Executive Summary of Ghaghara-Yamuna
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Flood Management Strategy for Ganga Basin Through Storage
Flood Management Strategy for Ganga Basin through Storage by N. K. Mathur, N. N. Rai, P. N. Singh Central Water Commission Introduction The Ganga River basin covers the eleven States of India comprising Bihar, Jharkhand, Uttar Pradesh, Uttarakhand, West Bengal, Haryana, Rajasthan, Madhya Pradesh, Chhattisgarh, Himachal Pradesh and Delhi. The occurrence of floods in one part or the other in Ganga River basin is an annual feature during the monsoon period. About 24.2 million hectare flood prone area Present study has been carried out to understand the flood peak formation phenomenon in river Ganga and to estimate the flood storage requirements in the Ganga basin The annual flood peak data of river Ganga and its tributaries at different G&D sites of Central Water Commission has been utilised to identify the contribution of different rivers for flood peak formations in main stem of river Ganga. Drainage area map of river Ganga Important tributaries of River Ganga Southern tributaries Yamuna (347703 sq.km just before Sangam at Allahabad) Chambal (141948 sq.km), Betwa (43770 sq.km), Ken (28706 sq.km), Sind (27930 sq.km), Gambhir (25685 sq.km) Tauns (17523 sq.km) Sone (67330 sq.km) Northern Tributaries Ghaghra (132114 sq.km) Gandak (41554 sq.km) Kosi (92538 sq.km including Bagmati) Total drainage area at Farakka – 931000 sq.km Total drainage area at Patna - 725000 sq.km Total drainage area of Himalayan Ganga and Ramganga just before Sangam– 93989 sq.km River Slope between Patna and Farakka about 1:20,000 Rainfall patten in Ganga basin -
Estimation of Paleo-Discharge of the Lost Saraswati River, North West India
EGU2020-21212 https://doi.org/10.5194/egusphere-egu2020-21212 EGU General Assembly 2020 © Author(s) 2021. This work is distributed under the Creative Commons Attribution 4.0 License. Estimation of paleo-discharge of the lost Saraswati River, north west India Zafar Beg, Kumar Gaurav, and Sampat Kumar Tandon Indian Institute of Science Education and Research Bhopal, Earth and Environment Sciences, India ([email protected], [email protected], [email protected] ) The lost Saraswati has been described as a large perennial river which was 'lost' in the desert towards the end of the 'Indus-Saraswati civilisation'. It has been suggested that this paleo river flowed in the Sutlej-Yamuna interfluve, parallel to the present-day Indus River. Today, in this interfluve an ephemeral river- the Ghaggar flows along the abandoned course of the ‘lost’ Saraswati River. We examine the hypothesis given by Yashpal et al. (1980) that two Himalayan-fed rivers Sutlej and Yamuna were the tributaries of the lost Saraswati River, and constituted the bulk of its paleo-discharge. Subsequently, the recognition of the occurrence of thick fluvial sand bodies in the subsurface and the presence of a large number of Harappan sites in the interfluve region have been used to suggest that the Saraswati River was a large perennial river. Further, the wider course of about 4-7 km recognised from satellite imagery of Ghaggar-Hakra belt in between Suratgarh and Anupgarh in the Thar strengthens this hypothesis. In this study, we have developed a methodology to estimate the paleo-discharge and paleo- width of the lost Saraswati River. -
The Conservation Action Plan the Ganges River Dolphin
THE CONSERVATION ACTION PLAN FOR THE GANGES RIVER DOLPHIN 2010-2020 National Ganga River Basin Authority Ministry of Environment & Forests Government of India Prepared by R. K. Sinha, S. Behera and B. C. Choudhary 2 MINISTER’S FOREWORD I am pleased to introduce the Conservation Action Plan for the Ganges river dolphin (Platanista gangetica gangetica) in the Ganga river basin. The Gangetic Dolphin is one of the last three surviving river dolphin species and we have declared it India's National Aquatic Animal. Its conservation is crucial to the welfare of the Ganga river ecosystem. Just as the Tiger represents the health of the forest and the Snow Leopard represents the health of the mountainous regions, the presence of the Dolphin in a river system signals its good health and biodiversity. This Plan has several important features that will ensure the existence of healthy populations of the Gangetic dolphin in the Ganga river system. First, this action plan proposes a set of detailed surveys to assess the population of the dolphin and the threats it faces. Second, immediate actions for dolphin conservation, such as the creation of protected areas and the restoration of degraded ecosystems, are detailed. Third, community involvement and the mitigation of human-dolphin conflict are proposed as methods that will ensure the long-term survival of the dolphin in the rivers of India. This Action Plan will aid in their conservation and reduce the threats that the Ganges river dolphin faces today. Finally, I would like to thank Dr. R. K. Sinha , Dr. S. K. Behera and Dr. -
Conceptual Model for the Vulnerability Assessment of Springs in the Indian Himalayas
climate Article Conceptual Model for the Vulnerability Assessment of Springs in the Indian Himalayas Denzil Daniel 1 , Aavudai Anandhi 2 and Sumit Sen 1,3,* 1 Centre of Excellence in Disaster Mitigation and Management, Indian Institute of Technology Roorkee, Roorkee 247667, India; [email protected] 2 Biological Systems Engineering Program, College of Agriculture and Food Sciences, Florida A&M University, Tallahassee, FL 32307, USA; [email protected] 3 Department of Hydrology, Indian Institute of Technology Roorkee, Roorkee 247667, India * Correspondence: [email protected]; Tel.: +91-1332-284754 Abstract: The Indian Himalayan Region is home to nearly 50 million people, more than 50% of whom are dependent on springs for their sustenance. Sustainable management of the nearly 3 million springs in the region requires a framework to identify the springs most vulnerable to change agents which can be biophysical or socio-economic, internal or external. In this study, we conceptualize vulnerability in the Indian Himalayan springs. By way of a systematic review of the published literature and synthesis of research findings, a scheme of identifying and quantifying these change agents (stressors) is presented. The stressors are then causally linked to the characteristics of the springs using indicators, and the resulting impact and responses are discussed. These components, viz., stressors, state, impact, and response, and the linkages are used in the conceptual framework to assess the vulnerability of springs. A case study adopting the proposed conceptual model is discussed Citation: Daniel, D.; Anandhi, A.; for Mathamali spring in the Western Himalayas. The conceptual model encourages quantification Sen, S. -
Current Condition of the Yamuna River - an Overview of Flow, Pollution Load and Human Use
Current condition of the Yamuna River - an overview of flow, pollution load and human use Deepshikha Sharma and Arun Kansal, TERI University Introduction Yamuna is the sub-basin of the Ganga river system. Out of the total catchment’s area of 861404 sq km of the Ganga basin, the Yamuna River and its catchment together contribute to a total of 345848 sq. km area which 40.14% of total Ganga River Basin (CPCB, 1980-81; CPCB, 1982-83). It is a large basin covering seven Indian states. The river water is used for both abstractive and in stream uses like irrigation, domestic water supply, industrial etc. It has been subjected to over exploitation, both in quantity and quality. Given that a large population is dependent on the river, it is of significance to preserve its water quality. The river is polluted by both point and non-point sources, where National Capital Territory (NCT) – Delhi is the major contributor, followed by Agra and Mathura. Approximately, 85% of the total pollution is from domestic source. The condition deteriorates further due to significant water abstraction which reduces the dilution capacity of the river. The stretch between Wazirabad barrage and Chambal river confluence is critically polluted and 22km of Delhi stretch is the maximum polluted amongst all. In order to restore the quality of river, the Government of India (GoI) initiated the Yamuna Action Plan (YAP) in the1993and later YAPII in the year 2004 (CPCB, 2006-07). Yamuna river basin River Yamuna (Figure 1) is the largest tributary of the River Ganga. The main stream of the river Yamuna originates from the Yamunotri glacier near Bandar Punch (38o 59' N 78o 27' E) in the Mussourie range of the lower Himalayas at an elevation of about 6320 meter above mean sea level in the district Uttarkashi (Uttranchal). -
Environmental Assessment and Environmental Management Framework for the State of Bihar
Project Draft EMF Report Environmental Assessment and Environmental Management Framework for the state of Bihar Draft Final Report (version 2) Submitted to Chief Engineer (Urban)-Cum-Member Secretary, Executive Committee, Bihar State Water and Sanitation Mission (BSWSM) (Public Health Engineering Department, Govt. of Bihar) Vishveshwariya Bhawan, Bailey Road, Patna-800001 Environmental Assessment and Environmental Management Framework for the state of Bihar © The Energy and Resources Institute 2013 Suggested format for citation T E R I. 2013 Inception Report for study on “Environmental Assessment and Environmental Management Framework for the state of Bihar” New Delhi: The Energy and Resources Institute. Contact Details Anshuman Associate Director (Water Resources) T E R I Tel. 2468 2100 or 2468 2111 Darbari Seth Block E-mail [email protected] IHC Complex, Lodhi Road Fax 2468 2144 or 2468 2145 New Delhi – 110 003 Web www.teriin.org India +91 • Delhi (0)11 ii Environmental Assessment and Environmental Management Framework for the state of Bihar Table of Contents _Toc352602516 Abbreviations .................................................................................................................... 1 Executive Summary ......................................................................................................... 3 1. Introduction ............................................................................................................... 15 1.1 Background .................................................................................................................... -
Team ( For) Team ( Against) Topic Slot JUDGES Mississipi
Team ( for) Team ( Against) Topic Slot JUDGES Are parents to be held responsible for the actions of their Mississipi - thames Kaveri children? 10:00-10:30 Aparna-Ananya Should MLAs and MPs should have a minimum level of Yamuna - tapi Krishna educational qualification? 17 apil- 10:00-10:30 prashasti-jay sandhiya- Mahanadhi Tigris Is Indian culture decaying? 5:00- 5:30 shailendra Should we make cartoons and TV a part of the educational Koshi Narmada process in elementary school? 10:45-11:15 shrishty-shivam Homework at school: should be banned or it is an essential Rupnarayan Sindhu part of our studies that teaches us to work independently. 11:30-12:00 Aparna-Ananya Jordan Jhelum - Indus Social media has improved human communication and reach. 11:30-12:00 prashasti-jay Patriotism is doing more harm than good when it comes to sandhiya- Danube Betwa International relations. 12:15-12:45 shailendra Government shouldn't have the access to personal information Colorado Brahmaputra of citizens through the linking of Adhaar. 12:15-12:45 shrishty-shivam Alknanda Tista Does 'NOTA' option in elections really make sense? 1:00-1:30 Aparna-Ananya Tests on animals: should animals be used for scientific Godavari Shinano achievements 1:00-1:30 Prashasti-jay sandhiya- Amazon Irtysh Film versions are never as good as the original books. 1:30-2:00 shailendra Sutlej Gandak Zoos should be banned. 1:30-2:00 shrishty-shivam Ganga Umngot Online system of education is a boon than a bane. 2:00-2:30 Aparna-Ananya zambezi- WILD CARD Team Team Winning Slot Jugdes Topics Social media comments should be Mississipi + Thames Kaveri Kaveri (A) 12:00- 12:30 p.m. -
On the Brink: Water Governance in the Yamuna River Basin in Haryana By
Water Governance in the Yamuna River Basin in Haryana August 2010 For copies and further information, please contact: PEACE Institute Charitable Trust 178-F, Pocket – 4, Mayur Vihar, Phase I, Delhi – 110 091, India Society for Promotion of Wastelands Development PEACE Institute Charitable Trust P : 91-11-22719005; E : [email protected]; W: www.peaceinst.org Published by PEACE Institute Charitable Trust 178-F, Pocket – 4, Mayur Vihar – I, Delhi – 110 091, INDIA Telefax: 91-11-22719005 Email: [email protected] Web: www.peaceinst.org First Edition, August 2010 © PEACE Institute Charitable Trust Funded by Society for Promotion of Wastelands Development (SPWD) under a Sir Dorabji Tata Trust supported Water Governance Project 14-A, Vishnu Digambar Marg, New Delhi – 110 002, INDIA Phone: 91-11-23236440 Email: [email protected] Web: www.watergovernanceindia.org Designed & Printed by: Kriti Communications Disclaimer PEACE Institute Charitable Trust and Society for Promotion of Wastelands Development (SPWD) cannot be held responsible for errors or consequences arising from the use of information contained in this report. All rights reserved. Information contained in this report may be used freely with due acknowledgement. When I am, U r fine. When I am not, U panic ! When I get frail and sick, U care not ? (I – water) – Manoj Misra This publication is a joint effort of: Amita Bhaduri, Bhim, Hardeep Singh, Manoj Misra, Pushp Jain, Prem Prakash Bhardwaj & All participants at the workshop on ‘Water Governance in Yamuna Basin’ held at Panipat (Haryana) on 26 July 2010 On the Brink... Water Governance in the Yamuna River Basin in Haryana i Acknowledgement The roots of this study lie in our research and advocacy work for the river Yamuna under a civil society campaign called ‘Yamuna Jiye Abhiyaan’ which has been an ongoing process for the last three and a half years. -
Satellite Imagery Evaluation of Soil Moisture Variability in North-East Part of Ganges Basin, India Proma Bhattacharyya
University of New Mexico UNM Digital Repository Earth and Planetary Sciences ETDs Electronic Theses and Dissertations 1-30-2013 Satellite imagery evaluation of soil moisture variability in north-east part of Ganges Basin, India Proma Bhattacharyya Follow this and additional works at: https://digitalrepository.unm.edu/eps_etds Recommended Citation Bhattacharyya, Proma. "Satellite imagery evaluation of soil moisture variability in north-east part of Ganges Basin, India." (2013). https://digitalrepository.unm.edu/eps_etds/6 This Thesis is brought to you for free and open access by the Electronic Theses and Dissertations at UNM Digital Repository. It has been accepted for inclusion in Earth and Planetary Sciences ETDs by an authorized administrator of UNM Digital Repository. For more information, please contact [email protected]. i Satellite Imagery Evaluation of Soil Moisture Variability in North-East part of Ganges Basin, India By Proma Bhattacharyya B.Sc Geology, University of Calcutta, India, 2007 M.Sc Applied Geology, Presidency College-University of Calcutta, 2009 THESIS Submitted in Partial Fulfillment of the Requirements for the Degree of Master of Science Earth and Planetary Sciences The University of New Mexico, Albuquerque, New Mexico Graduation Date – December 2012 ii ACKNOWLEDGMENTS I heartily acknowledge Dr. Gary W. Weissmann, my advisor and dissertation chair, for continuing to encourage me through the years of my MS here in the University of New Mexico. His guidance will remain with me as I continue my career. I also thank my committee members, Dr. Louis Scuderi and Dr. Grant Meyer for their valuable recommendations pertaining to this study. To my parents and my fiancé, thank you for the many years of support. -
Ganga As Perceived by Some Ganga Lovers Mother Ganga's Rights Are Our Rights
Ganga as Perceived by Some Ganga Lovers Mother Ganga’s Rights Are Our Rights Pujya Swami Chidanand Saraswati Nearly 500 million people depend every day on the Ganga and Her tributaries for life itself. Like the most loving of mothers, She has served us, nourished us and enabled us to grow as a people, without hesitation, without discrimination, without vacation for millennia. Regardless of what we have done to Her, the Ganga continues in Her steady fl ow, providing the waters that offer nourishment, livelihoods, faith and hope: the waters that represents the very life-blood of our nation. If one may think of the planet Earth as a body, its trees would be its lungs, its rivers would be its veins, and the Ganga would be its very soul. For pilgrims, Her course is a lure: From Gaumukh, where she emerges like a beacon of hope from icy glaciers, to the Prayag of Allahabad, where Mother Ganga stretches out Her glorious hands to become one with the Yamuna and Saraswati Rivers, to Ganga Sagar, where She fi nally merges with the ocean in a tender embrace. As all oceans unite together, Ganga’s reach stretches far beyond national borders. All are Her children. For perhaps a billion people, Mother Ganga is a living goddess who can elevate the soul to blissful union with the Divine. She provides benediction for infants, hope for worshipful adults, and the promise of liberation for the dying and deceased. Every year, millions come to bathe in Ganga’s waters as a holy act of worship: closing their eyes in deep prayer as they reverently enter the waters equated with Divinity itself. -
Hydrothermal Source of Radiogenic Sr to Himalayan Rivers
Hydrothermal source of radiogenic Sr to Himalayan rivers Matthew J. Evans Department of Geological Sciences, Cornell University, Ithaca, New York 14853-1504, USA Louis A. Derry Suzanne P. Anderson Department of Earth Sciences, University of California, Santa Cruz, California 95064, USA Christian France-Lanord Centre des Recherches PeÂtrographiques et GeÂochimiques, BP 20, Vandouvre-les-Nancy, 54501, France ABSTRACT ment; formations III and II of the crystallines Hot-spring waters near the Main Central thrust in the Marsyandi River of central Nepal are composed of calcic gneisses and marbles have Sr concentrations to 115 mM with 87Sr/86Sr to 0.77. Small amounts of hydrothermal as well as pelitic augen gneisses, and forma- water (#1% of total river discharge) have a signi®cant impact on the solute chemistry tion I contains mainly quartzo-pelitic gneisses and the budget of radiogenic Sr in the Marsyandi. In the upper Marsyandi, river chem- and some migmatites. The Manaslu leuco- istry re¯ects carbonate weathering, with 87Sr/86Sr # 0.72. As the Marsyandi ¯ows across granite is exposed in the northeastern part of the dominantly silicate High Himalayan Crystalline terrane, both 87Sr/86Sr and [Sr] in- the drainage. Variably metamorphosed Pre- crease, associated with increases in the concentration of Na1,K1, and Cl2, all of which cambrian sedimentary rocks make up the are high in the hydrothermal waters. Cation concentrations decrease along the Lesser Lesser Himalaya, pelitic schists and minor do- 13 Himalayan reach of the river. Hot-spring dissolved CO2 has a d C value to 15.9½, lomitic carbonates in the upper formation and indicating that metamorphic decarbonation reactions contribute CO2 to the ¯uids. -
Design and Analysis of Arch Dam with Autocad, ANSYS and Google Earth Software: a Case Study
ISSN (Online) 2393-8021 IARJSET ISSN (Print) 2394-1588 International Advanced Research Journal in Science, Engineering and Technology ISO 3297:2007 Certified Vol. 5, Issue 7, July 2018 Design and Analysis of Arch Dam with AutoCAD, ANSYS and Google Earth Software: A Case Study Shashank Nayan1, Arijit Kumar Banerji2, Md Asif SK3 B. Tech, Civil Engineering, BCREC, Durgapur, India1 Assistant Professor, Department of Civil Engineering, Dr. B. C. Roy Engineering College, Durgapur, India2 Assistant Professor, Department of Civil Engineering, Coochbehar Government Engineering College, India3 Abstract: In this research, a site is chosen for construction of dam, and its geotechnical data has been collected through online state government websites. It included topographical feature of the site, type of rock, soil, annual flow of river, annual rainfall. A narrow valley between the border of states Bihar and Jharkhand have been found through Google Map application software and we found the river Mohana flows throughout this valley. The abutment which is best suited for holding arms of the arch dam has been found here. Then Canon dimensions are known from google earth software. After it elementary dimension of the proposing arch dam is calculated using some empirical formulas [5]. These dimensions are plotted in AutoCAD worksheet and by joining these points we got the design. Most of the layout plans are taken from google earth software which may vary to the actual context of the realm. Each and every geo-co- ordinate with precision is noted down. Finally, a finite element analysis software which is ANSYS, is used for the checking the stability of structure.