An examination of suspended sediment concentrations throughout the Ganges-Brahmaputra River System was conducted to assess the spatial variability of river sediment in the world’s largest sediment dispersal system. During the high-discharge monsoon season, suspended sediment concentrations vary widely throughout different geomorphological classes of rivers (main river channels, tributaries, and distributaries). An analysis of the sediment loads in these classes indicates that 7% of the suspended load in the system is diverted from the Ganges and Ganges-Brahmaputra rivers into southern distributaries. Suspended sediment concentrations are also used to calculate annual suspended sediment loads of the main river channels. These calculations show that the Ganges carries 262 million tons/year and the Brahmaputra carries 387 million tons/year. These calculations are lower than published values because of either interannual variability and/or sampling artifacts and assumptions in the homogeneity of flow and sediment concentration. The conjoined Ganges-Brahmaputra River carries 530 million tons annually, or only 80% of the sum of the loads that the Ganges and Brahmaputra rivers carry upstream of the confluence. The remaining 20% of sediment is diverted from the main river by the distributaries and deposited along the main river channel during overbank flooding. Suspended sediment concentration is also examined in the north-south oriented tidal channels on the Bay of Bengal to determine whether sediment is delivered to the channels by one of two pathways: (1) sediment is discharged into the Bay of Bengal by the main river channel, carried west by coastal currents, and advected northward into the channels by tidal currents or (2) diverted from the main river bed through the distributaries, migrating southward into the tidal channels. Suspended sediment concentration and salinity data are inconclusive in determining sediment source. Beryllium-7 radioisotope data indicate that newly transported sediment is present in the tidal channels and offshore despite values in the Ganges and Ganges-Brahmaputra rivers being below detection. Sampling artifacts are likely caused by the below detection readings in the Ganges and Ganges-Brahmaputra rivers. Newly transported sediment is observed in a distributary south of the Ganges River and indicates that sediment is actively being transported to the distributary region.

An examination of suspended sediment concentrations throughout the Ganges-Brahmaputra River System was conducted to assess the spatial variability of river sediment in the world’s largest sediment dispersal system. During the high-discharge monsoon season, suspended sediment concentrations vary widely throughout different geomorphological classes of rivers (main river channels, tributaries, and distributaries). An analysis of the sediment loads in these classes indicates that 7% of the suspended load in the system is diverted from the Ganges and Ganges-Brahmaputra rivers into southern distributaries. Suspended sediment concentrations are also used to calculate annual suspended sediment loads of the main river channels. These calculations show that the Ganges carries 262 million tons/year and the Brahmaputra carries 387 million tons/year. These calculations are lower than published values because of either interannual variability and/or sampling artifacts and assumptions in the homogeneity of flow and sediment concentration. The conjoined Ganges-Brahmaputra River carries 530 million tons annually, or only 80% of the sum of the loads that the Ganges and Brahmaputra rivers carry upstream of the confluence. The remaining 20% of sediment is diverted from the main river by the distributaries and deposited along the main river channel during overbank flooding. Suspended sediment concentration is also examined in the north-south oriented tidal channels on the Bay of Bengal to determine whether sediment is delivered to the channels by one of two pathways: (1) sediment is discharged into the Bay of Bengal by the main river channel, carried west by coastal currents, and advected northward into the channels by tidal currents or (2) diverted from the main river bed through the distributaries, migrating southward into the tidal channels. Suspended sediment concentration and salinity data are inconclusive in determining sediment source. Beryllium-7 radioisotope data indicate that newly transported sediment is present in the tidal channels and offshore despite values in the Ganges and Ganges-Brahmaputra rivers being below detection. Sampling artifacts are likely caused by the below detection readings in the Ganges and Ganges-Brahmaputra rivers. Newly transported sediment is observed in a distributary south of the Ganges River and indicates that sediment is actively being transported to the distributary region.

Thesis (Ph. D.)--University of Wisconsin--Madison, 1941. / Typescript. Includes abstract and vita. eContent provider-neutral record in process. Description based on print version record. Includes bibliographical references (leaves 442-458).

This thesis examines the applicability of the Murray-Darling Basin (MDB) model of Integrated River Basin Management to the Ganges Basin by utilising the lessons from the Mekong experience of adopting the MDB model. The Ganges is one of the major rivers in the world and the sharing of its water has long been an issue of dispute between the riparian countries. Fragmented and uncoordinated upstream management of the Ganges has caused serious ecological and economic loss in the downstream environment posing a threat to future sustainability of river resources. Cooperation among the riparian countries of the Ganges in order to embrace an integrated and basin-wide management approach is rapidly becoming more important. Integrated River Basin Management (IRBM) is a concept widely advocated in different forums for managing the river basins of the world and is adopted in many transboundary river basins. The Australian example of managing the Murray-Darling Basin is considered as a model in the field. The Murray-Darling Basin Commission is well known internationally as a good example of a multi-jurisdictional water management institution. Similar river basin institutions are also evolving in other regions such as the Mekong River Commission for the management of the Mekong River in South-East Asia. The countries sharing the Ganges could learn lessons from the Murray-Darling and Mekong experiences and adopt a basin-wide approach for the better management of the Ganges. However, the policy transfer from a developed country to a developing country context is a challenging process. The highly pertinent contextual differences in social, economic, political, environmental and hydrological settings of the three cases need to be carefully addressed. The research critically examines these factors in the Murray-Darling, Mekong and the Ganges contexts, identifies the similarities and differences between them and attempts to understand the influence/s of these in the policy transfer or policy development process. This research adopted multiple-case studies involving both qualitative and quantitative methods. The cases of the Murray-Darling and Mekong were studied to understand the process and to utilise the lessons learned for the institutional development towards integrated and basin-wide approach for the Ganges. The study analyses the interview results from the experts in the relevant fields to get an insight of different issues and also to collect their opinions. The responses from the stakeholder interviews in Bangladesh were analysed to understand their perspective in this regard. The thesis concludes that adoption of the Murray-Darling Basin model of integrated management needs modification in the Ganges context and recommends a specific institutional structure for the basin-wide management of the Ganges. The thesis contributes to an area of knowledge in recent times by providing a greater understanding of the Integrated River Basin Management in a multi-jurisdictional context. It critically examines the issues in policy transfer from a developed to a developing country focussing on a little studied but significant international river basin, the Ganges. It is hoped that this thesis will contribute towards better policy options for the sustainable management of the international river system. / http://proxy.library.adelaide.edu.au/login?url= http://library.adelaide.edu.au/cgi-bin/Pwebrecon.cgi?BBID=1321536 / Thesis (Ph.D.) - University of Adelaide, School of Social Sciences, 2008

This paper studies if the Flagship Namami Gange program of Cleaning the river Ganges in India aligns with the transcendental discourse on the river. Web contents as Facebook, YouTube and Twitter along with Indian English daily newspaper reports are used here as the source of data. The study shows that the program aligns with the transcendental discourse on river Ganges as the Mother Goddess and reaching out to her devotees.

Thesis (M.A.)--University of North Texas, May, 2007. / Title from title page display. Includes bibliographical references.

This thesis sets out to develop a beginning of a philosophy of water by considering philosophical implications of ecological crises currently happening along the waters of the Ganges River. In my first chapter, I give a historical account of a philosophy of water. In my second chapter, I describe various natural and cultural representations of the Ganges, accounting for physical features of the river, Hindu myths and rituals involving the river, and ecological crises characterized by the pollution and damming of the river. In my third and final chapter, I look into the philosophical implications of these crises in terms of the works of the contemporary philosopher Bruno Latour.

Climate change is affecting several environmental factors and together with socio-economic changes put high pressure on water resources. Climate change manifest itself through increasing temperatures and changes in precipitation patterns and intensities, with knock-on effects on hydrologically-relevant parameters such as water flows, evapotranspiration rates, glacial melt etcetera, all of which have already been observed in the recent past and are predicted to continue in the future. India has the world’s second largest population. The majority of the population live in rural areas and are dependent on climate sensitive sectors such as agriculture, forestry and fishery. The Indian-Himalayan region supplies 600 million people with water, thus future climate change impacts on the hydrological cycle in the area are of great interest and concern. In order to cope with these predicted impacts, there is a need to adapt to the changing climate. This study combines data analyses from a hydro-climatic modelling campaign (carried out externally to this thesis), a literature review on climate change effects on agriculture and opportunities to adapt to these effects and participatory methods bringing stakeholders and scientists together in order to co-create adaptation options that are suitable to minimise short- and long-term climate change impacts on the water flows of the Ganges and hence agriculture in the region. The study concentrates on two districts in the Indo-Gangetic Plain that are characterised by their high dependency on the farming sector: Uttarkashi (upstream Ganges, Uttarakhand) and Patna (downstream Ganges, Bihar). The analysis of hydro-climatic data based on a modelling campaign focussed on three climate variables that are of significance for agriculture: precipitation, temperature, and evapotranspiration. To characterise future climates, four climate change projections based on IPCC’s representative concentrations pathways (RCPs) have been chosen: RCP 2.6, RCP 4.5, RCP 6.0, and RCP 8.5. The impacts of these scenarios on the above listed three climate variables are analysed over three time periods: 2011-2040, 2041-2070, and 2071-2100, with a special focus on the monsoon months from June to October, as this is the main crop (rice) growing season. The results from the hydro-climatic modelling indicate that the maximum, minimum, and average temperature will be increasing over the next century in both districts. An increase in evapotranspiration can be seen for both districts, with a few exceptions for RCP scenarios 2.6, 6.0 and 8.5 in April and May in Patna, and for all RCP scenarios in April, May and June in Uttarkashi. An increase in maximum and average precipitation can be seen for most RCP scenarios and future time periods (e.g. of exceptions in average precipitation: RCP 4.5 and 8.5 in June and July in the period 2011-2040) during the monsoon period in Patna. Similarly, in Uttarkashi maximum and average precipitation increases for all three time periods and RCP scenarios during the monsoon months of September and August (only for RCP scenarios 2.6 and 8.5). For the remaining months, the precipitation patterns show great variability for all scenarios and both regions. The literature review resulted in a table of adaptation options, where nine out of 63 were considered as transformational adaptation, and enabled identification of possible climate change impacts on agriculture in the two districts. The minimum temperature could result in more severe and intense hailstorms in the future for both districts. The increase in temperature could lead to a prolonged growing season in Uttarkashi, whilst the increase in average and maximum temperature in Patna could lead to heat-stress for the crops. Furthermore, the increase in average and maximum precipitation could lead to more severe and intense natural disasters e.g. landslides in Uttarkashi and floods in Patna. Moreover, the increase in average evapotranspiration combined with the decrease in average precipitation during some months could lead to an increasing need of irrigation. Two workshops were held in the region with the aim to bring together researchers and stakeholders (e.g. famers) in order to jointly discuss 1) the suitability of hydrological modelling data for preparing the agriculture sector to a changing climate, and 2) suggest suitable adaptation options based on researchers’ and stakeholders’ knowledge and experience. Information from the first workshop was obtained by a workshop report, whilst information from the second workshop was obtained from the author’s own participation. The result from the workshop showed that the farmers had several suggestions of suitable adaptation options e.g. implementation of irrigation system and improved access to credit. It also showed that the farmers already adapted to climate change e.g. usage of short- and long duration variations of rice and sowing date adjustment. The combination of these results informed the suggestions for adaptation options for the two districts, namely the development of disaster reduction plans and early warning systems for weather extremes, as well as a diversification of agriculture and more generally livelihoods. In addition, indirect adaptation measures suggested for both districts included insurance schemes against yield failure, improved access to credit schemes, and right/fair market prices. Specific measures for each district were also suggested e.g. heat-tolerant crops in Patna and implementation or irrigation systems in Uttarkashi. / Klimatförändringarna påverkar åtskilliga miljöfaktorer och tillsammans med socioekonomiska förändringar sätter de stort tryck på vattenresurser. Klimatförändringar manifesterar sig i stigande temperaturer och ändrade nederbördsmönster och nederbördsintensitet, med påföljande effekter på hydrologiskt relevanta parametrar så som vattenflöden, evapotranspirationsvärden, smältande glaciärer etcetera, vilka alla är effekter som redan observerats och är förutspådda att fortsätta under innevarande århundrande. Befolkningen i Indien är näst störst i världen. Större delen av befolkningen i Indien bor på landsbygden och är beroende av klimatkänsliga sektorer så som jordbruk, fiske och skogsbruk. Indiska Himalaya förser 600 miljoner människor med vatten, framtida effekter på den hydrologiska cykeln, orsakade av klimatförändringarna i området, är därför av största intresse. För att kunna hantera de framtida effekterna orsakade av klimatförändringarna är det viktigt att implementera klimatanpassningsstrategier. Den här studien kombinerar data analyser från en hydro-klimatisk modelleringskampanj (som är genomförd externt till det här arbetet), litteraturstudie över effekter på jordbruk orsakade av klimatförändringar och möjligheter att anpassa sig till dessa förändringar, samt involverar preferenser och kunskaper från intressenter inom det aktuella området för att kunna identifiera lämpliga klimatanpassningsstrategier. Studien har ett huvudfokus på klimatanpassning för jordbruksområden i två distrikt i Indien: Uttarkashi (uppströms Ganges, Uttarakhand) och Patna (nedströms Ganges, Bihar). Analysen av hydro-klimatisk data, baserad på en modelleringskampanj, fokuserar på tre klimatvariabler som är av betydelse för jordbrukssektor: nederbörd, temperatur, och evapotranspiration. För att kunna karakterisera framtida klimat har IPCCs fyra representativa koncentrationsvägar (RCPs) tagits hänsyn till: RCP 2.6, RCP 4.5, RCP 6.0, och RCP 8.5. Effekterna av dessa scenarier på de tre ovan listade klimatvariablerna är analyserade över tre framtida tidsperioder: 2011-2040, 2041-2070, 2071-2100, med ett speciellt fokus på monsunperioden från juni till oktober. Resultatet från analysen av hydro-klimatisk data indikerar en ökning under århundrandet i minimal, maximal, och genomsnittlig temperatur i båda distrikten. En ökning i evapotranspiration för båda distrikten kunde också identifieras, med några få undantag för RCP 2.6, 6.0 och 8.5 i april och maj i Patna, samt för alla RCP scenarier i april, maj och juni för Uttarkashi. Trender i nederbörd visar en ökning i maximal och genomsnittlig nederbörd för nästan alla scenarier under monsunperioden i Patna (exempel på scenarier där den genomsnittliga nederbörden inte ökar är RCP 4.5 och 8.5 i juni och juli under perioden 2011-2040). En ökning i maximal och genomsnittlig nederbörd identifierades i september för alla RCP scenarier och framtidsperioder, samt i augusti för RCP 2.6 och 8.5 i Uttarkashi. Kvarvarande månader visar på stor variabilitet i nederbörd för alla scenarier i båda distrikten. Litteraturstudien resulterade i en tabell med klimatanpassningsstrategier, där nio av 63 ansågs vara transformerande, samt identifierade möjliga effekter på jordbruket i de två distrikten orsakade av klimatförändringar. Ökningen i minimal temperatur kan leda till mer allvarliga och intensifierade hagelstormar i framtiden. Temperaturökningen kan i Uttarkashi leda till förlängd odlingssäsong medan ökningen i genomsnittlig och maximal temperatur kan leda till värmestress på grödorna i Patna. Vidare gäller att ökningen i maximal och genomsnittlig nederbörd kan leda till mer allvarliga naturkatastrofer i framtiden som exempelvis jordskred i Uttarkashi och översvämningar i Patna. Ökningen i evapotranspiration kombinerat med minskningen i genomsnittlig nederbörd under vissa månader skulle kunna leda till ett ökat bevattningsbehov. Två ”worskhops” anordnades i regionen med målet att sammanföra forskare och intressenter (exempelvis bönder) för att gemensamt diskutera 1) lämpligheten av användandet av hydrologiskt modellerad data för att förbereda jordbruket på klimatförändringar, och 2) föreslå lämpliga klimatanpassningsstrategier baserat på forskarnas och intressenternas kunskap och erfarenheter. Informationen från den första workshopen erhölls genom en workshoprapport, medan informationen i den andra workshopen erhölls genom författarens eget deltagande i workshopen. Resultatet från workshopen visade på att bönderna hade flertalet egna föreslag vad gäller lämpliga klimatanpassningsstrategier så som exempelvis implementerande av bevattningssystem och ökade kreditmöjligheter. Bönderna hade även börjat anpassa sig till klimatförändringar genom exempelvis ha lång- och korttids variationer av ris samt att de hade flyttat på datumet för sådden. Kombinationen av hydro-klimatisk data, litteratur och intressentpreferenser och kunskap möjliggjorde förslag på klimatanpassningsstrategier i de två distrikten. Strategier för att reducera skador på grödor och jordbruksmark orsakade av extrema händelser, varningssystem som varnar i ett tidigt skede, och diversifiering av försörjning är direkta klimatanpassningsstrategier som identifierades för båda distrikten. Försäkringslösningar, ökade kreditmöjligheter, och ett rättvist marknadspris var indirekta anpassningsstrategier som identifierats för båda distrikten. Även specifika anpassningsstrategier för respektive distrikt har identifierats, där exempelvis värme-tåliga grödor identifierades som viktigt för Patna och implementering av bevattningssystem identifierades som extra viktigt för Uttarkashi.

A simple correlation analysis was used to investigate the linear relationships between sea surface temperature (SST) and monthly flow of Ganges and Brahmaputra at the borders of Bangladesh and India using approximately 50 years of river discharge data. Strong correlations were found between the equatorial Pacific SST and boreal summer Ganges discharge from three-month lag to two-month lead times. The El Nio-Southern Oscillation (ENSO) explains Ganges flow variance exceeding 0.95 significance level using both the Nino 3.4 SST correlation and the composites made for El Nio (La Nina) periods. The May SST of the southwest Pacific Ocean to the east of Australia continent has a strong correlation (>0.6) with early summer Ganges discharges. Using a lag correlation analysis of Ganges discharge and SST, we found a steady and continuous development in the Nino 3.4 SST relationship, and a strong correlation with the southwest Pacific SST which is most pronounced three-four months prior to the onset of Asian summer monsoon. These relationships mean that at least 25% of the interannual summer Ganges River discharge variability can be explained by antecedent equatorial and southwest Pacific SST. It provides a possible statistical method for linear forecasting two or three months in advance. The Brahmaputra River discharge, on the other hand, shows weak relationships with tropical SST variability except for the Bay of Bengal and the higher northern latitudes of the Pacific.

Automatic river quality monitoring (ARQM) is potentially an important tool in water quality management for the National Rivers Authority (NRA) and similar organisations worldwide. The information produced by ARQM systems must be used in the most effective way and fully integrated with the manual monitoring effort. The status and development of ARQM systems in the freshwater and estuarine River Thames catchment are discussed and a practical appraisal of the design, operation and maintenance requirements given. Data capture, verification and presentation methods are developed and the use of ARQM data for real time management and subsequent analysis is advocated. Examples of data from the freshwater ARQM system are given which emphasise the variability of freshwater quality and the need for a comprehensive understanding of the behaviour of rivers before management decisions are made. The use of ARQM data for assessing the compliance of rivers with River Quality Objectives is examined. With respect to the tidal Thames, data processing methods to correct for the tidal movement of the waterbody are developed. ARQM data are used to highlight the principal factors affecting the water quality of the tidal Thames. The importance of the use of ARQM information in the effective management of the tidal Thames is discussed and operational examples demonstrate how it may be utilised as a basis for management decisions. The application of ARQM to the sub-tropical environment of the River Ganges, India, is investigated. An ARQM system has been designed and prototypes are operational. Extensive site surveys were carried out and the water quality status of the Ganges is discussed. Recommendations for the improvement and future development of ARQM systems are made. The use of ARQM information and its potential for improving the management of rivers is discussed.