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Thematische Bibliographien / Hydrology|Climate Change

Auswahl der wissenschaftlichen Literatur zum Thema „Hydrology|Climate Change“

Autor: Grafiati

Veröffentlicht am 14. September 2021

Zuletzt aktualisiert am 1. Februar 2022

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Inhaltsverzeichnis

Zeitschriftenartikel
Dissertationen
Bücher
Buchteile
Konferenzberichte
Berichte der Organisationen

Zeitschriftenartikel zum Thema "Hydrology|Climate Change":

1

Hattermann, Fred Fokko, Shaochun Huang und Hagen Koch. „Climate change impacts on hydrology and water resources“. Meteorologische Zeitschrift 24, Nr. 2 (13.04.2015): 201–11. http://dx.doi.org/10.1127/metz/2014/0575.

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2

Gleick, Peter H. „Climate change, hydrology, and water resources“. Reviews of Geophysics 27, Nr. 3 (1989): 329. http://dx.doi.org/10.1029/rg027i003p00329.

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3

Kutics, Károly, und Gabriella Kravinszkaja. „Lake Balaton hydrology and climate change“. Ecocycles 6, Nr. 1 (2020): 88–97. http://dx.doi.org/10.19040/ecocycles.v6i1.165.

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4

Huntingford, Chris, John Gash und Anna Maria Giacomello. „Climate change and hydrology: next steps for climate models“. Hydrological Processes 20, Nr. 9 (2006): 2085–87. http://dx.doi.org/10.1002/hyp.6208.

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5

Brubaker, K. L., und A. Rango. „Response of snowmelt hydrology to climate change“. Water, Air, & Soil Pollution 90, Nr. 1-2 (Juli 1996): 335–43. http://dx.doi.org/10.1007/bf00619293.

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6

Darling, W. G. „The isotope hydrology of quaternary climate change☆“. Journal of Human Evolution 60, Nr. 4 (April 2011): 417–27. http://dx.doi.org/10.1016/j.jhevol.2010.05.006.

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7

Lamichhane und Shakya. „Integrated Assessment of Climate Change and Land Use Change Impacts on Hydrology in the Kathmandu Valley Watershed, Central Nepal“. Water 11, Nr. 10 (02.10.2019): 2059. http://dx.doi.org/10.3390/w11102059.

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The population growth and urbanization are rapidly increasing in both central and peripheral areas of the Kathmandu Valley (KV) watershed. Land use/cover (LULC) change and climate variability/change are exacerbating the hydrological cycle in the KV. This study aims to evaluate the extent of changes in hydrology due to changes in climate, LULC and integrated change considering both factors, with KV watershed in central Nepal as a case study. Historical LULC data were extracted from satellite image and future LULC are projected in decadal scale (2020 to 2050) using CLUE-S (the Conversion of Land Use and its Effects at Small regional contest) model. Future climate is projected based on three regional climate models (RCMs) and two representative concentration pathways (RCPs) scenarios, namely, RCP4.5 and RCP8.5. A hydrological model in soil and water assessment tool (SWAT) was developed to simulate hydrology and analyze impacts in hydrology under various scenarios. The modeling results show that the river runoff for RCP4.5 scenarios is projected to increase by 37%, 21%, and 12%, respectively, for climate change only, LULC only, and integrated changes of both. LULC change resulted in an increase in average annual flow, however, a decrease in base-flow. Furthermore, the impacts of integrated changes in both LULC and climate is not a simple superposition of individual changes.

8

Mujumdar, P. P., und Subimal Ghosh. „CLIMATE CHANGE IMPACT ON HYDROLOGY AND WATER RESOURCES“. ISH Journal of Hydraulic Engineering 14, Nr. 3 (Januar 2008): 1–17. http://dx.doi.org/10.1080/09715010.2008.10514918.

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9

Miller, Norman L., Kathy E. Bashford und Eric Strem. „POTENTIAL IMPACTS OF CLIMATE CHANGE ON CALIFORNIA HYDROLOGY“. Journal of the American Water Resources Association 39, Nr. 4 (August 2003): 771–84. http://dx.doi.org/10.1111/j.1752-1688.2003.tb04404.x.

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10

Hagemann, S., C. Chen, D. B. Clark, S. Folwell, S. N. Gosling, I. Haddeland, N. Hanasaki et al. „Climate change impact on available water resources obtained using multiple global climate and hydrology models“. Earth System Dynamics 4, Nr. 1 (07.05.2013): 129–44. http://dx.doi.org/10.5194/esd-4-129-2013.

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Abstract. Climate change is expected to alter the hydrological cycle resulting in large-scale impacts on water availability. However, future climate change impact assessments are highly uncertain. For the first time, multiple global climate (three) and hydrological models (eight) were used to systematically assess the hydrological response to climate change and project the future state of global water resources. This multi-model ensemble allows us to investigate how the hydrology models contribute to the uncertainty in projected hydrological changes compared to the climate models. Due to their systematic biases, GCM outputs cannot be used directly in hydrological impact studies, so a statistical bias correction has been applied. The results show a large spread in projected changes in water resources within the climate–hydrology modelling chain for some regions. They clearly demonstrate that climate models are not the only source of uncertainty for hydrological change, and that the spread resulting from the choice of the hydrology model is larger than the spread originating from the climate models over many areas. But there are also areas showing a robust change signal, such as at high latitudes and in some midlatitude regions, where the models agree on the sign of projected hydrological changes, indicative of higher confidence in this ensemble mean signal. In many catchments an increase of available water resources is expected but there are some severe decreases in Central and Southern Europe, the Middle East, the Mississippi River basin, southern Africa, southern China and south-eastern Australia.

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Dissertationen zum Thema "Hydrology|Climate Change":

1

Serrat, Capdevila Aleix. „Climate Change Impacts in Hydrology: Quantification and Societal Adaptation“. Diss., The University of Arizona, 2009. http://hdl.handle.net/10150/194702.

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The research presented here attempts to bridge science and policy through the quantification of climate change impacts and the analysis of a science-fed participatory process to face a sustainability challenge in the San Pedro Basin (Arizona). Paper 1 presents an assessment of a collaborative development process of a decision support system model between academia and a multi-stakeholder consortium created to solve water sustainability problems in a local watershed. This study analyzes how science-fed multi-stakeholder participatory processes lead to sustainability learning promoting resilience and adaptation. Paper 2 presents an approach to link an ensemble of global climate model outputs with a hydrological model to quantify climate change impacts in the hydrology of a basin, providing a range of uncertainty in the results. Precipitation projections for the current century from different climate models and IPCC scenarios are used to obtain recharge estimates as inputs to a groundwater model. Quantifying changes in the basin's water budget due to changes in recharge, evapotranspiration (ET) rates are assumed to depend only on groundwater levels. Picking on such assumption, Paper 3 explores the effects of a changing climate on ET. Using experimental eddy covariance data from three riparian sites, it analyzes seasonal controls on ET. An approach to quantify evapotranspiration rates and growing season length under warmer climates is proposed. Results indicate that although atmospheric demand will be greater, increasing pan and reference crop evaporation, ET rates at the studied field sites will remain unchanged due to stomatal regulation. However, the length of the growing season will increase, mainly with an earlier leaf-out and at a lesser level by a delayed growing season end. These findings - implying decreased aquifer recharge, increased riparian water use and a lesser water balance - are very relevant for water management in semi-arid regions. Paper 4, in which I am second author, explores the theory relating changes in area-average and pan evaporation. Using the same experimental data as Paper 3, it corroborates a previous theoretical relationship and discusses the validity of Bouchet's hypothesis.

2

Hackett, William. „Changing Land Use, Climate, and Hydrology in the Winooski“. ScholarWorks @ UVM, 2009. http://scholarworks.uvm.edu/graddis/99.

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This study analyzes temporal trends and periodicity in seventy years of publicly available stream discharge and climate data for the Winooski River Basin of northern Vermont as well as lake level data for adjacent Lake Champlain. We also use random sampling and manual, point-based classification of recent and historical aerial imagery to quantify land use change over the past seventy years in the 2,704 km2 Winooski River Basin of northern Vermont. We find a general increase in annual precipitation, discharge, and mean lake level with time in the basin; discharge increases 18% over the period of record while precipitation increases by 14%. Over the last 70 years, mean annual temperature has increased at the Burlington Vermont station by 0.78 degrees Celsius (1.4 degrees Fahrenheit). Four sets of aerial photographs, taken at intervals of 12 to 29 years between 1937 and 2003 at thirty randomly selected sites, demonstrate that actively cleared land area has decreased by 14%, while forested land and impervious surfaces increased by 10% and 5%, respectively. Spectral analysis of precipitation, discharge and lake level data show a ~7.6 year periodicity, which is in phase with the North Atlantic Oscillation (NAO); higher than average precipitation and discharge are most likely when the NAO is in a positive mode. The NAO relationship demonstrates that discharge is largely controlled by precipitation; anthropogenic changing climate and changing land use over the past 70 years appear to have subtly changed the seasonality of discharge and caused an increase in base flow.

3

Larson, Robert, und 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.

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A modelling approach focused on snow hydrology was developed and applied to project future changes in spring streamflow volumes in the St. Mary River headwaters basin, Montana. A spatially distributed, physically-based, hydrometeorological and snow mass balance model was refined and used to produce snow water equivalent (SWE) and rainfall surfaces for the study watershed. Snowmelt runoff (SR) and effective rainfall runoff (RR) volumes were compiled for the 1961-2004 historical period. A statistical regression model was developed linking spring streamflow volume (QS) at Babb, Montana to the SR and RR modelled data. The modelling results indicated that SR explained 70% of the variability in QS while RR explained another 9%. The model was applied to climate change scenarios representing the expected range of future change to produce annual QS for the period 2010-2099. Compared to the base period (1961-1990), average QS change ranged from -3% to -12% for the 2020s period. Percent changes increased to between -25% and -32% for the 2050s, and -38% and -55% for the 2080s. Decreases in QS also accompanied substantial advances in the onset of spring snowmelt. Whereas the spring pulse onset on average occurred on April 8 for the base period, it occurred 36 to 50 days earlier during the 2080s. The findings suggest that increasing precipitation will not compensate for the effects of increasing temperature in watershed SWE and associated spring runoff generation. There are implications for stakeholder interests related to ecosystems, the irrigation industry, and recreation.
xii, 136 leaves : ill. ; 28 cm. --

4

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.

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5

Booth, Andrew. „Impacts of desiccation cracking and climate change on highway cutting hydrology“. Thesis, Loughborough University, 2014. https://dspace.lboro.ac.uk/2134/14825.

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Climate change is predicted to have a global effect on temperatures and precipitation rates throughout the world. The UK Climate projections expect that in the United Kingdom this will lead to warmer, drier summers and wetter winters, where events of extreme rainfall are more common. These changes are expected to impact on slope hydrology, and concurrently slope stability. In the United Kingdom this impact is expected to be negative, whereas in other countries, such as Italy and France it could lead to slopes being more stable. Infrastructure slopes in the UK range in age and construction quality, they are susceptible to serviceability problems, characterised by heterogeneous material properties and can fail unexpectedly due to progressive reduction in soil shear strength. In this thesis the effects of climate change on a highway cutting in the south of England are modelled, using numerical methods. A finite element model is created and developed in the software package GeoStudio VADOSE/W. The model has been validated against observed pore water pressure trends and magnitudes and is shown to be able to accurately replicate the behaviour. By incorporating the effects of desiccation cracking on the soil s material properties, by the means of bimodal soil water characteristic curve and hydraulic conductivity function, the replication of these trends is improved even further. A series of future climate series were created using the UKCP09 Weather Generator 2.0. These series were implemented with the VADOSE/W model as climate boundary conditions and models were run, and the results compared to control, current climate results. The results were investigated by the means of statistical analyses which revealed that climate change will have some significant effects on the slope s hydrology, increasing magnitudes of evapotranspiration greatly which can have further significant effects on the magnitude of suctions developing in the slope throughout the summer. It is thought that the results suggest that climate change will not have significant negative effects on slope stability. However it is important to remember that the results only apply with certainty to the specific slope and climate change scenario investigated here. The methods used and developed within this thesis can be extended to other locations, in the UK and internationally, analysing the effects of different climate change scenarios.

6

Wherry, Susan Amelia. „Climate Change Effects and Water Vulnerability in the Molalla Pudding River Basin, Oregon, USA“. Portland State University, 2013.

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7

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.

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8

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.

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Thesis: Ph. D., Massachusetts Institute of Technology, Department of Civil and Environmental Engineering, 2016.
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.

9

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.

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Shifting climatic regimes can increase or decrease the frequency of extreme hydrologic events (e.g., high and low streamflows) causing large societal and environmental impacts. The impacts are numerous and include human health and safety, the destruction of infrastructure, water resources, nutrient and sediment transport, and within stream ecological health. It is unclear how the hydrology of a given region will shift in response to climate change. This is especially the case in areas that are seasonally snow covered as the interplay of changing temperature, precipitation, and resulting snowpack can lead to an increased risk of flood or drought. This research aimed to understand the ways temperature and precipitation are changing using general circulation models and observed weather station data in the northeastern United States. With the knowledge that general circulation models do not accurately represent precipitation statistics and trends from the historical period, a large network of climate stations was utilized to further investigate shifts in precipitation. A hydrology model was utilized for further study of regional hydrology. The model used was the Regional Hydro-Ecologic Simulation System, which was calibrated to snow coverage and streamflow for a historical time period. The hydrology model was used to investigate the relationship of snow and streamflow in a changing climate. We characterized climate change and related impacts in the northeastern United States and estimated a decrease in snowfall of 50% and the number of days below freezing by 45 days by the end of the century. We also showed that precipitation is not only becoming more intense, but it is also more persistent -- a finding that may have significant hydrological implications including increased flood risk throughout the year. The 95th percentile of daily precipitation has increased by 0.5 mm per day per decade, while the probability of successive days with precipitation increased by 0.6 percent per decade. We also explored the role of snowpack in a changing climate. We found that temperature plays a larger role than precipitation in shifting hydrologic regime, because the warming-induced reduction of snowpack reduced the maximum flows more than the increasing precipitation increased the maximum flows. However, because of the increasing intensity and persistence of precipitation, instantaneous peak flows occurring outside of the snowmelt season will likely continue to increase during all times of the year. We shed light on the complexity of the modes of climate change and the interactions that increases in temperature and precipitation can have on the hydrology of a region.

10

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/.

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This thesis explores human-environment interactions during the Mid-Late Holocene in raised bogs in central Ireland. The raised bogs of central Ireland are widely-recognised for their considerable palaeoenvironmental and archaeological resources: research over the past few decades has established the potential for such sites to preserve sensitive records of Holocene climatic variability expressed as changes in bog surface wetness (BSW); meanwhile archaeological investigations over the past century have uncovered hundreds of peatland archaeological features dating from the Neolithic through to the Post-Medieval period including wooden trackways, platforms, and deposits of high-status metalwork. Previous studies have attempted to explore the relationship between records of past environmental change and the occurrence of peatland archaeological sites reaching varying conclusions. More recently, environmentally-deterministic models of human-environment interaction in Irish raised bogs at the regional scale have been explicitly tested leading to the conclusion that there is no relationship between BSW and past human activity. These relationships are examined in more detail on a site-by-site basis in this thesis. To that end, testate amoebae-derived BSW records from nine milled former raised bogs in central Ireland were produced from sites with known and dated archaeological records. Relationships between BSW records and environmental conditions within the study area were explored through both the development of a new central Ireland testate amoebae transfer function and through comparisons between recent BSW records and instrumental weather data. Compilation of BSW records from the nine fossil study sites show evidence both for climate forcing, particularly during 3200-2400 cal BP, as well as considerable inter-site variability. Considerable inter-site variability was also evident in the archaeological records of the same sites. Whilst comparisons between BSW and archaeological records do not show a consistent linear relationship, examination of records on a site-by-site basis were shown to reveal interpretatively important contingent relationships. It is concluded therefore, that future research on human-environment interactions should focus on individual sites and should utilise theoretical approaches from the humanities in order to avoid the twin pitfalls of masking important local patterns of change, and of environmental determinism.

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Bücher zum Thema "Hydrology|Climate Change":

1

Gosain, Ashvani K. Modelling climate change impact on the hydrology of the eastern Himalayas. Kathmandu: International Centre for Integrated Mountain Development, 2010.

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Klaus, Seidel. Remote sensing in snow hydrology: Runoff modelling, effect of climate change. Berlin: Springer ; Chichester, UK, 2004.

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3

Seidel, Klaus. Remote sensing in snow hydrology: Runoff modelling, effect of climate change. Berlin: Springer, 2004.

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Brolsma, Reinder Jacob. Effect of climate change on temperate forest ecosystems. Utrecht: Royal Dutch Geographical Society, 2010.

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Dankers, Rutger. Sub-arctic hydrology and climate change: A case study of the Tana River Basin in Northern Fennoscandia. Utrecht: Koninklijk Nederlands Aardrijkskundig Genootschap, 2002.

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6

Blackburn, W. H., und Gregory L. Johnson. Presenting the climate and hydrology research component of the Agricultural Research Service Global Change Research Program: Global change, water resources and agriculture. Boise, Idaho: USDA Agricultural Research Service, Northwest Watershed Research Center, 1992.

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Hladný, Josef. Impacts of a potential climate change on hydrology and water resources in the Czech Republic: Country study of climate change for the Czech Republic, element 2. Prague: Český hydrometeorologický ústav, 1997.

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Agency, European Environment. Regional climate change and adaptation: The Alps facing the challenge of changing water resources. Luxembourg: Office for Official Publications of the European Communities, 2009.

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Abtew, Wossenu, Assefa M. Melesse und Shimelis G. Setegn. Nile River Basin: Ecohydrological challenges, climate change and hydropolitics. Cham: Springer, 2014.

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Workshop on the Effects of Global Climate Change on Hydrology and Water Resources at the Catchment Scale (4th 1997 Honolulu, Hilo, and Kona, Hawaii). Fourth PWRI-USGS Workshop on Hydrology, Water Resources, and Global Climate Change: February 24-28, 1997, Honolulu, Hilo, and Kona, Hawaii USA : summary report. [Washington, D.C.?]: Japan-U.S. Committee on Hydrology, Water Resources, and Global Climate Change, 1997.

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Buchteile zum Thema "Hydrology|Climate Change":

1

HARDING, RICHARD, NIGEL ARNELL, NICK REYNARD, CHRISTEL PRUDHOMME, ELEANOR BLYTH und CHRIS TAYLOR. „Climate Change and Hydrology“. In Progress in Modern Hydrology: Past, Present and Future, 302–23. Chichester, UK: John Wiley & Sons, Ltd, 2015. http://dx.doi.org/10.1002/9781119074304.ch10.

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2

Ye, Duzheng. „Sensitivity of Climate Model to Hydrology“. In Understanding Climate Change, 101–8. Washington, D. C.: American Geophysical Union, 2013. http://dx.doi.org/10.1029/gm052p0101.

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Moors, E. J., und A. J. Dolman. „Land-Use Change, Climate and Hydrology“. In Global Environmental Change and Land Use, 139–65. Dordrecht: Springer Netherlands, 2003. http://dx.doi.org/10.1007/978-94-017-0335-2_6.

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Hyndman, David W. „Impacts of Projected Changes in Climate on Hydrology“. In Global Environmental Change, 211–20. Dordrecht: Springer Netherlands, 2014. http://dx.doi.org/10.1007/978-94-007-5784-4_131.

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5

Breuer, Lutz, Jean-François Exbrayat, Ina Plesca, Wouter Buytaert, Theresa Ehmann, Thorsten Peters, Edison Timbe, Katja Trachte und David Windhorst. „Global Climate Change Impacts on Local Climate and Hydrology“. In Ecosystem Services, Biodiversity and Environmental Change in a Tropical Mountain Ecosystem of South Ecuador, 265–74. Berlin, Heidelberg: Springer Berlin Heidelberg, 2013. http://dx.doi.org/10.1007/978-3-642-38137-9_19.

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Rowntree, Peter R., und Lydia Dümenil. „Hydrology in Climate Models and Effects on Climate“. In The Role of Water and the Hydrological Cycle in Global Change, 59–104. Berlin, Heidelberg: Springer Berlin Heidelberg, 1995. http://dx.doi.org/10.1007/978-3-642-79830-6_3.

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Brubaker, K. L., und A. Rango. „Response of Snowmelt Hydrology to Climate Change“. In Clean Water: Factors that Influence Its Availability, Quality and Its Use, 335–54. Dordrecht: Springer Netherlands, 1996. http://dx.doi.org/10.1007/978-94-009-0299-2_32.

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8

Barry, Roger G. „Alpine Climate Change and Cryospheric Responses: An Introduction“. In Climate and Hydrology in Mountain Areas, 1–4. Chichester, UK: John Wiley & Sons, Ltd, 2006. http://dx.doi.org/10.1002/0470858249.ch1.

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9

Chattopadhyay, Somsubhra, und Manoj K. Jha. „Assessment of Climate Change Impact on Watershed Hydrology“. In Proceedings of the 2013 National Conference on Advances in Environmental Science and Technology, 3–11. Cham: Springer International Publishing, 2016. http://dx.doi.org/10.1007/978-3-319-19923-8_1.

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Matalas, Nicholas C. „Stochastic Hydrology in the Context of Climate Change“. In Climate Change and Water Resources Planning Criteria, 89–101. Dordrecht: Springer Netherlands, 1997. http://dx.doi.org/10.1007/978-94-017-1051-0_6.

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Konferenzberichte zum Thema "Hydrology|Climate Change":

1

„Climate Change Has Impacted Winter Hydrology in Ontario“. In ASABE 1st Climate Change Symposium: Adaptation and Mitigation. American Society of Agricultural and Biological Engineers, 2015. http://dx.doi.org/10.13031/cc.20152123855.

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2

„Impacts of Variability of Climate Datasets on Watershed Hydrology under Changing Climate“. In ASABE 1st Climate Change Symposium: Adaptation and Mitigation. American Society of Agricultural and Biological Engineers, 2015. http://dx.doi.org/10.13031/cc.2015212391.

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3

Steinschneider, S., C. Brown, R. N. Palmer und D. Ahlfeld. „Hydrology Models for Climate Change Assessment: Inter-Decadal Climate Variability and Parameter Calibration“. In World Environmental and Water Resources Congress 2011. Reston, VA: American Society of Civil Engineers, 2011. http://dx.doi.org/10.1061/41173(414)428.

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4

Capell,, R., D. Tetzlaff, R. Essery und C. Soulsby. „Climate change impacts on catchment hydrology – a tracer-aided model approach“. In BHS 11th National Hydrology symposium. British Hydrological Society, 2012. http://dx.doi.org/10.7558/bhs.2012.ns10.

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5

„Long-term trends in climate and hydrology in an agricultural headwater watershed“. In ASABE 1st Climate Change Symposium: Adaptation and Mitigation. American Society of Agricultural and Biological Engineers, 2015. http://dx.doi.org/10.13031/cc.20152124135.

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6

Bui, Tai D. „Applied Eco-Hydraulics and Eco-Hydrology for Climate Change Conditions“. In World Environmental and Water Resources Congress 2011. Reston, VA: American Society of Civil Engineers, 2011. http://dx.doi.org/10.1061/41173(414)405.

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7

„Impacts of Climate Change on Hydrology and Water Quality in a watershed in Ontario“. In ASABE 1st Climate Change Symposium: Adaptation and Mitigation. American Society of Agricultural and Biological Engineers, 2015. http://dx.doi.org/10.13031/cc.20152123838.

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8

Dracup, J. A., und S. Vicuna. „An Overview of Hydrology and Water Resources Studies on Climate Change: The California Experience“. In World Water and Environmental Resources Congress 2005. Reston, VA: American Society of Civil Engineers, 2005. http://dx.doi.org/10.1061/40792(173)483.

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9

Ebrahimi, Elahe, Yuosef Filizadeh und Kamran Asgari. „Anzali Wetland Hydrology Monitoring to Detect the Effects of Land Use and Climate Change“. In 2009 Second International Conference on Environmental and Computer Science. IEEE, 2009. http://dx.doi.org/10.1109/icecs.2009.17.

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10

Somsubhra Chattopadhyay und Manoj Kumar Jha. „Watershed modeling of Haw River Basin for Hydrology, Water Quality and Climate Change Study“. In 2012 Dallas, Texas, July 29 - August 1, 2012. St. Joseph, MI: American Society of Agricultural and Biological Engineers, 2012. http://dx.doi.org/10.13031/2013.42171.

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Berichte der Organisationen zum Thema "Hydrology|Climate Change":

1

Zomer, Robert, A. Trabucco, M. Wang und Jianchu Xu. Projected Climate Change Impact on Hydrology, Bioclimatic Conditions, and Terrestrial Ecosystems in the Asian Highlands. World Agroforestry Centre (ICRAF), 2016. http://dx.doi.org/10.5716/wp16006.pdf.

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2

Bharati, Luna, Guillaume Lacombe, Pabitra Gurung, Priyantha Jayakody, Chu Thai Hoanh und Vladimir Smakhtin. The impacts of water infrastructure and climate change on the hydrology of the Upper Ganges River. International Water Management Institute (IWMI), 2011. http://dx.doi.org/10.5337/2011.210.

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