Thèses sur le sujet « Hydrology|Climate Change »
Créez une référence correcte selon les styles APA, MLA, Chicago, Harvard et plusieurs autres
Consultez les 50 meilleures thèses pour votre recherche sur le sujet « Hydrology|Climate Change ».
À côté de chaque source dans la liste de références il y a un bouton « Ajouter à la bibliographie ». Cliquez sur ce bouton, et nous générerons automatiquement la référence bibliographique pour la source choisie selon votre style de citation préféré : APA, MLA, Harvard, Vancouver, Chicago, etc.
Vous pouvez aussi télécharger le texte intégral de la publication scolaire au format pdf et consulter son résumé en ligne lorsque ces informations sont inclues dans les métadonnées.
Parcourez les thèses sur diverses disciplines et organisez correctement votre bibliographie.
Serrat, Capdevila Aleix. « Climate Change Impacts in Hydrology : Quantification and Societal Adaptation ». Diss., The University of Arizona, 2009. http://hdl.handle.net/10150/194702.
Hackett, William. « Changing Land Use, Climate, and Hydrology in the Winooski ». ScholarWorks @ UVM, 2009. http://scholarworks.uvm.edu/graddis/99.
Larson, Robert, et University of Lethbridge Faculty of Arts and Science. « Modelling climate change impacts on mountain snow hydrology, Montana-Alberta ». Thesis, Lethbridge, Alta. : University of Lethbridge, Faculty of Arts and Science, 2008, 2008. http://hdl.handle.net/10133/669.
xii, 136 leaves : ill. ; 28 cm. --
Parry, Louise Margaret. « Monsoon variability, climate change and impacts on hydrology in the Himalaya ». Thesis, University of Bristol, 2016. https://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.715813.
Booth, Andrew. « Impacts of desiccation cracking and climate change on highway cutting hydrology ». Thesis, Loughborough University, 2014. https://dspace.lboro.ac.uk/2134/14825.
Wherry, Susan Amelia. « Climate Change Effects and Water Vulnerability in the Molalla Pudding River Basin, Oregon, USA ». Portland State University, 2013.
Culbertson, Andreas Mitsutoshi. « Effects of climate change on Maumee River basin hydrology and nutrient runoff ». The Ohio State University, 2015. http://rave.ohiolink.edu/etdc/view?acc_num=osu1437226063.
Siam, Mohamed S. « Assessing impacts of climate change on the hydrology of the Nile River ». Thesis, Massachusetts Institute of Technology, 2016. http://hdl.handle.net/1721.1/104328.
Cataloged from PDF version of thesis.
Includes bibliographical references (pages 179-194).
The human population living in the Nile basin is projected to double by 2050, approaching one billion. The increase in water demand associated with this burgeoning population fuels an ongoing water conflict between the riparian countries. Uncertainty regarding potential future changes in the flow of the Nile River as a result of climate change adds further stress to this critical situation. In this thesis, we investigate the impacts of climate change on hydrology and climate of the Nile basin. In particular, we predict and explain the future changes in interannual variability and long-term mean of the flow in Nile river. We analyze observations on recent change in the flow regime. First, we examine the role of El Niño Southern Oscillation (ENSO) in shaping the interannual variability of the flow in the Nile river. We document an association between variability of ENSO and interannual variability in the flow of the Nile river. We provide a physically-based explanation of this teleconnection. Then, we build on this teleconnection and future predications regarding the frequency of El Niño and La Nina events to project enhancement in future variability of the flow in the Nile river. Second, an improved version of the MIT Regional climate model (MRCM) is used to investigate the future changes in the long-term mean flow in the Nile river. The new version of MRCM includes new parameterizations of large scale cloud and rainfall developed as part of this thesis, which significantly improved the simulation of clouds coverage and radiation at the surface under current climate conditions. The updated version of the model is forced with modified lateral boundary conditions and greenhouse gas concentrations that are assumed to describe future conditions. The impacts on the rainfall over the basin due to local and regional changes in concentration of atmospheric gases are compared to those due to global changes in the humidity and temperature. The numerical simulations using MRCM suggest that increasing humidity at the lateral boundaries due to global processes would enhance the large scale rainfall, particularly during the rainy season. However, air temperature becomes warmer aloft due to the same global processes, which would tend to stabilize the atmosphere and reduce convective rainfall. On the other hand, increasing the concentration of greenhouse gases at local and regional scales would destabilize the vertical profile of air temperature, by increasing the air temperature in the middle and lower atmospheric layers, and hence would enhance convective rainfall. Based on the conclusions of this thesis, the long-term mean and standard deviation of the annual flow in the Nile river are projected to increase for the future period (2000-2100) compared to the past period (1900-2000) by approximately 15% and 50%, respectively. Although the increase in long-term mean of the annual flow should slightly reduce the water stress in the Nile basin, additional water storage capacity in the basin would be needed in order to benefit from the expected additional water in the future.
by Mohamed S. Siam.
Ph. D.
Guilbert, Justin. « The Impacts Of Climate Change On Precipitation And Hydrology In The Northeastern United States ». ScholarWorks @ UVM, 2016. http://scholarworks.uvm.edu/graddis/646.
Stastney, Phil. « Examining the relationships between Holocene climate change, hydrology, and human society in Ireland ». Thesis, University of Reading, 2015. http://centaur.reading.ac.uk/48052/.
Young, Daniel Stuart. « Peatland hydrology, climate change and human societies in Middle and Late Holocene Ireland ». Thesis, University of Reading, 2017. http://centaur.reading.ac.uk/73800/.
Zulkafli, Zed Diyana. « The hydrology of the Peruvian Amazon river and its sensitivity to climate change ». Thesis, Imperial College London, 2014. http://hdl.handle.net/10044/1/23939.
Putman, Annie L. « Tracking the moisture sources of storms at Barrow, Alaska| Seasonal variations and isotopic characteristics ». Thesis, Dartmouth College, 2014. http://pqdtopen.proquest.com/#viewpdf?dispub=1553179.
Enhanced warming and increasingly ice-free Arctic seas affect Arctic precipitation. We investigate increased Arctic precipitation due to declining sea ice by relating variations in moisture sources to stable isotope compositions of precipitation. We develop a novel method for deriving moisture sources using condensation profiles derived from cloud radar measurements to formulate initial heights for air mass back trajectories. This method was used to locate the moisture sources of seventy Barrow, AK storm events between 2009 and 2013. Trajectories were calculated by NOAA's HYSPLIT, using GDAS reanalysis wind fields. We demonstrate that the moisture source migrates with season, from distal in winter to proximal in summer. Moisture source dew point exhibits a semiannual cycle, with summer and winter maxima. The spring minimum reflects the reintroduction of the Arctic source. The autumn dew point minimum reflects pre-ice ocean cooling locally. 36% of isotopic variation is statistically explained by a combination of the moisture source dew point and trajectory cooling. Transport distance and path both influence the best descriptor of isotopic composition. For local events, dew point is the stronger influence on isotopic composition, explaining 21% of variance. For distal events, the effects of trajectory cooling supersedes the moisture source signal. The orographic effect of the Alaskan and Brooks ranges account for the influence of trajectory path on isotopic composition. Local moisture events during transition seasons were slightly enriched relative to distal events. If we measure further isotopic enrichment during future transition seasons, it may reflect increased contributions from the Arctic source and thus precipitation increase. Deuterium excess reflects various combinations of latitude, sea surface temperature and relative humidity. Moisture source dew point significantly but weakly predicts storm-specific d-excess. Similar analyses can be performed across the Arctic if reanalysis data can generate reliable condensation profiles. To evaluate the efficacy of condensation profiles produced by reanalysis data, we compared the condensation profiles derived from cloud radar to those from reanalysis. On average, reanalysis produced condensation profiles with mean cloud height 1.4 times higher than those from cloud radar. The greater elevation bias translated into a more distal, and thus warmer and drier, moisture source.
Rajagopal, Seshadri. « Assessing Water Management Impacts of Climate Change for a Semi-arid Watershed in the Southwestern US ». Diss., The University of Arizona, 2012. http://hdl.handle.net/10150/228475.
Tsarouchi, Georgia-Marina. « Modelling land-use and climate change impacts on hydrology : the Upper Ganges river basin ». Thesis, Imperial College London, 2014. http://hdl.handle.net/10044/1/24809.
Bring, Arvid. « Arctic Climate and Water Change : Information Relevance for Assessment and Adaptation ». Doctoral thesis, Stockholms universitet, Institutionen för naturgeografi och kvartärgeologi (INK), 2013. http://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-86919.
At the time of doctoral defence the following papers were unpublished and had a status as follows: Paper 2: Accepted; Paper 4: Manuscript
SMALL, DAVID LEROY. « A DIAGNOSTIC STUDY OF A POSSIBLE ACCELERATION OF THE HYDROLOGIC CYCLE ». University of Cincinnati / OhioLINK, 2006. http://rave.ohiolink.edu/etdc/view?acc_num=ucin1159210962.
Jung, Gerlinde. « Regional climate change and the impact on hydrology in the Volta Basin of West Africa ». Karlsruhe : Forschungszentrum Karlsruhe, 2006. http://d-nb.info/983081263/34.
Mileham, Lucinda Juliet. « Impact of climate change on the terrestrial hydrology of a humid, equatorial catchment in Uganda ». Thesis, University College London (University of London), 2008. http://discovery.ucl.ac.uk/17227/.
Bounhieng, Vilaysane. « INTEGRATED IMPACT ASSESSMENT OF CLIMATE CHANGE ON HYDROLOGY OF THE XEDONE RIVER BASIN, LAO PDR ». 京都大学 (Kyoto University), 2016. http://hdl.handle.net/2433/204586.
Shang, Linyuan. « Climate Change And Land Use/cover Change Impacts On Watershed Hydrology, Nutrient Dynamics – A Case Study In Missisquoi River Watershed ». ScholarWorks @ UVM, 2019. https://scholarworks.uvm.edu/graddis/1016.
Pryor, John W. « Framework Integrating Climate Model, Hydrology, and Water Footprint to Measure the Impact of Climate Change on Water Scarcity in Lesotho, Africa ». Scholar Commons, 2018. https://scholarcommons.usf.edu/etd/7353.
Hough-Snee, Nathaniel. « Relationships between Riparian Vegetation, Hydrology, Climate and Disturbance across the Western United States ». Thesis, Utah State University, 2016. http://pqdtopen.proquest.com/#viewpdf?dispub=10154374.
Flow regime, the magnitude, duration and timing of streamflow, controls the development of floodplain landforms on which riparian vegetation communities assemble. Streamflow scours and deposits sediment, structures floodplain soil moisture dynamics, and transports propagules. Flow regime interacts with environmental gradients like climate, land-use, and biomass-removing disturbance to shape riparian plant distributions across landscapes. These gradients select for groups of riparian plant species with traits that allow them to establish, grow, and reproduce on floodplains – riparian vegetation guilds. Here I ask, what governs the distributions of groups of similar riparian plant species across landscapes? To answer this question, I identify relationships between riparian vegetation guilds and communities and environmental gradients across the American West. In Chapter One, I discuss guild-based classification in the context of community ecology and streams. In Chapter Two, I identified five woody riparian vegetation guilds across the interior Columbia and upper Missouri River Basins, USA, based on species’ traits and morphological attributes. I modeled guild occurrence across environmental gradients, including climate, disturbance, channel form attributes that reflect hydrology, and relationships between guilds. I found guilds’ distributions were related to hydrology, disturbance, and competitive or complementary interactions (niche partitioning) between co-occurring guilds. In Chapter Three, I examine floodplain riparian vegetation across the American West, identifying how hydrology, climate, and floodplain alteration shape riparian vegetation communities and their guilds. I identified eight distinct plant communities ranging from high elevation mixed conifer forests to gallery cottonwood forests to Tamarisk-dominated novel shrublands. I aggregated woody species into four guilds based on their traits and morphological attributes: an evergreen tree guild, a mesoriparian shrub guild, a mesoriparian tree guild, and a drought and hydrologic disturbance tolerant shrub guild. Communities and guilds’ distributions were governed by climate directly, and indirectly as mediated through streamflow. In Chapter Four, I discuss the utility of guild-based assessments of riparian vegetation, current limitations to these approaches, and potential future applications of the riparian vegetation guild concept to floodplain conservation and management. The classification of vegetation into functional trait-based guilds provides a flexible, framework from which to understand riparian biogeography, complementing other models frameworks for riparian vegetation.
Thakali, Ranjeet. « ANALYZING THE EFFECTS OF CLIMATE CHANGE ON URBAN STORMWATER INFRASTUCTURES ». OpenSIUC, 2017. https://opensiuc.lib.siu.edu/theses/2156.
Yang, Heng. « The hydrologic effects of climate change and urbanization in the Las Vegas Wash Watershed, Nevada ». University of Cincinnati / OhioLINK, 2013. http://rave.ohiolink.edu/etdc/view?acc_num=ucin1384334002.
Mukherjee, Rajarshi, et Rajarshi Mukherjee. « Implications of Statistical and Dynamical Downscaling Methods on Streamflow Projections for the Colorado River Basin ». Thesis, The University of Arizona, 2016. http://hdl.handle.net/10150/620708.
Jung, Gerlinde [Verfasser]. « Regional climate change and the impact on hydrology in the Volta Basin of West Africa / Gerlinde Jung ». Karlsruhe : Forschungszentrum Karlsruhe, 2006. http://d-nb.info/983081263/34.
Kigobe, Max. « Modelling the effects of land use change and climate variability on the hydrology of the upper Nile ». Thesis, Imperial College London, 2012. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.555946.
Somor, Andrew. « Quantifying streamflow change following bark beetle outbreak in multiple central Colorado catchments ». Thesis, The University of Arizona, 2010. http://hdl.handle.net/10150/193435.
Stagge, James Howard. « Optimization of Multi-Reservoir Management Rules Subject to Climate and Demand Change in the Potomac River Basin ». Diss., Virginia Tech, 2012. http://hdl.handle.net/10919/77144.
Ph. D.
Wyatt, Clinton J. W. « Estimating aquifer response following forest restoration and climate change along the Mogollon Rim, northern Arizona ». Thesis, Northern Arizona University, 2013. http://pqdtopen.proquest.com/#viewpdf?dispub=1537821.
Landscape-scale forest restoration treatments are planned for four national forests in Northern Arizona: the Coconino, Kaibab, Tonto, and Apache-Sitgreaves National Forests. The first analysis area comprises 900,000 acres on the Coconino and Kaibab National Forests where the U.S. Forest Service is proposing restoration activities on approximately 600,000 acres over a ten year period pending acceptance of an Environmental Impact Statement. These forest restoration treatments are intended to accomplish a number of objectives including reducing the threat of catastrophic wild fire and subsequent flooding and to restore forest health, function, and resiliency. Previous studies suggest that in semi-arid, ponderosa pine watersheds there was a possibility to increase surface water yields 15-40% when basal area was reduced by 30-100%. Because of these results, there is considerable interest in the amount of increased water yield that may recharge from these activities.
The objectives of this study were to 1) examine the state of knowledge of forest restoration thinning and its hydrological responses and to evaluate the quality and type of related references that exist within the literature and 2) simulate possible changes in recharge and aquifer response following forest restoration treatments and climate change. A systematic review process following the guidelines suggested by the Collaboration for Environmental Evidence was conducted to examine literature relevant to this topic. The Northern Arizona Regional Groundwater-Flow Model was used to simulate the changes expected from forest restoration treatments and climate change.
The systematic review returned 37 references that were used to answer questions regarding tree removal and the associated hydrological responses. Data from individual studies suggest that forest treatments that reduce tree density tend to increase surface water yield and groundwater recharge while reducing evapotranspiration. On average, there was a 0-50% increase in surface water yield when 5-100% of a watershed was treated. Groundwater results were less conclusive and there was no overall correlation for all studies between percent area treated and groundwater recharge. A majority of studies (33 of 37) reported statistically significant results, either as increases in water yield, decreases in evapotranspiration, or increases in groundwater table elevation. Results are highly variable, and diminish within five to ten years for water yield increases and even quicker (< 4 years) for groundwater table heights.
Using a groundwater-flow model, it was estimated that over the ten-year period of forest restoration treatment there was a 2.8% increase in annual recharge to aquifers in the Verde Valley compared to conditions that existed in 2000-2005. However, these increases were assumed to quickly decline after treatment due to regrowth of vegetation and forest underbrush. Furthermore, estimated increases in groundwater recharge were masked by decreases in water levels, stream baseflow, and groundwater storage resulting from surface water diversions and groundwater pumping. These results should be used in conjunction with other data such as those recovered from paired-watershed studies to help guide decision-making with respect to groundwater supply and demand issues, operations, and balancing the needs of both natural and human communities.
Lang, Megan Weiner. « Radar monitoring of hydrology in Maryland's forested coastal plain wetlands implications for predicted climate change and improved mapping / ». College Park, Md. : University of Maryland, 2005. http://hdl.handle.net/1903/2944.
Thesis research directed by: Geography. Title from t.p. of PDF. Includes bibliographical references. Published by UMI Dissertation Services, Ann Arbor, Mich. Also available in paper.
Mwangi, Hosea Munge. « Impact of land use change and climate variability on watershed hydrology in the Mara River Basin, East Africa ». Thesis, Bangor University, 2016. https://research.bangor.ac.uk/portal/en/theses/impact-of-land-use-change-and-climate-variability-on-watershed-hydrology-in-the-mara-river-basin-east-africa(54692d94-33ee-40a5-9475-d5f1f7148be3).html.
Mwangi, Hosea Munge. « Impact of Land Use Change and Climate Variability on Watershed Hydrology in the Mara River Basin, East Africa ». Doctoral thesis, Saechsische Landesbibliothek- Staats- und Universitaetsbibliothek Dresden, 2017. http://nbn-resolving.de/urn:nbn:de:bsz:14-qucosa-209530.
Ranatunga, Thushara D. « Simulation of Watersheds Hydrology under Different Hydro-Climatic Settings ». University of Cincinnati / OhioLINK, 2015. http://rave.ohiolink.edu/etdc/view?acc_num=ucin1421925170.
Siswanto, Shantosa Yudha. « Impact Evaluation of Future Climate and Land Use Scenarios on Water and Sediment Regime using Distributed Hydrological Modelling in a Tropical Rainforest Catchment in West Java (Indonesia) ». Doctoral thesis, Universitat Politècnica de València, 2020. http://hdl.handle.net/10251/153152.
[ES] El cambio climático ha afectado a Indonesia, por ejemplo, incrementando la temperatura del aire en la superficie, incluso en la cuenca del Upper Citarum. Este fenómeno conduce a la falta de agua en la estación seca, reduciendo la producción agrícola lo que es un gran obstáculo para su actividad. Además, la actividad humana ha producido cambios severos en LULC en la cuenca del Upper Citarum, Indonesia. Esto se debe al elevado crecimiento de la población en la región, por el que se han convertido campos de arroz y áreas boscosas en suelo urbano. De esta forma, el objetivo general de esta tesis es comprender y analizar el impacto de los cambios climáticos y LULC en el proceso hidrológico y su relación con los cambios históricos y futuros mediante el uso de modelos distribuidos espacialmente en la cuenca tropical del Upper Citarum. El modelo distribuido TETIS se ha implementado para obtener los resultados de escenarios pasados y futuros en los ciclos de agua y sedimentos. Se usaron batimetrías históricas anuales en el embalse para calibrar y validar el submodelo de sedimentos que involucra la evolución de la densidad de Miller y la eficiencia de retención de la ecuación de Brune. Con el fin de arrojar más luz sobre estos problemas, el escenario de cambio climático se ha implementado en base al modelo de cambio climático bajo las trayectorias RCP 45 y RCP 85. Además, para intentar resolver el problema LULC, también se ha implementado el LULC histórico y futuro. El modelo LCM se usó para pronosticar el LULC en 2029 y los resultados muestran, por un lado, una continuación en la expansión de las áreas urbanas a expensas de los arrozales contiguos. Los resultados determinaron que la deforestación y la urbanización fueron los factores más influyentes para la alteración de los procesos hidrológicos y sedimentológicos en la cuenca del Upper Citarum. Por lo tanto, disminuye la evapotranspiración, aumenta la producción de agua al aumentar todos sus componentes; escorrentía, interflujo y flujo base. Los cambios en LULC están produciendo y producirán, un incremento relativamente pequeño de las tasas de erosión, aumentando el área excede la erosión de Tsl. La producción de sedimentos aumentará en 2029 como resultado del incremento de la erosión. Se espera que otros escenarios de LULC como la conservación, el plan gubernamental y los escenarios de vegetación natural tengan un incremento en la evapotranspiración total, y se espera que la producción de agua disminuya. El régimen de inundación, la erosión y la sedimentación se reducen drásticamente. Por lo tanto, habrá un incremento de la vida útil del embalse y la energía hidroeléctrica. El cambio climático altera la magnitud del equilibrio hídrico y puede identificarse a partir del cambio de infiltración, escorrentía, interflujo, flujo base y producción de agua. Esos incrementos finalmente cambian el régimen de inundación y erosión de la cuenca. La trayectoria RCP 85 tiene un mayor impacto en comparación con la trayectoria RCP 45 en el ciclo hidrológico y de sedimentos. El cambio de LULC tiene un mayor impacto en el balance hídrico, el régimen de inundación, la erosión y la sedimentación. La combinación del cambio climático y LULC tiene un mayor impacto en los flujos de equilibrio hídrico, erosión, inundación, sedimentación y será catastrófico para la operación hidroeléctrica de la presa Saguling.
[CA] El canvi climàtic ha afectat Indonèsia, per exemple, incrementant la temperatura de l'aire en la superfície, inclús en la conca de l'Upper Citarum. Aquest fenomen conduïx a la falta d'aigua en l'estació seca, reduint la producció agrícola, el que és un gran obstacle per a la seua activitat. A més, l'activitat humana ha produït canvis severs en LULC en la conca de l'Upper Citarum, Indonèsia. Açò es deu a l'elevat creixement de la població en la regió, motiu pel qual s'han anat convertint camps d'arròs i àrees boscoses en sòl urbà. D'aquesta manera, l'objectiu general d'aquesta tesi és comprendre i analitzar l'impacte dels canvis climàtics i LULC en el procés hidrològic i la seua relació amb els canvis històrics i futurs per mitjà de l'ús de models distribuïts espacialment en la conca tropical de l'Upper Citarum. El model distribuït TETIS s'ha implementat per a obtindre els resultats d'escenaris passats i futurs en els cicles de l'aigua i sediments. Es van usar batimetries històriques anuals en l'embassament per a calibrar i validar el submodel de sediments que involucra l'evolució de la densitat de Miller i l'eficiència de retenció de l'equació de Brune. Amb la finalitat de donar més llum a aquests problemes, l'escenari de canvi climàtic s'ha implementat basant-se en el model de canvi climàtic davall les trajectòries RCP 45 i RCP 85. A més, per a intentar resoldre el problema LULC, també s'ha implementat el LULC històric i futur. El model LCM es va usar per a pronosticar el LULC en 2029 i els resultats mostren, d'una banda, una continuació en l'expansió de les àrees urbanes a costa dels arrossars contigus. Els resultats van determinar que la desforestació i la urbanització van ser els factors més influents per a l'alteració dels processos hidrològics i sedimentològics en la conca de l'Upper Citarum. Per tant, disminuïx l'evapotranspiració, augmenta la producció d'aigua en augmentar tots els seus components; escorrentia, interflux i flux base. Els canvis en LULC estan produint i produiran, un increment relativament xicotet de les taxes d'erosió, augmentant l'àrea excedix l'erosió de Tsl. La producció de sediments augmentarà en 2029 com a resultat de l'increment de l'erosió. S'espera que altres escenaris de LULC com la conservació, el pla governamental i els escenaris de vegetació natural tinguen un increment en l'evapotranspiració total, i s'espera que la producció d'aigua disminuïsca. El règim d'inundació, l'erosió i la sedimentació es reduïxen dràsticament. Per tant, hi haurà un increment de la vida útil de l'embassament i l'energia hidroelèctrica. El canvi climàtic altera la magnitud de l'equilibri hídric i pot identificar-se a partir del canvi d'infiltració, escorrentia, interflux, flux base i producció d'aigua. Eixos increments finalment canvien el règim d'inundació i erosió de la conca. La trajectòria RCP 85 té un major impacte en comparació amb la trajectòria RCP 45 en el cicle hidrològic i de sediments. El canvi de LULC té un major impacte en el balanç hídric, el règim d'inundació, l'erosió i la sedimentació. La combinació del canvi climàtic i LULC té un major impacte en els fluxos d'equilibri hídric, erosió, inundació, sedimentació i serà catastròfic per a l'operació hidroelèctrica de la presa Saguling.
thank the Directorate General of Higher Education of Indonesia (DIKTI), for granting me the opportunity to pursue PhD study and adventure in Europe. The authors are also thankful to the Spanish Ministry of Economy and Competitiveness through the research projects TETISMED (CGL2014-58127-C3-3-R) and TETISCHANGE (RTI2018-093717-B-I00).
Siswanto, SY. (2020). Impact Evaluation of Future Climate and Land Use Scenarios on Water and Sediment Regime using Distributed Hydrological Modelling in a Tropical Rainforest Catchment in West Java (Indonesia) [Tesis doctoral no publicada]. Universitat Politècnica de València. https://doi.org/10.4995/Thesis/10251/153152
TESIS
Witte, Becky A. « Impacts of Climate Change and Population Growth on Water Stress in the Tucson Active Management Area ». Thesis, The University of Arizona, 2013. http://hdl.handle.net/10150/293624.
Liu, Huidong. « Environmental change in former and present Karner Blue butterfly habitats ». Bowling Green State University / OhioLINK, 2008. http://rave.ohiolink.edu/etdc/view?acc_num=bgsu1210181611.
Cresso, Matilda. « The Impact of Climate Changes On Hydrology and Water Resources In the Andean Páramos-Colombia ». Thesis, Stockholms universitet, Institutionen för naturgeografi, 2019. http://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-179849.
MAXIMOV, IVAN A. « INTEGRATED ASSESSMENT OF CLIMATE AND LAND USE CHANGE EFFECTS ON HYDROLOGY AND WATER QUALITY OF THE UPPER AND LOWER GREAT MIAMI RIVER ». University of Cincinnati / OhioLINK, 2003. http://rave.ohiolink.edu/etdc/view?acc_num=ucin1060964940.
Bhandari, Ranjit. « ANALYZING STREAMFLOW VARIABILITY UNDER CMIP5 PROJECTIONS USING SWAT MODEL ». OpenSIUC, 2018. https://opensiuc.lib.siu.edu/theses/2363.
Maldonado, Philip Pasqual. « Low Flow Variations in Source Water Supply for the Occoquan Reservoir System Based on a 100-Year Climate Forecast ». Thesis, Virginia Tech, 2011. http://hdl.handle.net/10919/35203.
This study uses established techniques to incorporate both climate and land use/demand change into a hydrologic model of the Occoquan watershed, which encompasses an area of approximately 1,550 square kilometers in Northern Virginia, U.S.A., and is part of the drinking water supply to approximately 1.7 million residents.
Master of Science
Niraula, Rewati. « Understanding the Hydrological Response of Changed Environmental Boundary Conditions in Semi-Arid Regions : Role of Model Choice and Model Calibration ». Diss., The University of Arizona, 2015. http://hdl.handle.net/10150/594961.
Siebenmorgen, Christopher B. « Potential climate change impacts on hydrologic regimes in northeast Kansas ». Thesis, Kansas State University, 2010. http://hdl.handle.net/2097/6993.
Department of Biological & Agricultural Engineering
Kyle R. Douglas-Mankin
The Great Plains once encompassed 160 million hectares of grassland in the central United States. In the last several decades, conversion of grassland to urban and agricultural production areas has caused significant increases in runoff and erosion. Past attempts to slow this hydrologic system degradation have shown success, but climate change could once again significantly alter the hydrology. The Intergovernmental Panel on Climate Change (IPCC) studies the state of knowledge pertaining to climate change. The IPCC has developed four possible future scenarios (A1, A2, B1 and B2). The output temperature and precipitation data for Northeast Kansas from fifteen A2 General Circulation Models (GCMs) were analyzed in this study. This analysis showed that future temperature increases are consistent among the GCMs. On the other hand, precipitation projections varied greatly among GCMs both on annual and monthly scales. It is clear that the results of a hydrologic study will vary depending on which GCM is used to generate future climate data. To overcome this difficulty, a way to take all GCMs into account in a hydrologic analysis is needed. Separate methods were used to develop three groups of scenarios from the output of fifteen A2 GCMs. Using a stochastic weather generator, WINDS, monthly adjustments for future temperature and precipitation were applied to actual statistics from the 1961 – 1990 to generate 105 years of data for each climate scenario. The SWAT model was used to simulate watershed processes for each scenario. The streamflow output was analyzed with the Indicators of Hydrologic Alteration program, which calculated multiple hydrologic indices that were then compared back to a baseline scenario. This analysis showed that large changes in projected annual precipitation caused significant hydrologic alteration. Similar alterations were obtained using scenarios with minimal annual precipitation change. This was accomplished with seasonal shifts in precipitation, or by significantly increasing annual temperature. One scenario showing an increase in spring precipitation accompanied by a decrease in summer precipitation caused an increase in both flood and drought events for the study area. The results of this study show that climate change has the potential to alter hydrologic regimes in Northeast Kansas.
Zhang, Feng. « Climate change assessment for the southeastern United States ». Diss., Georgia Institute of Technology, 2011. http://hdl.handle.net/1853/45770.
Swetnam, Tyson L., Paul D. Brooks, Holly R. Barnard, Adrian A. Harpold et Erika L. Gallo. « Topographically driven differences in energy and water constrain climatic control on forest carbon sequestration ». WILEY, 2017. http://hdl.handle.net/10150/624369.
Braff, Pamela. « Evaluating The Impacts Of Land Use And Climate Change On The Hydrology Of Headwater Wetlands In The Coastal Plain Of Virginia ». W&M ScholarWorks, 2020. https://scholarworks.wm.edu/etd/1593091561.
Henriques, Catarina. « Hydrology and water resources management in East Anglia and north west England in the context of climate and socio-economic change ». Thesis, Cranfield University, 2007. http://dspace.lib.cranfield.ac.uk/handle/1826/2743.
La, Frenierre Jeff David. « Assessing the Hydrologic Implications of Glacier Recession and the Potential for Water Resources Vulnerability at Volcan Chimborazo, Ecuador ». The Ohio State University, 2014. http://rave.ohiolink.edu/etdc/view?acc_num=osu1402593347.
Datko, James A. « Carbon mitigation in the power sector as a solution to global climate change, a good idea but how much water will it cost ? » The Ohio State University, 2010. http://rave.ohiolink.edu/etdc/view?acc_num=osu1284138162.