Gotowe bibliografie tematyczne / Water resources

Gotowa bibliografia na temat „Water resources”

Autor: Grafiati

Data publikacji: 4 czerwca 2021

Data aktualizacji: 7 lipca 2024

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Artykuły w czasopismach na temat "Water resources"

Ungalov, Akmal. "WATER RESOURCES MODELING UNDER CLIMATE CHANGE". American Journal of Interdisciplinary Innovations and Research 5, nr 12 (1.12.2023): 29–35. http://dx.doi.org/10.37547/tajiir/volume05issue12-07.

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Modeling of changes in water resources in the Chirchik river basin in the past, present, and futurehas been carried out. Changes in river basin flow dynamics showed an increase in the proportion of precipitation frequency change by 2030 (2020–2039), 3050 (2040–2069) and 2070 under two IPCC scenarios (RCP4.5 and RCP8.5). Although there is a tendency to increase water flow in the Chirchik River basin under climate change scenarios, it was found that due to the uneven distribution of water resources in the future, the available water may not be sufficient based on the needs of water users in the basin.

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Luecke, Daniel F. "Water Resources". Environment: Science and Policy for Sustainable Development 32, nr 4 (maj 1990): 42–45. http://dx.doi.org/10.1080/00139157.1990.9929964.

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Wallis, Ray L., i Sally J. Robinson. "Water Resources". Environment: Science and Policy for Sustainable Development 33, nr 10 (grudzień 1991): 31–33. http://dx.doi.org/10.1080/00139157.1991.9932553.

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Adler, Robert W. "Water Resources". Environment: Science and Policy for Sustainable Development 35, nr 9 (listopad 1993): 4–40. http://dx.doi.org/10.1080/00139157.1993.9929121.

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HAEFNER, H., i P. PAMPALONI. "Water resources". International Journal of Remote Sensing 13, nr 6-7 (kwiecień 1992): 1277–303. http://dx.doi.org/10.1080/01431169208904191.

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James, T. "Water World [water resources]". Engineering & Technology 8, nr 2 (1.03.2013): 59–61. http://dx.doi.org/10.1049/et.2013.0207.

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Ali, Malik H. "Towards Shrimp Resources Investment in Iraq water". IRAQI JOURNAL OF AQUACULTURE 12, nr 2 (2015): 1–6. http://dx.doi.org/10.21276/ijaq.2015.12.2.1.

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Zhang, Fengyi, Zening Wu, Danyang Di i Huiliang Wang. "Water resources allocation based on water resources supply-demand forecast and comprehensive values of water resources". Journal of Hydrology: Regional Studies 47 (czerwiec 2023): 101421. http://dx.doi.org/10.1016/j.ejrh.2023.101421.

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K, VENUGOPAL. "Water Resources Management". International Journal on Design and Manufacturing Technologies 1, nr 1 (2007): 60–62. http://dx.doi.org/10.18000/ijodam.70011.

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Anonymous. "Karst water resources". Eos, Transactions American Geophysical Union 66, nr 7 (1985): 61. http://dx.doi.org/10.1029/eo066i007p00061.

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Rozprawy doktorskie na temat "Water resources"

Martinez, Vila, i Martin Alvaro. "Integrated water resources management: restoration of water quality in water resources from developing countries". Thesis, Сумський державний університет, 2013. http://essuir.sumdu.edu.ua/handle/123456789/31626.

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Water is most essential but scarce resource in developing countries. Presently the quality & the availability of the fresh water resources is the most pressing of the many environmental challenges on the national horizon. The stress on water resources is from multiple sources and the impacts can take diverse forms. Geometric increase in population coupled with rapid urbanization, industrialization and agricultural development has resulted in high impact on quality and quantity of water in developing countries. The situation warrants immediate redressal through radically improved water resource and water quality management strategies. When you are citing the document, use the following link http://essuir.sumdu.edu.ua/handle/123456789/31626

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MendonÃa, Luiz Alberto Ribeiro. "Water resources of Araripe". Universidade Federal do CearÃ, 2001. http://www.teses.ufc.br/tde_busca/arquivo.php?codArquivo=15908.

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nÃo hÃ
Com a finalidade de entender o funcionamento dos aqÃÃferos da Chapada do Araripe, quantificar suas reservas e avaliar a vulnerabilidade Ã poluiÃÃo, foram aplicados, na ausÃncia de dados hidrogeolÃgicos e hidrolÃgicos sistematizados, mÃtodos de hidrogeologia, hidroquÃmica, hidrologia isotÃpica, edafologia, ecologia e modelagem numÃrica. Os resultados sÃo interpretados sinoticamente. Foram feitos (i) a avaliaÃÃo da geologia, (ii) a interpretaÃÃo de medidas quÃmica e isotÃpica (O-18, C-13, H-3 e C-14) das Ãguas, (iii) o estudo da matÃria orgÃnica dos solos (importante agente na recarga) utilizando os isÃtopos N-15 e C-13, (iv) o cÃlculo da capacidade de infiltraÃÃo, em solos de diferentes formaÃÃes florestais, utilizando o modelo de GREEN e AMPT, (v) a simulaÃÃo do fluxo subterrÃneo utilizando os modelos computacionais MODFLOW e MODPATH e (vi) a obtenÃÃo dos Ãndices de vulnerabilidade Ã poluiÃÃo utilizando o mÃtodo de FOSTER e HIRATA. Verificou-se, desta maneira, a intima interrelaÃÃo entre hidrologia, climatologia e ecologia da chapada. Na porÃÃo leste, Ãrea de floresta e de pluviosidade elevada, as Ãguas do Sistema AqÃÃfero Superior sÃo jovens (tempo de residÃncia de ≈ 180 anos e δ 18O≈ -3,24 â) derivadas de chuvas atuais (δ 18O ≈ -3,2 â), enquanto na porÃÃo oeste, mais seca e com vegetaÃÃo rala, encontra-se paleo-Ãguas (pmC ≈ 25,5, ≈10.932 anos) marcadas ainda pelo clima pleistocÃnico mais frio (δ 18O ≈ -5 â). Na primeira Ãrea, a recarga Ã avaliada em ≈ 4 % da precipitaÃÃo anual; porem, as anÃlises de solos indicam uma reduÃÃo da capacidade de infiltraÃÃo para somente 20 % em Ãreas desmatadas, ilustrando a forte influÃncia de mudanÃas da cobertura vegetal sobre o balanÃo hÃdrico (e a vazÃo das fontes) da chapada. A reserva permanente do Sistema AqÃÃfero Superior, calculada pelo MODFLOW, Ã de 13 * 109 m3/ano, a reserva reguladora de 21,4 * 106 m3/ano e a infiltraÃÃo profunda atravÃs de fraturas no aquiclude Santana de 3 * 105 m3/ano. A porÃÃo leste, Ã de moderada vulnerabilidade Ã poluiÃÃo, com exceÃÃo da falha de Jardim que Ã de alta vulnerabilidade. A porÃÃo oeste apresenta-se de baixa vulnerabilidade, com exceÃÃo da falha nas proximidades dos poÃos SerrolÃndia I e II que Ã de moderada vulnerabilidade. Os barreiros estÃo em estado sanitÃrio muito ruim e constituem a entrada principal de poluiÃÃo para a Ãgua subterrÃnea
The objectives of this research were to understand the aquifers of the Araripe Plateau, quantify their resources, and assess their vulnerability to pollution. In order to address the lack of hydrologic and hydrogeologic data, methods from various areas were employed (hydrogeology, hydrochemistry, isotope hydrology, soil science, ecology and numerical modeling). Results are interpreted in a synoptic way. We performed (i) geologic analysis, (ii) chemical and isotopic analyses (O-18, C-13, H-3 and C-14) of water samples, (iii) studied organic material in soils (important to recharge) using N-15 and C-13, (iv) determined the capacity of infiltration for soils with different vegetation using the GREEN and AMPT model, (v) performed MODFLOW and MODPATH simulations of groundwater flow, and (vi) vulnerability study (FOSTER and HIRATA). In this fashion, an intimate relationship between hydrology, climate and ecology was verified for the Araripe Plateau. In the eastern section, with forests and elevated rainfall, waters of the Upper Aquifer System are young (residence time ≈ 180 years) and are derived from present day rainfall, whereas in the western section, with low rainfall and sparse vegetation, paleo-waters (pmC ≈ 25,5, ≈10.932 years) are found, identified by its colder pleistocenic climate (δ 18O ≈ -5 â). In the first area, recharge is estimated to be ≈ 4 % of annual rainfall. However, for areas of deforestation, soil analyses indicate a reduction in the infiltration capacity to only 20 %, illustrating the strong influence of changes in vegetation on the water balance (and the discharge of springs) of the Plateau. MODFLOW simulations calculate for the Upper Aquifer System permanent reserves of 13*109 m3/year, regulating reserves of 21,4*106 m3/year, and a deep percolation, through fractures in the aquiclude Santana, to the Cariri Valley of 3*105 m3/year. With respect to vulnerability, the eastern section is moderate, with exception of the fault of Jardim which is highly vulnerable. The western section of the Araripe Plateau presents low vulnerability, but increasing to moderate in the area of the wells Serrolandia I and II. The ponds (âbarreirosâ) of the Plateau are of very poor sanitary condition and represent critical spots for aquifer pollution

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Heinke, Jens. "Water Resources in the Anthropocene". Doctoral thesis, Humboldt-Universität zu Berlin, 2021. http://dx.doi.org/10.18452/22497.

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Der hydrologische Kreislauf versorgt die Menschheit mit Wasserressourcen, die für ihr Wohlergehen unabdingbar sind. Ziel dieser Arbeit ist es, das Verständnis über klimabedingte Veränderungen des hydrologischen Kreislaufs zu verbessern, wie diese die Verfügbarkeit von Wasserressourcen in der Zukunft beeinflussen und welche Möglichkeiten bestehen, den Druck auf die verfügbaren Wasserressourcen durch Verringerung des anthropogenen Wasserverbrauchs zu reduzieren. Diese Dissertation zeigt, dass der Klimawandel eine große Bedrohung für die Wasserversorgung der zukünftigen Bevölkerung darstellt. Durch Begrenzung des Anstiegs der globalen Mitteltemperatur auf 2 K oder sogar 1,5 K über das vorindustrielle Niveau können gravierende negative Auswirkungen auf die Wasserverfügbarkeit jedoch weitgehend vermieden werden. Dennoch wären einige Regionen wie der Mittelmeerraum "eher wahrscheinlich" von schwerwiegenden hydrologischen Veränderungen betroffen, und in großen Teilen der Welt könnten negative Auswirkungen auf die Wasserverfügbarkeit aufgrund der großen Unsicherheiten in den Projektionen nicht ausgeschlossen werden. Bei der Untersuchung der Nachfrageseite liegt der Schwerpunkt auf der Wassernutzung in der Tierproduktion. Diese Dissertation schätzt den gegenwärtigen Wasserverbrauch für die Produktion von Tierfutter auf 4666 km3/yr (44 % des gesamten landwirtschaftlichen Wasserverbrauchs). Große Verbesserungen der Wasserproduktivität können bei Schweinen und Geflügel durch Verbesserungen sowohl in der Futtermittelproduktion als auch in der Tierhaltung erzielt werden. Bei Wiederkäuern liegt das größte Potenzial in der Verbesserung der Tierhaltung. Allerdings geht eine effizientere Futterverwertung bei Wiederkäuern, die durch erhöhte Beigabe von Kraftfutter erzielt wird, mit einem erhöhten Wasserbedarf für die Produktion des Futters einher. Dadurch ist die Verbesserung der Wasserproduktivität bei Wiederkäuern begrenzt.
The hydrological cycle provides humanity with water resources that are essential for its well-being. The aim of this thesis is to advance the understanding of climate-related changes in the hydrological cycle, how they will affect the availability of water resources in the future, and what opportunities exist to reduce anthropogenic water use to lower the pressure on water resources. This thesis demonstrates that climate change is a large threat to freshwater supply for future populations. Limiting the increase in global mean temperature to 2 K or even 1.5 K above pre-industrial levels can mitigate most of the severe negative impacts on water resources. However, some regions such as the Mediterranean would still ‘more likely than not’ be affected by severe hydrological change, and in large parts of the world, negative impacts on water availability could not be ruled out due to the large uncertainties in the projections. On the demand side, the focus is on water use in the livestock sector. This thesis estimates that about 4666 km3/yr (44 % of total agricultural water use) are currently used for feed production for the livestock sector. Large improvements in livestock water productivity can be achieved for pigs and poultry by improvements in feed production and livestock rearing alike. For ruminants, the largest potential lies in improving livestock management. However, improving the feed use efficiency of ruminants through increased supplementation with forage crops comes at the cost of increased water requirements to produce the feed. This limits the potential for improving livestock water productivity in ruminant production.

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RUGGIU, DARIO. "Hydrological changes on water resources". Doctoral thesis, Università degli Studi di Cagliari, 2021. http://hdl.handle.net/11584/309578.

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Water is one of the essential elements for the nature and human being. The development of good practise of managing water resources are necessary to maintain sufficient availability and to support socio-economic activities and preserve natural ecosystems. For these reasons, it is fundamental to improve the knowledge of cause-effect relations that drives hydrological cycle, which determines water availability. Climate and land use (LU) are two of the main drivers of the water cycle and indeed, the knowledge of their influence on hydrology is a fundamental research question. Of course, the future water availability is strictly related to future climatic and LU scenarios and then a critical role is assumed by the prediction and assessment of these two. A climate and LU change impact study will be developed to investigate the near-future water availability in the Mediterranean area. In detail, on the basis of the state of art and the actual knowledge, the main objective of this dissertation is to estimate the probability density function (pdf) of annual surface runoff Q in transient climate and LU conditions in the island of Sardinia (Italy). The study case has been selected due to the ongoing important process of climate change, overexploitation and degradation of natural resources affecting the entire island (see e.g. ISPRA, ENEA and CIRCE studies). These analyses might have a strategic importance for stakeholders and government agencies that are interested in the management of water resources due to the well-known issue of water availability in the Mediterranean area. The knowledge of the near-future impact of climate and LU change could be useful to establish regional guidelines and good practices to avoid the ongoing reduction of water resources in Sardinia. After a detailed review of the existing methodologies for describing and detecting climate and LU change and their influence in hydrological processes, a methodology based on the Budyko’s theory that aims at assessing near future Q pdf in a closed form has been adopted. Five parameters are requested, referring to mean and standard deviation of annual rainfall P and annual potential evapotranspiration PET and Fu’s parameter ω. Sets of these parameters will be assessed to define different climatic and LU scenarios for the near future. EUROCORDEX and Land Use CORINE projects will be used to represent climate and LU in the present and in the near future. Results showed that in the near future Q will decrease due to the reduction of P and the increase of PET. The variability of Q will decrease due the reduction of variability of P. Finally, it has been observed that in Sardinia the main driver in the change of Q pdf will be climate change, while the LU plays a secondary role.

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Carter, Richard C. "Water resources and water management in north east Nigeria". Thesis, Cranfield University, 1995. http://dspace.lib.cranfield.ac.uk/handle/1826/11117.

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This thesis addresses some aspects of shallow groundwater resources, and the wider issues of water resources use and allocation, in the Yobe river basin, north east Nigeria. The studies reported here were carried out in the context of a research linkage, between a Nigerian and a British _University, set up explicitly to support a large rural development programme. This is probably the first time strategic academic research and regional development have been linked on such a scale in the region. ' Despite significant investment in the past in irrigation and other water resource developments, basic data on land and water resources, and their present use, are limited. Short term studies by Consultants have proved to be no substitute for long term routine monitoring, together with good natural and social science research. « 4 Priority research needs are identified in the sciences of climatology and hydrology, and in the use and management of water in the region. There is very limited knowledge of climatic and hydrological change over the last few decades, and almost total ignorance of the existing ' water uses, their economic value, and the efficiency or otherwise of traditional water management practices. The main issues addressed in the thesis are (i) the shallow groundwater resources of the Manga Grasslands, a upland dunefield, and the Yobe river valley floodplain or fadama, and (ii) the allocation of water resources, especially in the context of large irrigation demands. _ The thesis is presented in the form of six papers -(5 published, one submitted for publication), with a extended introduction (Chapter 1) and a short conclusion (Chapter 8). The main findings and conclusions of the work are that: (i) groundwater recharge to the upland is almost certainly much larger than present abstractions; (ii) groundwater recharge to the floodplains is small compared to present regional shallow groundwater abstraction; (iii) development of shallow groundwater resources for irrigation in the Manga Grasslands would be most inadvisable because of resource limitations and salinity hazards; (iv) limited development of small scale irrigation, together with careful monitoring and modelling should go ahead in the Yobe fadana; (v) the remaining questions concerning the mechanisms and magnitude of groundwater recharge throughout the region need to be resolved a a matter of urgency; (vi) water allocation policy can be developed rationally, based on clear objectives and criteria, a good research base, and transparency of motive.

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Carter, R. "Water resources and water management in North East Nigeria". Thesis, Cranfield University, 1995. http://dspace.lib.cranfield.ac.uk/handle/1826/11117.

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Gelt, Joe, i Marv Waterstone. "Water Resources Research Center Serves the Arizona Water Community". Arizona-Nevada Academy of Science, 1988. http://hdl.handle.net/10150/296416.

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From the Proceedings of the 1988 Meetings of the Arizona Section - American Water Resources Association and the Hydrology Section - Arizona-Nevada Academy of Science - April 16, 1988, University of Arizona, Tucson, Arizona

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Joorabchi, Amirhassan. "Intelligent Predictive Models for Water resources Engineering". Thesis, Griffith University, 2009. http://hdl.handle.net/10072/367450.

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Fresh water is considered to be one of the most important resources for humans and the environment. Due to the increase in population and the currently unsustainable usage of this limited resource, more attention is needed in the management of water resources. Advanced computational methods can help in attaining a better understanding of all aspects of water. Indeed, a better understanding of water resources requires a vast knowledge of a wide variety of fields such as atmospheric science, geology, hydrology, hydraulics and mathematics etc. To assist in this process computing techniques have been widely applied in water resources engineering problems. An artificial neural network (ANN) has been applied to solve many engineering problems since the 1980s. However, there are still many engineering fields that have the potential to benefit from ANN, such as water resource engineering. In the present research two important applications; time-series prediction and function estimation for water resource engineering are investigated. Within water engineering the prediction of river discharge is important. The results can be used for many purposes including flooding management, risk assessment and saving lives. New techniques are always being sought to improve the accuracy of predictions. In the first part of this research a neural network model was developed as a tool for time-series prediction to forecast water flow discharge of Fitzroy River near Rockhampton in central Queensland. A feed-forward back-propagation network was selected to predict the daily time-series of the Fitzroy Rivers’ discharge at The Gap station, Queensland. The data was derived from the Queensland Department of Natural Resources and Mines. The two developed ANN models are investigated and compared after many trials with a number of inputs, outputs, hidden layers, learning rate and transfer functions. The final model uses the flow data for 15 successive days and then predicts the discharge for the next 4 days. The results show that an accurate prediction was obtained during flood events. The advantage of the ANN model, when compared to other numerical models, is that it only uses the historical data of the discharge from this particular river. Thus it is free of the need for other data such as rainfall data, topography of the area and stream sections. In addition, after the ANN was trained, a very fast prediction was obtained. Consequently, this model can be used as a real-time tool for flow forecasting in the Fitzroy River. Similar models could be developed, based on the structure of this ANN model, for any river in Australia and in the world. Another interesting problem in water resource engineering is groundwater dynamics that occur near the coast. Indeed, a knowledge of groundwater dynamics in coastal aquifers is important for understanding sediment transport processes in the swash zone; shoreline stability; the design of coastal structures close to beaches; water quality in closed coastal lakes and lagoons; the operation of dune sewage disposal and domestic water supply. Analytical methods or numerical models have been used to predict this groundwater table fluctuation due to tides, waves and precipitation etc. In the present study ANN is adopted to simulate groundwater table fluctuations. In the study a multilayer feed-forward neural network model has been developed and trained using a back-propagation algorithm. The training data was based on field measurements (KANG et al., 1994a) from five different locations down the east coast of Australia. The data included information on watertable, tide elevation, beach slopes and hydraulic conductivity at each beach. The results from the developed model show that the artificial neural network model is very successful in terms of the prediction of a target that is dependent on a number of variables. Sensitivity analysis was undertaken which confirmed that a variation in tide elevation is the most important parameter to use for simulating groundwater flow in coastal aquifers. In contrast the low number of training data available for hydraulic conductivity and beach slope did not have a significant effect on the prediction of groundwater table fluctuations in this model. Thus, to improve the accuracy of prediction for the developed model, more data should be collected.
Thesis (Masters)
Master of Philosophy (MPhil)
Griffith School of Engineering
Science, Environment, Engineering and Technology
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Schwarz, Mark Andrew. "Integrating Water Resources Into Land Use Planning: Connecting Local Land use Decisions and Water Resource Impacts". Thesis, The University of Arizona, 2007. http://hdl.handle.net/10150/190410.

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Water supply development has changed significantly in the last fifty years. Expanding existing water supplies or locating and securing new water supplies has become increasingly difficult and highly constrained. In addition, awareness of and experience with the deleterious environmental impacts of water supply development has further constrained future development. Given this new paradigm, it is imperative that growing areas identify water supplies to accommodate new development before the development occurs. This report provides an analysis of the physical and institutional characteristics of land use and water resource development in Pima County, Arizona. Using this analysis, policy recommendations are formulated to improve the County’s integration of land use and water resource planning. In the case of Pima County, a comprehensive plan water resources element is used as the policy vehicle for reforming public policies.

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Defenbaugh, Angela Lynn. "Evaluating Ohio River Basin Waters: A Water Quality and Water Resources Internship with the Ohio River Valley Water Sanitation Commission". Miami University / OhioLINK, 2014. http://rave.ohiolink.edu/etdc/view?acc_num=miami1389295851.

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Książki na temat "Water resources"

Lane, Alexander, Michael Norton i Sandra Ryan. Water Resources. Chichester, UK: John Wiley & Sons, Ltd, 2017. http://dx.doi.org/10.1002/9781118793985.

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Hanmer, Trudy J. Water resources. New York: F. Watts, 1985.

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Anisfeld, Shimon C. Water resources. Washington: Island Press, 2010.

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(Firm), National Geographic Learning, red. Water resources. Independence, KY]: National Geographic Learning, 2014.

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Geological Survey (U.S.). Water Resources Division. Colorado District, red. Water resources. [Denver, CO]: U.S. Geological Survey, Colorado District, 1995.

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Water resources. Washington: Island Press, 2010.

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Kay, Brian H. Water Resources. London: Taylor & Francis Group Plc, 2003.

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United States. Superintendent of Documents. Water pollution and water resources. Washington, D.C: U.S. G.P.O., Supt. of Docs., 1987.

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Water resources and water management. Amsterdam: Elsevier, 1987.

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United States. Superintendent of Documents. Water pollution and water resources. [Washington, D.C.]: U.S. G.P.O., Supt. of Docs., 1990.

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Części książek na temat "Water resources"

Rauschenbach, Thomas, Albrecht Gnauck, Oliver Krol, Thomas Bernard i Torsten Pfützenreuter. "Water Resources". W Modeling, Control and Optimization of Water Systems, 5–104. Berlin, Heidelberg: Springer Berlin Heidelberg, 2015. http://dx.doi.org/10.1007/978-3-642-16026-4_2.

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Biswas, Asit K. "Water Resources". W Water Resources of North America, 251–56. Berlin, Heidelberg: Springer Berlin Heidelberg, 2003. http://dx.doi.org/10.1007/978-3-662-10868-0_28.

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Oki, Taikan, i Pat J. F. Yeh. "Water Resources". W Encyclopedia of Remote Sensing, 903–9. New York, NY: Springer New York, 2014. http://dx.doi.org/10.1007/978-0-387-36699-9_193.

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Salameh, Elias, Musa Shteiwi i Marwan Al Raggad. "Water Resources". W Water Resources of Jordan, 9–59. Cham: Springer International Publishing, 2018. http://dx.doi.org/10.1007/978-3-319-77748-1_2.

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Sene, Kevin. "Water Resources". W Hydrometeorology, 383–409. Cham: Springer International Publishing, 2016. http://dx.doi.org/10.1007/978-3-319-23546-2_13.

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Krzysztofowicz, Roman. "Water Resources". W Encyclopedia of Operations Research and Management Science, 1635–39. Boston, MA: Springer US, 2013. http://dx.doi.org/10.1007/978-1-4419-1153-7_1122.

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Sene, Kevin. "Water Resources". W Hydrometeorology, 315–39. Dordrecht: Springer Netherlands, 2009. http://dx.doi.org/10.1007/978-90-481-3403-8_11.

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Stec, Agnieszka. "Water Resources". W Sustainable Water Management in Buildings, 13–19. Cham: Springer International Publishing, 2019. http://dx.doi.org/10.1007/978-3-030-35959-1_2.

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Booth, Colin A., i Susanne M. Charlesworth. "Water Resources". W Water Resources in the Built Environment, 1–7. Chichester, UK: John Wiley & Sons, Ltd, 2014. http://dx.doi.org/10.1002/9781118809167.ch1.

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Awange, Joseph. "Water Resources". W GNSS Environmental Sensing, 273–309. Cham: Springer International Publishing, 2017. http://dx.doi.org/10.1007/978-3-319-58418-8_14.

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Streszczenia konferencji na temat "Water resources"

Hossain, G. M. Akram, i Md Nurul Islam. "Water Resources Management in Bangladesh". W Joint Conference on Water Resource Engineering and Water Resources Planning and Management 2000. Reston, VA: American Society of Civil Engineers, 2000. http://dx.doi.org/10.1061/40517(2000)233.

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Le Fanic, R. "Water resources management in the bottled water business". W WATER RESOURCES MANAGEMENT 2009. Southampton, UK: WIT Press, 2009. http://dx.doi.org/10.2495/wrm090031.

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Festa, G., D. Verde i R. Magini. "Rehabilitation of a water distribution system with diffused water losses". W WATER RESOURCES MANAGEMENT 2009. Southampton, UK: WIT Press, 2009. http://dx.doi.org/10.2495/wrm090241.

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Hamer, W. G. "The cost of water and water markets in Southern California, USA". W WATER RESOURCES MANAGEMENT IV. Southampton, UK: WIT Press, 2007. http://dx.doi.org/10.2495/wrm070461.

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Westerling, David L. "Water Resources Development from a Congressional Viewpoint". W Joint Conference on Water Resource Engineering and Water Resources Planning and Management 2000. Reston, VA: American Society of Civil Engineers, 2000. http://dx.doi.org/10.1061/40517(2000)234.

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Desai, J., i S. K. Tank. "Studies on water quality index (WQI) of ground water of Surat City, India". W WATER RESOURCES MANAGEMENT 2011. Southampton, UK: WIT Press, 2011. http://dx.doi.org/10.2495/wrm110281.

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de Castro, P. Canelas. "Climate change and water management: is EU Water Law adapted to climate change?" W WATER RESOURCES MANAGEMENT 2011. Southampton, UK: WIT Press, 2011. http://dx.doi.org/10.2495/wrm110741.

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Symmonds, G. S. "Changing the water paradigm: how real-time data puts sustainability into water utilities". W WATER RESOURCES MANAGEMENT 2015. Southampton, UK: WIT Press, 2015. http://dx.doi.org/10.2495/wrm150141.

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Mecca, S. J., i S. D. Mecca. "Commercial water auditing in Stella". W WATER RESOURCES MANAGEMENT IV. Southampton, UK: WIT Press, 2007. http://dx.doi.org/10.2495/wrm070181.

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Bjornlund, H., A. Zuo, C. Parrack, S. Wheeler i R. de Loë. "Water reallocation policies: public perceptions". W WATER RESOURCES MANAGEMENT 2011. Southampton, UK: WIT Press, 2011. http://dx.doi.org/10.2495/wrm110521.

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Raporty organizacyjne na temat "Water resources"

Carlson, H., A. Pietroniro, P. Gober, W. Leger, S. Merrill, L. Balkhi, S. Foley, B. Halliday i L. Martz. Water resources. Natural Resources Canada/CMSS/Information Management, 2021. http://dx.doi.org/10.4095/328396.

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Matsumura-Tundisi, Takako, i José Galizia Tundisi. Water Resources Management. Editora Scienza, marzec 2018. http://dx.doi.org/10.26626/978-85-5953-031-5.2018b001.

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Brown, Thomas C., Romano Foti i Jorge Ramirez. Water resources (Chapter 12). Washington, DC: U.S. Department of Agriculture, Forest Service, Washington Office, 2012. http://dx.doi.org/10.2737/wo-gtr-87.

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Transboundary Water Resources Management and the Potential for Integrated Water Resources Management. American Museum of Natural History, 2011. http://dx.doi.org/10.5531/cbc.ncep.0015.

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Integrated Water Resources Management (IWRM) is an evolving concept used to address the difficult issues associated with making efficient and effective use of the world’s limited water resources. IWRM differs by country due to geography, culture, and stage of development, but generally involves the management of all water resources taking into account other natural resource management, as well as social, economic, environmental and technical issues. A significant issue in water management is the need for cooperation among nations sharing transboundary waters that may have different usage requirements. We look at the history, progress, and challenges in implementing IWRM in the management of transboundary water resources in three case studies: the Rhine River (Europe), the Mekong River (Southeast Asia), and the Zambezi River (Southern Africa).

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Integrated Water Resources Management in Latin America and the Caribbean. Inter-American Development Bank, grudzień 1998. http://dx.doi.org/10.18235/0008817.

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This technical study contains the strategy of the Inter-American Development Bank for its involvement in integrated water resources management in Latin America and the Caribbean. The strategy was developed through an iterative step by step procedure in consultation with country water resource officials, Bank staff, nongovernmental organizations, and international lending and technical assistance organizations. The first part of the study is an overview of water resource management in Latin America and the Caribbean and the second part is the Bank's strategy, including their goals and objectives, guiding principles and strategic instruments for integrated water resources management.

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Water resources of Massachusetts. US Geological Survey, 1992. http://dx.doi.org/10.3133/wri904144.

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Water Resources Data, Alaska, Water Year 2000. US Geological Survey, 2001. http://dx.doi.org/10.3133/wdrak001.

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Water Resources Data, Alaska, Water Year 2001. US Geological Survey, 2002. http://dx.doi.org/10.3133/wdrak011.

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Water resources data, Alaska, water year 2002. US Geological Survey, 2003. http://dx.doi.org/10.3133/wdrak021.

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Water resources data, Alaska, water year 2003. US Geological Survey, 2004. http://dx.doi.org/10.3133/wdrak031.

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