumes) in order to assess, at "metric" and "kilometric" resolution , the crop water requirements and the extracted irrigation volumes in the Kairouan plain (central Tunisia). The adopted approach combines field experimentation, modeling and the use of multi-sensor / multi-resolution remote sensing data. Two modeling tools are used: the soil water balance model SAMIR and the energy balance model, SPARSE. SAMIR and SPARSE estimates are assessed using field measurements (Scintillometer XLAS measurements) and field surveys (observed irrigation volumes). The seasonal irrigation volumes estimated by the SAMIR model are acceptable, even though results at finer timescales (monthly and below) needed to be improved. Hence, the SAMIR model parameters, especially the uncalibrated ones are revisited in order to improve the results. SPARSE estimates of sensible and latent heat ?uxes are in close agreement with those obtained from the XLAS. However, the extrapolation from instantaneous to daily ET is less obvious.
85

Análisis del impacto del crecimiento de las megaciudades sobre el ciclo hidrológico bajo escenarios de cambio climático. Aplicación a la cuenca del río Bogotá (Colombia).

Romero Hernández, Claudia Patricia 02 January 2023 (has links)
[ES] Actualmente, el 54% de la población mundial vive en ciudades y se espera que en 2050 este porcentaje aumente al 68% (UNDESA, 2019). Una parte importante de esta población urbana se concentra en megaciudades, definidas como áreas urba-nas con más de 10 millones de habitantes. En América Latina, las principales megaciudades son Sao Paulo y Ciudad de México, con más de 20 millones de habitantes en cada una. Buenos Aires, Río de Janeiro, Lima y Bogotá son mega-ciudades aún en desarrollo (Cepal, 2013). La presente tesis doctoral tiene como objetivo identificar y analizar los impactos que la dinámica de crecimiento urbano de una megaciudad induce sobre el com-portamiento de las componentes del ciclo hidrológico. La investigación desarro-llada incorpora el efecto del cambio climático de forma conjunta con el efecto del cambio de uso de suelo urbano. Para ello, se ha planteado una metodología de agregación de parámetros hidrológicos en superficies urbanas que se ha aplicado a la megaciudad de Bogotá, utilizando el modelo hidrológico TETIS y el modelo de cambios de uso de suelo LCM, bajo los escenarios oficiales de cambio climático vigentes en Colombia. Los resultados obtenidos muestran que el análisis conjunto de cambio de uso de suelo y cambio climático proporciona herramientas valiosas para comprender el comportamiento hidrológico de la cuenca en la que se sitúan las megaciudades y predecir su evolución futura. En el caso de la megaciudad de Bogotá se ha obser-vado que el mayor efecto en las componentes del ciclo hidrológico se produce por el cambio de usos de suelo, el cual se ve incrementado por las acciones inducidas por el cambio climático. La utilización de modelos numéricos que consideren todos estos aspectos es de especial relevancia a la hora de definir los planes, políti-cas y programas de desarrollo en entornos densamente urbanizados. / [CA] Actualment, el 54% de la població mundial viu a ciutats i s'espera que el 2050 aquest percentatge augmenti al 68% (UNDESA, 2019). Una part important d'a-questa població urbana es concentra en megaciutats, definides com a àrees urba-nes amb més de 10 milions d'habitants. A Amèrica Llatina, les principals mega-ciutats són Sao Paulo i Ciutat de Mèxic, amb més de 20 milions d'habitants a cadascuna. Buenos Aires, Rio de Janeiro, Lima i Bogotá són megaciutats encara en desenvolupament (Cepal, 2013). Aquesta tesi doctoral té com a objectiu identificar i analitzar els impactes que la dinàmica de creixement urbà d'una megaciutat indueix sobre el comportament dels components del cicle hidrològic. La investigació desenvolupada incorpora l'efecte del canvi climàtic de forma conjunta amb l'efecte del canvi d'ús de sòl urbà. Per això, s'ha plantejat una metodologia d'agregació de paràmetres hidrolò-gics en superfícies urbanes que s'ha aplicat a la megaciutat de Bogotà, utilitzant el model hidrològic TETIS i el model de canvis d'ús de sòl LCM, sota els escenaris oficials de canvi climàtic vigents a Colòmbia. Els resultats obtinguts mostren que l'anàlisi conjunta de canvi d'ús de sòl i canvi climàtic proporciona eines valuoses per comprendre el comportament hidrològic de la conca on se situen les megaciutats i predir-ne l'evolució futura. En el cas de la megaciutat de Bogotà s'ha observat que l'efecte més gran en les components del cicle hidrològic es produeix pel canvi d'usos de sòl, el qual es veu incrementat per les accions induïdes pel canvi climàtic. La utilització de models numèrics que considerin tots aquests aspectes és especialment rellevant a l'hora de definir els plans, polítiques i programes de desenvolupament en entorns densament urbanit-zats / [EN] Currently 54% of the world population lives in cities and it is expected that by 2050 this percentage will increase to 68% (UNDESA, 2019). An important part of this urban population is concentrated in megacities, defined as urban areas with more than 10 million inhabitants. In Latin America, the main megacities are Sao Paulo and Mexico City, with more than 20 million inhabitants. Buenos Aires, Rio de Janeiro, Lima and Bogotá are megacities still in development (Cepal, 2013). This doctoral thesis aims to identify and analyse the impacts that the dynamics of urban growth of a megacity induce on the behaviour of of the hydrological cycle components. The research carried out incorporates the effect of climate change together with the effect of urban land use change. To do this, a methodology for aggregating hydrological parameters in urban areas has been proposed. This methodology has been applied to the megacity of Bogotá, using the TETIS hydro-logical model and the LCM land use change model, under the official climate change scenarios in force in Colombia. Results obtained show that the joint analysis of land use change and climate change provides valuable tools to understand the hydrological behaviour of the basin in which the megacities are located and predict their future evolution. In the case of the megacity of Bogotá, it has been observed that the greatest effect on the components of the hydrological cycle is produced by the land use change, which is increased by the actions induced by climate change. The use of numeri-cal models that consider all these aspects is of special relevance when defining development plans, policies and programs in densely urbanized environments. / Romero Hernández, CP. (2022). Análisis del impacto del crecimiento de las megaciudades sobre el ciclo hidrológico bajo escenarios de cambio climático. Aplicación a la cuenca del río Bogotá (Colombia) [Tesis doctoral]. Universitat Politècnica de València. https://doi.org/10.4995/Thesis/10251/191025
86

Flood inundation mapping of the Catalpa Creek Watershed

Poudel, Subodh 08 December 2023 (has links) (PDF)
This study addresses flood risk assessment in the Catalpa Creek watershed, located in northeast Mississippi, USA. Employing the Hydrological Modeling System (HEC-HMS) and the River Analysis System (HEC-RAS), integrated models were developed and calibrated, to predict flood behavior within the watershed. The study conducted flood frequency analyses for return periods ranging from 2 to 100 years and generated flood inundation maps, pinpointing flood-prone areas. Mitigation measures for flood risk management were recommended. The results underscore the effectiveness of the integrated modeling approach for simulating and understanding the complex dynamics of flood events. The research identified critical flood-prone zones, emphasizing the importance of proactive flood risk management. The calibrated hydrological model serves as a valuable tool for stormwater management, water resource planning, and watershed assessment. The study provides insights into flood risk in the Catalpa Creek watershed, offering valuable guidance to regional decision-makers. This study lays the foundation for future investigations in floodplain encroachment, sediment transport, stream restoration, and flood inundation hazard mapping.
87

Flood mitigation at catchment scale: assessing the effectiveness of constructed wetlands / Översvämningshantering utifrån ett avrinningsområdesperspektiv: utvärdering av effektiviteten av anlagda våtmarker

Ekström, Elin January 2023 (has links)
Considering the potential for natural wetlands to store and retain water in the landscape,restored and constructed wetlands are increasingly implemented as Nature‐BasedSolutions (NBS) to mitigate downstream flooding. However, there is a frequent lack ofknowledge of the performance of NBS, and particularly wetlands, and how to best selectperformance indicators to measure their effectiveness. The aim of this study was to assessthe flood regulation services of multiple constructed wetlands at catchment scale. TheSWAT+ model was used to assess the impacts of 35 constructed wetlands in the 193 km2Råån catchment in southwest Sweden. The assessment was based on a paired simulationscenario, with and without wetlands, and performance was evaluated based on impacts onthe downstream river hydrograph (peak flow rate, time-to-peak, recession curve shape,daily streamflow average) as well as event-based (daily average streamflow for differentprecipitation ranges), descriptive (average wetland storage capacity), consequential(overbank flooding) and social (social acceptance) indicators. The results implied that theflow regulating capability of the modeled wetlands was directly related to their outflowmechanisms. The wetlands had an average storage capacity of 0.38 m3 per m2 area butbecause the wetlands seemed to frequently exceed their maximum storage capacity duringhigh flow events, and the excess water was immediately spilled downstream, the wetlandsprovided limited flood regulation services. There were no visible impacts on thehydrograph-related indicators and the daily streamflow average was reduced by anegligible 0.02%. Furthermore, there were no significant differences in wetlandperformance between small and heavy rainfall events and the model output showed nosigns of overbank flooding for either wetland scenario. In terms of social acceptance, recentwetland projects in Råån catchment seem to have been well-received by farmers andlandowners in the area. However, lack of wetland-specific data, such as volume and dailyinflow and outflow data, as well as other model uncertainties, motivated a low confidencegrade for the indicators. In fact, if indicator values are to be useful tools in the futureintegration of wetlands as nature-based solutions, in-situ monitoring data of wetland waterbalance components are required. To support future policies and decision-making, adaptedtools and further research are needed to assess the impact of NBS on upstream-downstream processes. / Naturliga våtmarkers förmåga att hålla kvar och lagra vatten i landskapet gör attrestaurerade och anlagda våtmarker alltmer implementeras som naturbaserade lösningarför att mildra översvämningar i nedströms belägna områden. Det råder dock brist påkunskap om hur effektiva naturbaserade lösningar är och hur nyckelindikatorer bäst kanväljas för att mäta hur väl dessa system fungerar. Syftet med denna studie var att utvärderaanlagda våtmarkers förmåga att mildra översvämningar i ett avrinningsområde. SWAT+modellen användes för att bedöma påverkan av 35 anlagda våtmarker i Råånsavrinningsområde (193 km2) utanför Helsingborg. Bedömningen baserades på ettsimuleringspar, med och utan våtmarker, och effektiviteten utvärderades baserat påhydrografens egenskaper (flödestopp, stegringsfasen, recessionsfasen, daglig medel-vattenföring) samt med en nederbördsbaserad (daglig medelvattenföring för olikanederbördsintervall), beskrivande (genomsnittlig lagringskapacitet), konsekvensbaserad(översvämmad mark) och social (social acceptans) indikator. Resultatet antydde att denflödesreglerande förmågan hos de modellerade våtmarkerna var direkt kopplad till derasutflödesmekanismer. Våtmarkerna hade en genomsnittlig lagringskapacitet på 0.38 m3 perm2 yta men eftersom de ofta verkade överskrida sina maximala lagringskapaciteter underhögflöden, och överskottsvattnet omedelbart släpptes igenom nedströms, tillhandahöllvåtmarkerna en mycket begränsad flödesdämpande funktion. Det fanns inga synligaeffekter på de hydrografrelaterade indikatorerna och den dagliga medelvattenföringenminskade med försumbara 0.02%. Dessutom sågs inga signifikanta skillnader mellan småoch kraftiga nederbördshändelser och modellen visade inga tecken på översvämmad markför något av våtmarksscenarierna. Vad gäller social acceptans tycks de senastevåtmarksprojekten i Rååns avrinningsområde ha tagits emot väl av lantbrukare ochmarkägare i området. Bristen på våtmarksspecifika data, såsom volym och dagliga in- ochutflödesdata, samt andra modellosäkerheter medförde dock ett lågt förtroende förindikatorerna. Om indikatorvärden ska vara användbara verktyg i den framtida integ-reringen av våtmarker krävs uppmätta data över våtmarkernas vattenbalanskomponenter.För att stödja framtida beslutsfattande behövs även anpassade verktyg och ytterligareforskning för att bedöma påverkan av naturbaserade lösningar på uppströms-nedströmsprocesser.
88

Utilisation du concept de connectivité en hydrologie : définitions, approches expérimentales et éléments de modélisation

Ali, Geneviève 09 1900 (has links)
Alors que certains mécanismes pourtant jugés cruciaux pour la transformation de la pluie en débit restent peu ou mal compris, le concept de connectivité hydrologique a récemment été proposé pour expliquer pourquoi certains processus sont déclenchés de manière épisodique en fonction des caractéristiques des événements de pluie et de la teneur en eau des sols avant l’événement. L’adoption de ce nouveau concept en hydrologie reste cependant difficile puisqu’il n’y a pas de consensus sur la définition de la connectivité, sa mesure, son intégration dans les modèles hydrologiques et son comportement lors des transferts d’échelles spatiales et temporelles. Le but de ce travail doctoral est donc de préciser la définition, la mesure, l’agrégation et la prédiction des processus liés à la connectivité hydrologique en s’attardant aux questions suivantes : 1) Quel cadre méthodologique adopter pour une étude sur la connectivité hydrologique ?, 2) Comment évaluer le degré de connectivité hydrologique des bassins versants à partir de données de terrain ?, et 3) Dans quelle mesure nos connaissances sur la connectivité hydrologique doivent-elles conduire à la modification des postulats de modélisation hydrologique ? Trois approches d’étude sont différenciées, soit i) une approche de type « boite noire », basée uniquement sur l’exploitation des données de pluie et de débits sans examiner le fonctionnement interne du bassin versant ; ii) une approche de type « boite grise » reposant sur l’étude de données géochimiques ponctuelles illustrant la dynamique interne du bassin versant ; et iii) une approche de type « boite blanche » axée sur l’analyse de patrons spatiaux exhaustifs de la topographie de surface, la topographie de subsurface et l’humidité du sol. Ces trois approches sont ensuite validées expérimentalement dans le bassin versant de l’Hermine (Basses Laurentides, Québec). Quatre types de réponses hydrologiques sont distingués en fonction de leur magnitude et de leur synchronisme, sachant que leur présence relative dépend des conditions antécédentes. Les forts débits enregistrés à l’exutoire du bassin versant sont associés à une contribution accrue de certaines sources de ruissellement, ce qui témoigne d’un lien hydraulique accru et donc d’un fort degré de connectivité hydrologique entre les sources concernées et le cours d’eau. Les aires saturées couvrant des superficies supérieures à 0,85 ha sont jugées critiques pour la genèse de forts débits de crue. La preuve est aussi faite que les propriétés statistiques des patrons d’humidité du sol en milieu forestier tempéré humide sont nettement différentes de celles observées en milieu de prairie tempéré sec, d’où la nécessité d’utiliser des méthodes de calcul différentes pour dériver des métriques spatiales de connectivité dans les deux types de milieux. Enfin, la double existence de sources contributives « linéaires » et « non linéaires » est mise en évidence à l’Hermine. Ces résultats suggèrent la révision de concepts qui sous-tendent l’élaboration et l’exécution des modèles hydrologiques. L’originalité de cette thèse est le fait même de son sujet. En effet, les objectifs de recherche poursuivis sont conformes à la théorie hydrologique renouvelée qui prône l’arrêt des études de particularismes de petite échelle au profit de l’examen des propriétés émergentes des bassins versants telles que la connectivité hydrologique. La contribution majeure de cette thèse consiste ainsi en la proposition d’une définition unifiée de la connectivité, d’un cadre méthodologique, d’approches de mesure sur le terrain, d’outils techniques et de pistes de solution pour la modélisation des systèmes hydrologiques. / As core processes of the transformation of rainfall into runoff are not fully understood, the concept of hydrologic connectivity has been put forward to explain why some processes occur episodically, in a very discrete short-lived manner, as a response to intermittent atmospheric water input, storm characteristics and soil moisture storage. Even though emerging as a very powerful tool for explaining the growing numbers of nonlinear hydrologic behaviours documented around the world, the hydrologic connectivity concept raises major issues for future research in catchment hydrology in terms of its definition, its measure, its integration into hydrological models and its scaling in the space and the time domains. The aim of this doctoral work is to precise the definition, the measure, the scaling and the prediction of processes underlying hydrologic connectivity while focusing on the following research questions: (1) What methodological framework should guide investigations of hydrologic connectivity?, (2) How to assess hydrologic connectivity from field data?, and (3) To what extent can the ongoing knowledge acquisition on hydrologic connectivity be used to improve success with hydrological modeling? Three study approaches are discriminated, namely: (i) a black box approach that only relies on rainfall and runoff data without examining the internal catchment behaviour; (ii) a grey box approach based on punctual geochemical data illustrating the catchment internal state; and (iii) a white box approach involving exhaustive spatial patterns of surface and subsurface topographic variables and soil moisture. These three approaches are then tested against field data from the Hermine catchment (Lower Laurentians, Quebec). It is possible to classify the Hermine catchment hydrological responses with regards to their magnitude and their timing, the switching from one response type to another depending on antecedent conditions. It is revealed that high discharge values monitored at the catchment outlet are produced by increased contributions from specific runoff sources, thus hinting towards a reinforced hydraulic linkage and an enhanced degree of connectivity between runoff sources and the stream channel. It is established that saturated areas whose spatial extent exceeds 0.85 ha are critical for high runoff generation. Soil moisture spatial patterns in temperate humid forested catchments are shown to have statistical properties that are very different from those encountered in temperate rangelands; hence the necessity of using different spatial connectivity metrics in these contrasted environments. The co-existence of “linear” and “nonlinear” contributing sources is also illustrated in the Hermine catchment. These results suggest that some concepts should be revised for hydrological modeling purposes. The originality of the present thesis is mainly inherited from its prime focus. The pursued research objectives are in accordance with the future trend in catchment hydrology, especially as hydrologists are urged to move from site-specific experiments and results to more easily generalizable concepts that favour the study of emergent catchment properties such as connectivity. Thus, the major contribution of this thesis is the proposal of a unified definition of connectivity, a comprehensive methodological framework, technical tools and operational ideas for the better performance of hydrological models.
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Análise comparativa do efeito da distribuição espaço-tempo em eventos pluviométricos intensos na formação de vazões em bacias urbanas. / Comparative analysis of the effect of space-time distribution of heavy rainfall events in the formation of flows in urban catchments.

Girnius, Lígia de Souza 18 May 2016 (has links)
Esta pesquisa tem como finalidade discutir os impactos da variabilidade espacial e temporal de precipitações intensas nas vazões de cursos d\'água em bacias urbanizadas mediante a análise de dados históricos da pluviometria obtidos durante eventos críticos. A bacia hidrográfica do rio Tietê, em sua porção mais urbanizada, é a área objeto deste estudo. Após uma revisão sobre o tema na literatura específica, foram desenvolvidas chuvas de projeto com os padrões observados e com padrões teóricos, frequentemente utilizados na geração das tormentas sintéticas. O volume total precipitado foi associado ao período de retorno (TR) de 100 anos, a partir da análise estatística de chuvas pontuais e pela aplicação de fatores de redução de área (FRA) observados na área em estudo e de outras regiões, que vêm sendo utilizados em projetos de drenagem, sem qualquer estudo de validação; o intuito foi o de demonstrar a importância da definição de FRA específicos, a fim de evitar superdimensionamentos e otimizar as soluções. As chuvas de projeto foram aplicadas num modelo matemático de transformação chuva-vazão, devidamente calibrado, para obtenção das vazões de projeto resultantes no limite de jusante da bacia hidrográfica, frente aos diferentes padrões de solicitações hidrológicas. Para auxiliar a calibração do modelo estavam disponíveis dados dos postos telemétricos do Sistema de Alerta a Inundações de São Paulo - SAISP, curvas-chave e, para melhor representação dos eventos de precipitação observados, pode-se contar com as imagens do radar de Ponte Nova, em complementação às informações da rede de superfície. A comparação dos resultados obtidos no modelo hidrológico mostrou que os efeitos dos parâmetros variáveis (volume, distribuição espacial e temporal) são expressivos na composição dos hidrogramas de projeto. Dos testes realizados, identificaram-se as situações mais e menos críticas para a bacia, em termos de distribuição espacial e temporal e duração da chuva de projeto, além de estabelecer as diferenças no dimensionamento do sistema de drenagem pela adoção de FRA específico. Concluiu-se que, pela metodologia proposta, é possível chegar a vazões máximas de projeto apenas pela simulação de tormentas sintéticas, com diferenças de 10% a 20% das tormentas observadas maximizadas. Há, no entanto, a necessidade de realização de estudos adicionais, tanto para definição dos valores de FRA específicos, quanto de simulação de quantidade maior de padrões críticos observados, para a aplicação prática das indicações desse estudo com maior confiabilidade. / This research aims to discuss the impact of the spatial and temporal variability of heavy rainfall in the river flows in urbanized catchments by the historical rainfall data analysis obtained during critical events. The Tiete River catchment, in its most urbanized portion, is the subject of study of this research. After a review of the subject in the specific literature, design rainfall was developed along with the observed and theoretical patterns, often used in the generation of synthetic storms. The total volume precipitated was associated with the 100 years return period (RP), from the statistical analysis of point rainfall and for the application of areal reduction factors (ARF) observed in the study area and in other regions, which have been used in drainage projects without any validation study; the intention was to demonstrate the importance of the definition of specific ARF, in order to avoid oversizing and optimizing solutions. The design precipitation was applied on rainfall-runoff mathematical model, properly calibrated, so as to obtain the resulting design flow at the downstream boundary of the catchment, facing the different patterns of hydrological solicitations. In order to assist the calibration of the model, available data has been used from telemetric stations of the Sistema de Alerta a Inundações de São Paulo (São Paulo Flooding Alert System) - SAISP, discharge curves, and for better representation of the observed precipitation events, can be counted on the images taken from the Ponte Nova radar, as a complement to the information from the surface network. The comparison of the results of the hydrological model has shown that the effects of the variable parameters (volume, spatial and temporal distributions) are significant in the composition of the design hydrograph. Out of the performed tests, the most and the least critical situations were identified concerning the catchment in terms of both spatial and temporal distribution as well as the duration of the design storm. Also, the differences in the dimensions of the of the drainage system design were established by the adoption of specific ARF. Thus, it has been concluded, according to the proposed methodology, that it is possible to reach maximum design flow just by simulating synthetic storms, with differences ranging from 10% to 20% of the observed storms maximized. However, there is a need for additional studies, either to set up setting specific values of ARF or to simulate a larger quantity of critical patterns observed, in order to apply the indications of this study with higher reliability.
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Assessment of water security using conceptual, deterministic and stochastic frameworks / Avaliação da segurança hídrica a partir de base conceitual, determinística e estocástica

Rodrigues, Dulce Buchala Bicca 21 November 2014 (has links)
A comprehensive assessment of water security incorporates a range of water-related concepts, since water policy issues to specific technical aspects of hydrological conditions and their interactions with societal needs and ecosystem functioning. This doctoral thesis is organized into three chapters that address such range of water security-related topics, aiming to establish a conceptual baseline and propose deterministic and stochastic accounting frameworks for a river basin water security evaluation. Specific assumptions and research questions are defined in each chapter, and are related to the management of \'Cantareira water supply system\' (located in Southeastern Brazil), focusing on different scales and on its political and hydrological aspects as well. The first chapter acts as a conceptual baseline for water security assessment, by examining general aspects of the Brazilian water policy and water allocation system. This study contrasts Brazilian and American water management systems applied to water transfer projects, discussing experiences from the \'Cantareira system\' and Colorado river basin. A deterministic accounting framework is presented in the second chapter, which is based on management of blue and green water kinds (defined in accordance with hydrological processes and storage types), and demonstrates how a quantitative analysis of provisioning and use (abstraction and consumption) of both water kinds can be conducted. An agricultural basin (291 km²) within the Cantareira water supply system (located upstream of the Cachoeira reservoir) was used to illustrate this approach. The impact of blue and green water use on median water resources conditions is accounted by the scarcity indicator, while the vulnerability indicator considers the probability of low availability of water resources. In the third chapter quantifies and discusses the impacts of uncertainties on water security indicators (proposed in the chapter 2), based on a multi-model and resampling framework, that considers several uncertainty sources including those related to: i) observed streamflow data; ii) hydrological model structure; iii) residual analysis; iv) Environmental Flow Requirement methods; v) the definition of critical conditions for water provision; and vi) the critical demand imposed by human activities. Then, the uncertainty is propagated through different methodological arrangements applied to the same study basin of chapter 2. In brief, the first chapter indicates that both Brazilian and American water management system can potentially contribute to each other. In the second chapter, the Blue/Green water-based accounting framework reveal clear spatial and temporal patterns of water scarcity and vulnerability levels within the basin, thereby improving our understanding of how and where water-related threats to human and aquatic ecosystem security can arise (so called hot-spots). The third chapter provide a general method that can form basis for meaningful support to end-users facing water resource challenges by enabling them to incorporate a viable uncertainty analysis into a robust decision making process. Further investigation are proposed in each research step of this doctoral thesis. / A avaliação da segurança hídrica pode incorporar vários conceitos relacionados à água, desde aspectos da política de recursos hídricos até questões hidrológicas específicas e suas interações com a sociedade e ecossistemas. Esta tese de doutorado busca estabelecer uma base conceitual e propor esquemas metodológicos com base determinística e estocástica para avaliação da segurança hídrica de bacias hidrográficas. Objetivos específicos são definidos em cada capítulo e relacionam-se à gestão do \'Sistema Cantareira de abastecimento de água\' (localizado no Sudeste do Brasil), com foco em diferentes escalas, bem como aspectos políticos e hidrológicos. O primeiro capítulo é apresentado como baseline conceitual, examinando aspectos gerais da política de recursos hídricos e sistemas alocação de água. Este estudo compara sistemas de gestão aplicados a projetos de transposição de água inter/intra-bacias no Brasil e Estados Unidos, discutindo experiências do Sistema Cantareira e da bacia do rio Colorado. O segundo capítulo, por sua vez, propõe e analisa um esquema metodológico determinístico baseado na gestão das águas azul e verde (definidas de acordo com processos hidrológicos e unidades de armazenamento). Este estudo demonstra como uma análise quantitativa da provisão e utilização de ambos os tipos de água pode ser conduzida, propondo indicadores de escassez e vulnerabilidade hídrica. Esta abordagem foi aplicada em uma bacia agrícola (291 km²), localizada a montante do reservatório Cachoeira, que é integrante do Sistema Cantareira. O terceiro capítulo quantifica e analisa os impactos das incertezas sobre os indicadores de segurança hídrica propostos no capítulo 2, utilizando um esquema metodológico estocástico baseado em múltiplos modelos e reamostragem, que incorpora variadas fontes de incerteza, tais como: i) dados observados de vazão; ii) estrutura do modelo hidrológico; iii) análise de resíduos do modelo hidrológico; iv) estimativa de vazão ambiental; v) definição de condições críticas de provisão e vi) demanda hídrica. Em seguida, as incertezas são propagadas através de diferentes arranjos metodológicos aplicados na mesma bacia estudo do capítulo 2. Em conclusão, o primeiro capítulo sugere uma potencial troca de contribuições provenientes de ambos os sistemas de gestão brasileiro e americano. O segundo capítulo revela padrões espaciais e temporais dos resultados dos indicadores de escassez e vulnerabilidade, melhorando assim a compreensão de como e onde ameaças à segurança hídrica podem surgir. Por sua vez, a análise de incertezas desenvolvida no terceiro capítulo é capaz de gerar suporte a gestores de recursos hídricos e processo de tomada de decisões robustas. Recomendações específicas são geradas em cada capítulo da presente tese de doutorado.

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