Impact of Land-Use and Climatic Changes on Hydrology of the Himalayan Basin: a Case Study of the Kosi Basin Keshav Prasad Sharma University of New Hampshire, Durham

Total Page:16

File Type:pdf, Size:1020Kb

Impact of Land-Use and Climatic Changes on Hydrology of the Himalayan Basin: a Case Study of the Kosi Basin Keshav Prasad Sharma University of New Hampshire, Durham University of New Hampshire University of New Hampshire Scholars' Repository Doctoral Dissertations Student Scholarship Spring 1997 Impact of land-use and climatic changes on hydrology of the Himalayan Basin: A case study of the Kosi Basin Keshav Prasad Sharma University of New Hampshire, Durham Follow this and additional works at: https://scholars.unh.edu/dissertation Recommended Citation Sharma, Keshav Prasad, "Impact of land-use and climatic changes on hydrology of the Himalayan Basin: A case study of the Kosi Basin" (1997). Doctoral Dissertations. 1961. https://scholars.unh.edu/dissertation/1961 This Dissertation is brought to you for free and open access by the Student Scholarship at University of New Hampshire Scholars' Repository. It has been accepted for inclusion in Doctoral Dissertations by an authorized administrator of University of New Hampshire Scholars' Repository. For more information, please contact [email protected]. INFORMATION TO USERS This manuscript has been reproduced from the microfilm master. UMI films the text directly from the original or copy submitted. Thus, some thesis and dissertation copies are in typewriter free, while others may be from any type o f computer printer. The quality of this reproduction is dependent upon the quality of the copy submitted. Broken or indistinct print, colored or poor quality illustrations and photographs, print bleedthrough, substandard margins, and improper alignment can adversely afreet reproduction. In the unlikely event that the author did not send UMI a complete manuscript and there are missing pages, these will be noted. Also, if unauthorized copyright material had to be removed, a note will indicate the deletion. Oversize materials (e.g., maps, drawings, charts) are reproduced by sectioning the original, beginning at the upper left-hand comer and continuing from left to right in equal sections with small overlaps. Each original is also photographed in one exposure and is included in reduced form at the back o f the book. Photographs included in the original manuscript have been reproduced xerographically in this copy. Higher quality 6” x 9” black and white photographic prints are available for any photographs or illustrations appearing in this copy for an additional charge. Contact UMI directly to order. UMI A Bell & Howell Information Company 300 North Zeeb Road, Ann A'toor MI 48106-1346 USA 313/761-4700 800/521-0600 Reproduced with permission of the copyright owner. Further reproduction prohibited without permission. Reproduced with permission of the copyright owner. Further reproduction prohibited without permission. IMPACT OF LAND-USE AND CLIMATIC CHANGES ON HYDROLOGY OF THE HIMALAYAN BASIN: A CASE STUDY OF THE KOSI BASIN BY KESHAV PRASAD SHARMA Diploma in Science, Tribhuvan University, 1975 Degree in Atmospheric Physics, Tribhuvan University, 1979 Master o f Technology in Hydrology, University o f Roorkee, 1982 DISSERTATION Submitted to the University o f New Hampshire in Partial Fulfillment o f the Requirements for the Degree o f Doctor o f Philosophy in Earth Sciences May, 1997 Reproduced with permission of the copyright owner. Further reproduction prohibited without permission. UMI Number: 9730844 Copyright 1997 by Sharma, Keshav Prasad All rights reserved. UMI Microform 9730844 Copyright 1997, by UMI Company. All rights reserved. This microform edition is protected against unauthorized copying under Title 17, United States Code. UMI 300 North Zeeb Road Ann Arbor, MI 48103 Reproduced with permission of the copyright owner. Further reproduction prohibited without permission. ALL RIGHTS RESERVED c 1997 Keshav Prasad Sharma Reproduced with permission of the copyright owner. Further reproduction prohibited without permission. This dissertation has been examined and approved. .W-t- [J j H Dissertation Director, Berrien Moore III, Director of the Institute for the Studv of* Earth. Oceans, and Space. Charles S. Vorosmarty, Research Assistant Professor of Eartnj Sciences and Earth, Oceans, and Space. Professor of Hydrology and Water Resources. Paul A. Mavewski, Professor of Glaciology in Earth Sciences and Earth, Oceans, and Space. MatthewT^a^^Ass^ntProfessor of Hydrogeology. May 9, L997 Date Reproduced with permission of the copyright owner. Further reproduction prohibited without permission. ACKNOWLEDGMENTS Timely completion of this dissertation work was possible only through support, guidance, constructive comments, and continuous encouragement that I received from my advisor Professor Berrien Moore III throughout this research work. I am grateful to all the members of my committee for allowing me to work with them and for their thought­ ful comments on the draft. I am particularly indebted to Dr. Charles J. Vorosmarty and Professor S. L. Dingman for their help, guidance, and several discussions. I acknowledge the enormous help provided by Dr. Sharad. P. Adhikary and Kiran Shankar in Nepal and Karen Bushold at the University of New Hampshire. Several colleagues and staff at the University of New Hampshire and at the De­ partment of Hydrology and Meteorology in Nepal have helped me in different aspects of research work, field work and data collection. I am particularly thankful to: Dilip Gautam, Narendra Khanal, Dirk Metzko, and W. Laible in Nepal and Balazs Fekete and Nancy Voorhis at the University of New Hampshire. Several pieces of information, obtained from Annette Schloss, Fay Rubin, John Canfield, Alastair Lough, and Scott Robeson, and discussions with Dr. Janet Campbell and Professor Loren D. Meeker helped to refine some of the chapters of this dissertation. I would like to acknowledge the Department of Hydrology and Meteorology, Kathmandu for making hydrological and meteorological data available for this study. The department also made available different facilities for carrying out field and labora­ tory works at its central office in Kathmandu and at the basin office in Dharan. The iv Reproduced with permission of the copyright owner. Further reproduction prohibited without permission. German Development Service (GDS) provided partial support for some of the field activities and travels. Some supplementary hydrological and meteorological data were obtained from Eastern Region Road Maintenance Project, Dharan. Forest Resource Information System Project of the Department of Forest, Nepal provided land-use data for eastern Nepal in digital format. Lastly, I want to express my thanks to all the members of my family for supporting me with their love and affection during the long period of research work. Many thanks are due to my daughter Kalandika who helped me to enter the volumes of data into computer. This work has been supported by the NASA Mission to Planet Earth grant number NAGW 2669. Most of the researches were carried out at the Complex Systems Research Center, Institute for the Study of Earth, Oceans, and Space, University of New Hamp­ shire. V Reproduced with permission of the copyright owner. Further reproduction prohibited without permission. TABLE OF CONTENTS ACKNOWLEDGMENTS.........................................................................................iv LIST OF TA BLES................................................................................................... x LIST OF FIGURES........................................................................................... xiii GLOSSARY OF ABBREVIATION..................................................................... xvii ABSTRACT.......................................................................................................... xx CHAPTER PAGE I. INTRODUCTION...................................................................................... 1 Background ................................................................................................. 3 Objectives .................................................................................................. 7 Research Questions ..................................................................................... 7 Scope and Limitations of the Study ............................................................. 8 II STUDY AREA.......................................................................................... 11 Basin Characteristics .................................................................................. 14 Hydrometeorological Characteristics ........................................................... 23 III REVIEW OF RELATED LITERATURE.............................................. 27 Land-use changes in the Himalayas ................................................................ 27 Catastrophic degradation .............................................................. 28 Normal Processes .......................................................................... 29 Greening trend ............................................................................. 31 Realities........................................................................................ 32 Land-use and climate change ................................................................... 33 Sensitivity of the Himalayan clim ate ......................................................... 34 Discussion ................................................................................................ 37 IV COLLECTION AND ANALYSIS OF DATA............................................ 39 Meteorological and hydrological d a t^ ....................................................... 39 Land-use and anthropogenic d a ta .............................................................
Recommended publications
  • Kosi Embankment Breach in Nepal: Need for a Paradigm Shift in Responding to Floods
    SPECIAL ARTICLE Kosi Embankment Breach in Nepal: Need for a Paradigm Shift in Responding to Floods Ajaya Dixit The breach of the Kosi embankment in Nepal in n 18 August 2008, a flood control embankment along the August 2008 marked the failure of conventional ways Kosi River in Nepal terai breached and most of its mon- soon discharge and sediment load began flowing over an of controlling floods. After discussing the physical O area once kept flood-secure by the eastern Kosi embankment. Soon characteristics of the Kosi River and the Kosi barrage a disaster had unfolded in Sunsari district of Nepal terai and in six project, this paper suggests that the high sediment districts of north-east Bihar of India: Supaul, Madhepura, Saharsa, content of the Kosi River implies a major risk to the Arariya, Purniya and Khagariya. About 50,000 Nepalis and a stag- gering 3.5 million Indians (people of Bihar) were affected. A few proposed Kosi high dam and its ability to control floods died but the exact death toll is not known. The extent of the adverse in Bihar. It concludes by proposing the need for a effects of the widespread inundation on the dependent social and paradigm shift in dealing with the risks of floods. economic systems is only gradually becoming evident. Cloudbursts, landslides, mass movements, mud flows and flash floods are common in the mountains during the monsoon. In the plains of southern Nepal, northern Uttar Pradesh, Bihar, West Bengal and Bangladesh, rivers augmented by monsoon rains overflow their banks. Sediment eroded from the upper moun- tains is transported to the lower reaches and deposited on valleys and on the plains.
    [Show full text]
  • 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
    [Show full text]
  • World Bank Document
    Water Policy 15 (2013) 147–164 Public Disclosure Authorized Ten fundamental questions for water resources development in the Ganges: myths and realities Claudia Sadoffa,*, Nagaraja Rao Harshadeepa, Donald Blackmoreb, Xun Wuc, Anna O’Donnella, Marc Jeulandd, Sylvia Leee and Dale Whittingtonf aThe World Bank, Washington, USA *Corresponding author. E-mail: [email protected] bIndependent consultant, Canberra, Australia cNational University of Singapore, Singapore dDuke University, Durham, USA Public Disclosure Authorized eSkoll Global Threats Fund, San Francisco, USA fUniversity of North Carolina at Chapel Hill and Manchester Business School, Manchester, UK Abstract This paper summarizes the results of the Ganges Strategic Basin Assessment (SBA), a 3-year, multi-disciplinary effort undertaken by a World Bank team in cooperation with several leading regional research institutions in South Asia. It begins to fill a crucial knowledge gap, providing an initial integrated systems perspective on the major water resources planning issues facing the Ganges basin today, including some of the most important infrastructure options that have been proposed for future development. The SBA developed a set of hydrological and economic models for the Ganges system, using modern data sources and modelling techniques to assess the impact of existing and potential new hydraulic structures on flooding, hydropower, low flows, water quality and irrigation supplies at the basin scale. It also involved repeated exchanges with policy makers and opinion makers in the basin, during which perceptions of the basin Public Disclosure Authorized could be discussed and examined. The study’s findings highlight the scale and complexity of the Ganges basin. In par- ticular, they refute the broadly held view that upstream water storage, such as reservoirs in Nepal, can fully control basin- wide flooding.
    [Show full text]
  • The Sediment Load of Indian Rivers — an Update
    Erosion and Sediment Yield: Global and Regional Perspectives (Proceedings of the Exeter Symposium, July 1996). IAHS Publ. no. 236, 1996. 183 The sediment load of Indian rivers — an update V. SUBRAMANIAN School of Environmental Studies, Jawaharlal Nehru University, New Delhi 110 067, India Abstract This paper summarizes recent information collected on sediment transport in Indian rivers. It reveals the major contribution which Indian rivers make to the total amount of sediment delivered to the ocean at a global scale, but also highlights the large temporal and spatial variability of riverine sediment transport in the Indian sub-continent. This variability is evident not only in the quantity of the sediment transported but also in the size and mineralogical characteristics of the sediment loads. INTRODUCTION The present estimate of global sediment discharge at 15-16 X 10161 year"1 (Walling & Webb, 1983) is perhaps an underestimated value due to undetermined values for several minor catchments (Milliman &Meybeck, 1995). Nevertheless, it is now well recognized that the Pacific Oceanic islands and South and Southeast Asia constitute a single geographic region which contributes nearly 80% of the global sediment budget. Over the years, considerable data have been collected concerning sediment transport in several Indian rivers. For example, Abbas & Subramanian (1984) estimated the sediment load of the Ganges at Farraka Barrage to be 1235 t km"2 year"1, which is 8 times the world average erosion rate (1501 km“2 year"1) calculated by Milliman & Meade (1983). To improve our understanding of sediment transport processes in South Asia, there is a need to examine recently collected information.
    [Show full text]
  • Constructing Reservoir Dams in Deglacierizing Regions of the Nepalese Himalaya the Geneva Challenge 2018
    Constructing reservoir dams in deglacierizing regions of the Nepalese Himalaya The Geneva Challenge 2018 Submitted by: Dinesh Acharya, Paribesh Pradhan, Prabhat Joshi 2 Authors’ Note: This proposal is submitted to the Geneva Challenge 2018 by Master’s students from ETH Zürich, Switzerland. All photographs in this proposal are taken by Paribesh Pradhan in the Mount Everest region (also known as the Khumbu region), Dudh Koshi basin of Nepal. The description of the photos used in this proposal are as follows: Photo Information: 1. Cover page Dig Tsho Glacial Lake (4364 m.asl), Nepal 2. Executive summary, pp. 3 Ama Dablam and Thamserku mountain range, Nepal 3. Introduction, pp. 8 Khumbu Glacier (4900 m.asl), Mt. Everest Region, Nepal 4. Problem statement, pp. 11 A local Sherpa Yak herder near Dig Tsho Glacial Lake, Nepal 5. Proposed methodology, pp. 14 Khumbu Glacier (4900 m.asl), Mt. Everest valley, Nepal 6. The pilot project proposal, pp. 20 Dig Tsho Glacial Lake (4364 m.asl), Nepal 7. Expected output and outcomes, pp. 26 Imja Tsho Glacial Lake (5010 m.asl), Nepal 8. Conclusions, pp. 31 Thukla Pass or Dughla Pass (4572 m.asl), Nepal 9. Bibliography, pp. 33 Imja valley (4900 m.asl), Nepal [Word count: 7876] Executive Summary Climate change is one of the greatest challenges of our time. The heating of the oceans, sea level rise, ocean acidification and coral bleaching, shrinking of ice sheets, declining Arctic sea ice, glacier retreat in high mountains, changing snow cover and recurrent extreme events are all indicators of climate change caused by anthropogenic greenhouse gas effect.
    [Show full text]
  • Damage from the April-May 2015 Gorkha Earthquake Sequence in the Solukhumbu District (Everest Region), Nepal David R
    Damage from the april-may 2015 gorkha earthquake sequence in the Solukhumbu district (Everest region), Nepal David R. Lageson, Monique Fort, Roshan Raj Bhattarai, Mary Hubbard To cite this version: David R. Lageson, Monique Fort, Roshan Raj Bhattarai, Mary Hubbard. Damage from the april-may 2015 gorkha earthquake sequence in the Solukhumbu district (Everest region), Nepal. GSA Annual Meeting, Sep 2016, Denver, United States. hal-01373311 HAL Id: hal-01373311 https://hal.archives-ouvertes.fr/hal-01373311 Submitted on 28 Sep 2016 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. DAMAGE FROM THE APRIL-MAY 2015 GORKHA EARTHQUAKE SEQUENCE IN THE SOLUKHUMBU DISTRICT (EVEREST REGION), NEPAL LAGESON, David R.1, FORT, Monique2, BHATTARAI, Roshan Raj3 and HUBBARD, Mary1, (1)Department of Earth Sciences, Montana State University, 226 Traphagen Hall, Bozeman, MT 59717, (2)Department of Geography, Université Paris Diderot, 75205 Paris Cedex 13, Paris, France, (3)Department of Geology, Tribhuvan University, Tri-Chandra Campus, Kathmandu, Nepal, [email protected] ABSTRACT: Rapid assessments of landslides Valley profile convexity: Earthquake-triggered mass movements (past & recent): Traditional and new construction methods: Spectrum of structural damage: (including other mass movements of rock, snow and ice) as well as human impacts were conducted by many organizations immediately following the 25 April 2015 M7.8 Gorkha earthquake and its aftershock sequence.
    [Show full text]
  • Journal of Integrated Disaster Risk Manangement
    IDRiM(2013)3(1) ISSN: 2185-8322 DOI10.5595/idrim.2013.0061 Journal of Integrated Disaster Risk Management Original paper Determination of Threshold Runoff for Flood Warning in Nepalese Rivers 1 2 Dilip Kumar Gautam and Khadananda Dulal Received: 05/02/2013 / Accepted: 08/04/2013 / Published online: 01/06/2013 Abstract The Southern Terai plain area of Nepal is exposed to recurring floods. The floods, landslides and avalanches in Nepal cause the loss of lives of about 300 people and damage to properties worth about 626 million NPR annually. Consequently, the overall development of the country has been adversely affected. The flood risk could be significantly reduced by developing effective operational flood early warning systems. Hence, a study has been conducted to assess flood danger levels and determine the threshold runoff at forecasting stations of six major rivers of Nepal for the purpose of developing threshold-stage based operational flood early warning system. Digital elevation model data from SRTM and ASTER supplemented with measured cross-section data and HEC-RAS model was used for multiple profile analysis and inundation mapping. Different inundation scenarios were generated for a range of flood discharge at upstream boundary and flood threshold levels or runoffs have been identified for each river, thus providing the basis for developing threshold-stage based flood early warning system in these rivers. Key Words Flood, danger level, threshold runoff, hydrodynamic model, geographic information system 1. INTRODUCTION Nepal's Terai region is the part of the Ganges River basin, which is one of the most disaster-prone regions in the world.
    [Show full text]
  • Ganges Strategic Basin Assessment
    Public Disclosure Authorized Report No. 67668-SAS Report No. 67668-SAS Ganges Strategic Basin Assessment A Discussion of Regional Opportunities and Risks Public Disclosure Authorized Public Disclosure Authorized Public Disclosure Authorized GANGES STRATEGIC BASIN ASSESSMENT: A Discussion of Regional Opportunities and Risks b Report No. 67668-SAS Ganges Strategic Basin Assessment A Discussion of Regional Opportunities and Risks Ganges Strategic Basin Assessment A Discussion of Regional Opportunities and Risks World Bank South Asia Regional Report The World Bank Washington, DC iii GANGES STRATEGIC BASIN ASSESSMENT: A Discussion of Regional Opportunities and Risks Disclaimer: © 2014 The International Bank for Reconstruction and Development / The World Bank 1818 H Street NW Washington, DC 20433 Telephone: 202-473-1000 Internet: www.worldbank.org All rights reserved 1 2 3 4 14 13 12 11 This volume is a product of the staff of the International Bank for Reconstruction and Development / The World Bank. The findings, interpretations, and conclusions expressed in this volume do not necessarily reflect the views of the Executive Directors of The World Bank or the governments they represent. The World Bank does not guarantee the accuracy of the data included in this work. The boundaries, colors, denominations, and other information shown on any map in this work do not imply any judgment on part of The World Bank concerning the legal status of any territory or the endorsement or acceptance of such boundaries. Rights and Permissions The material in this publication is copyrighted. Copying and/or transmitting portions or all of this work without permission may be a violation of applicable law.
    [Show full text]
  • Introduction
    CHAPTER - I INTRODUCTION 1.0 Background Ministry of Water Resources, Government of India in the year 2004 decided to undertake comprehensive assessment of feasibility of linking of the rivers of the country starting with southern rivers in a fully consultative manner and to explore the feasibility of intrastate river links of the country. Accordingly, proposal for inclusion of prefeasibility / feasibility studies of intrastate links aspect in NWDA's mandate was put up for consideration in Special General Meeting of NWDA Society held on June 28, 2006 and it was decided to incorporate this function in NWDA's mandate. Finally, MoWR vide Resolution dated November 30, 2006 modified the functions of NWDA Society to include preparation of prefeasibility/feasibility studies of intrastate links. The functions of NWDA were further modified vide MoWR Resolution dated May 19, 2011 to undertake the work of preparation of Detailed Project Reports (DPRs) of intrastate links also by NWDA. Further, the Gazette notification of the enhanced mandate was issued on June 11, 2011. In the meantime, on the basis of approval conveyed by MoWR in June, 2005, NWDA requested all the State Governments to identify the intrastate link proposals in their States and send details to NWDA for their prefeasibility / feasibility studies. Bihar responded to NWDA's request vide letter No. PMC-5(IS)-01/2006-427, Patna dated May 15, 2008 and submitted their proposals. Subsequently, a meeting was held between the officers of Water Resource Department (WRD), Government of Bihar and NWDA on June 16, 2008 in Patna. In the said meeting, Government of Bihar requested NWDA to prepare the prefeasibility reports of six intrastate links out of which two were irrigation schemes.
    [Show full text]
  • Geomorphological Studies and Flood Risk Assessment of Kosi River Basin Using Remote 2011-13 Sensing and Gis Techniques
    Contents List of Tables ............................................................................................................................... 4 Lists of Figures ............................................................................................................................ 5 1. Introduction ........................................................................................................................ 7 1.1 General .......................................................................................................................... 7 1.2 Flood Risk Concept ....................................................................................................... 7 1.3 Background and Motivation ....................................................................................... 12 1.4 Research Questions and Objectives ............................................................................ 13 1.5 Study Area .................................................................................................................. 14 1.6 Organization of Thesis Chapters ................................................................................. 14 2. Literature Review ............................................................................................................. 16 2.1 General ........................................................................................................................ 16 2.2 Geomorphic Controls of Floods .................................................................................
    [Show full text]
  • Programme – Policy – Implementation of Program – Monitoring Flood 2008 - Impact
    Environment and Sustainable development: Improving Systems Performance Floods in Kosi • Failure of – Programme – Policy – Implementation of program – Monitoring Flood 2008 - Impact • The flood killed close to 1000 people and forced nearly 30 lakh people from their homes in Bihar. No cattle dead, main economic soruce of livelihood, not known. • Widespread disease and fear of epidemic • More than 300,000 houses were destroyed and at least 340,000 hectares (840,000 acres) of crops were damaged. • Crops worth over Rs.1.5 billion damaged and destroyed. 2008 Floods – Response • National Disaster Declared • Government announced USD 230 million • Announced construction of hazard safe houses for 100,000 families. • World Bank Supported the above program with USD 220 million commitment. • Chief minister asked for 145 billion rehabilitation package. • Instituted inquiry commission under Justice Walia • OUTCOME: • Out of a total 100,000 houses to be constructed by the Government in the Kosi region comprising Madhepura, Saharsa and Supaul districts, only 12,500 were erected till February 2014. • Justice Walia commission report tabled in 2014 (after FIVE YEARS) identified administrative failure and holds government responsible. Who’s at fault? • KOSI for being the way it is – Bihar’s Sorrow • Government – national, state, local, etc. • Zero accountability – authoriies responsible for it go left untouched. • Lack of preparedness • Lack of communication to the downstream population at the time of the embankment breach • Corruption – poor quality material used in construction of barrages/dams and poor upkeep. • Zero value of human life..that sustains CHALTA HAI ATTITUDE – Almost always last minute response. • Who else………God?? Nature’s Fury or Man made Disaster? • Kosi is named as Sorrow of Bihar!! • Since 1963, Kosi has breached 7 times and 2008 at kusaha was its 8th and most impactful.
    [Show full text]
  • FLOOD FREQUENCY ANALYSIS for KOSI RIVER at ITS BARRAGE SITE Radha Krishan1 and L.B
    J. Indian Water Resour. Soc., Vol 36, No. 1, January, 2016 FLOOD FREQUENCY ANALYSIS FOR KOSI RIVER AT ITS BARRAGE SITE Radha Krishan1 and L.B. Roy2 ABSTRACT Floods are natural events that have always been an integral part of the geologic history of earth. Human settlements and coactivity have always tended to use flood plains. The Kosi river in north Bihar plains of Eastern India presents a challenge in terms of long and recurring flood hazard. Despite a long history of flood control management in the basin for more than five decades, the river continues to bring a lot of misery through extensive flooding. In the present paper the Log-Pearson Type III distribution, a statistical technique for fitting frequency distribution, has been used to predict the design flood for the river at its barrage site for the discharge data from 1964 to 2008 obtained from WRD, Govt. of Bihar. Apart from this the morphology of the River and the Kosi project have also been described and discussed. Keywords: Floods, Kosi river, frequency distribution methods INTRODUCTION Flood and drainage are the two vital interrelated problems of Bihar, a poverty stricken state particularly in North Bihar. The North Bihar plains are drained by some Himalayan rivers and the Ganga being the trunk drain. These rivers are perennial as these are rain as well as snow fed. Important rivers of North Bihar include the Kosi, Gandak, Baghmati, Burhi Gandak, Kamla, Kamla-Balan Mahananda, Kareh and few others. All these rivers have relatively youthful topography and are engaged in channel deepening. They move parallel to the Ganga in the South-east direction and then drain into it.
    [Show full text]