Inventory of Glacial Lakes and Identification of Potentially
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GLACIERS of NEPAL—Glacier Distribution in the Nepal Himalaya with Comparisons to the Karakoram Range
Glaciers of Asia— GLACIERS OF NEPAL—Glacier Distribution in the Nepal Himalaya with Comparisons to the Karakoram Range By Keiji Higuchi, Okitsugu Watanabe, Hiroji Fushimi, Shuhei Takenaka, and Akio Nagoshi SATELLITE IMAGE ATLAS OF GLACIERS OF THE WORLD Edited by RICHARD S. WILLIAMS, JR., and JANE G. FERRIGNO U.S. GEOLOGICAL SURVEY PROFESSIONAL PAPER 1386–F–6 CONTENTS Glaciers of Nepal — Glacier Distribution in the Nepal Himalaya with Comparisons to the Karakoram Range, by Keiji Higuchi, Okitsugu Watanabe, Hiroji Fushimi, Shuhei Takenaka, and Akio Nagoshi ----------------------------------------------------------293 Introduction -------------------------------------------------------------------------------293 Use of Landsat Images in Glacier Studies ----------------------------------293 Figure 1. Map showing location of the Nepal Himalaya and Karokoram Range in Southern Asia--------------------------------------------------------- 294 Figure 2. Map showing glacier distribution of the Nepal Himalaya and its surrounding regions --------------------------------------------------------- 295 Figure 3. Map showing glacier distribution of the Karakoram Range ------------- 296 A Brief History of Glacier Investigations -----------------------------------297 Procedures for Mapping Glacier Distribution from Landsat Images ---------298 Figure 4. Index map of the glaciers of Nepal showing coverage by Landsat 1, 2, and 3 MSS images ---------------------------------------------- 299 Figure 5. Index map of the glaciers of the Karakoram Range showing coverage -
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 -
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. -
Even the Himalayas Have Stopped Smiling
Even the Himalayas Have Stopped Smiling CLIMATE CHANGE, POVERTY AND ADAPTATION IN NEPAL 'Even the Himalayas Have Stopped Smiling' Climate Change, Poverty and Adaptation in Nepal Disclaimer All rights reserved. This publication is copyright, but may be reproduced by any method without fee for advocacy, campaigning and teaching purposes, but not for resale. The copyright holder requests that all such use be registered with them for impact assessment purposes. For copying in any other circumstances, or for re-use in other publications, or for translation or adaptation, prior written permission must be obtained from the copyright holder, and a fee may be payable. This is an Oxfam International report. The affiliates who have contributed to it are Oxfam GB and Oxfam Hong Kong. First Published by Oxfam International in August 2009 © Oxfam International 2009 Oxfam International is a confederation of thirteen organizations working together in more than 100 countries to find lasting solutions to poverty and injustice: Oxfam America, Oxfam Australia, Oxfam-in-Belgium, Oxfam Canada, Oxfam France - Agir ici, Oxfam Germany, Oxfam GB, Oxfam Hong Kong, Intermon Oxfam, Oxfam Ireland, Oxfam New Zealand, Oxfam Novib and Oxfam Quebec. Copies of this report and more information are available at www.oxfam.org and at Country Programme Office, Nepal Jawalakhel-20, Lalitpur GPO Box 2500, Kathmandu Tel: +977-1-5530574/ 5542881 Fax: +977-1-5523197 E-mail: [email protected] Acknowledgements This report was a collaborative effort which draws on multiple sources, -
Field Report on the Preliminary Feasibility Study
Field report on the Preliminary Feasibility Study On Walking Trees along Lifezone Ecotones in Barun Valley, Nepal (A pilot project to develop key indicators for monitoring Biomeridians - Climate Response through Information & Local Engagement) Report Prepared By: The East Foundation (TEF), Sankhuwasabha, Nepal and Future Generations University, Franklin, WV, USA Submitted to Department of National Parks and Wildlife Conservation Babar Mahal, Kathmandu June 2018 1 Table of Contents Contents Page No. 1. Background ........................................................................................................................................... 4 2. Rationale ............................................................................................................................................... 5 3. Study Methodology ............................................................................................................................... 6 3.1 Contextual Framework ...................................................................................................................... 7 3.2 Study Area Description ..................................................................................................................... 9 3.3 Experimental Design and Data Collection Methodology ............................................................... 12 4. Study Findings .................................................................................................................................... 13 4.1 Geographic Summary -
Use of Space Technology in Glacial Lake Outburst Flood Mitigation: a Case Study of Imja Glacier Lake
Use of Space Technology In Glacial Lake Outburst Flood Mitigation: A case study of Imja glacier lake Abstract: Glacial Lake Outburst Flood (GLOF) triggered by the climate change affects the mountain ecosystem and livelihood of people in mountainous region. The use of space tools such as RADAR, GNSS, WiFi and GIS by the experts in collaboration with local community could contribute in achieving SDG-13 goals by assisting in GLOF risk identification and mitigation. Reducing geographical barriers, space technology can provide information about glacial lakes situated in inaccessible and high altitudes. A case study of application of these space tools in risk identification and mitigation of Imja Lake of Everest region is presented in this essay. Article: Introduction Climate change has emerged as one of the burning issues of the 21st century. According to Inter Governmental Panel for Climate Change (IPCC), it is defined as ' a change of climate which is attributed directly or indirectly to human activity that alters the composition of the global atmosphere and which is in addition to natural climate variability observed over comparable time periods' (IPCC, 2020). Some of its immediate impacts are increment of global temperature, extreme or low rainfall and accelerated melting of glaciers leading to Glacial Lake Outburst Flood (GLOF). The local people in the vicinity of potential hazards are the ones who have to suffer the most as a consequence of climate change. It would not only cause economic loss but also change the topography of the place, alter the social fabrics and create long-term livelihood issues which might take generations to recover. -
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. -
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. -
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. -
Peverest Base Camp Trek
Ultimate Island peak PeveRest Base Camp Trek A trekking & climbing experience that blows the mind! Your go to trekking experts for Nepal, Everest and all the adventures inbetween. What's inside? Why trek with EverTrek? 3 Route map 4 Trip overview 5 What’s included 6 Experience needed 7 Your itinerary 8 Equipment list 18 Extend your adventure 22 2 ultimate island peak & eveRest base camptrek 21 days Nepal Trip Duration - 21 Days Accommodation - 15 nights lodge, 2 nights tent, 3 nights hotel Tour Detail - 18 days trekking Max altitude - 6189m (20,305ft) IntroductioN High in the Khumbu region of Nepal, close to Mt Everest and closer still to the steep south face of Mt Lhotse, the aptly named Island Peak (6189m) rises above the glaciated valleys below. With its outrageous location and challenging summit ridge, this peak has been a favourite with our guides, leaders, and clients for a number of years. Ultimate Island Peak and Everest Base Camp Expedition is the ultimate experience in the Everest region for any one looking to attempt a Himalayan peak for the first time. You will not only climb Island Peak at 6189m (20,305ft) but also reach the historic Everest Base Camp (5364m) whilst also climbing 2 of the high passes of Cho La (5,420m) and Kongma La (5,535m) along with the sunrise hike to Kala Patthar (5,545m). One heck of an adventure! 3 clockwise route map of ultimate island peak and eveRest base camp 4 trip overview Trekking via Namche Bazaar we follow the route to Everest Base Camp via the Gokyo valley and Cho La Pass route and into Lobuche beside the Khumbuglacier. -
1 CURRICULAM VITAE Name Bijay Kumar Pokhrel Current Position Ph
CURRICULAM VITAE Name Bijay Kumar Pokhrel Current position Ph.D. student of Agricultural Economics at Louisiana State University, Baton Rouge, Louisiana, USA Address for 3450 Nicholson Dr, Apartment No. 1049 correspondence Zip: 70802, Baton Rouge, Louisiana, USA Email: [email protected] [email protected] [email protected] Cell.no. 225-916-7873 Key Qualification Mr. Bijay Kumar Pokhrel has over 20 years of professional experiences in different disciplines of Civil Engineering namely: Irrigation, Road, Building, Water Supply and Sanitation, and Hydrology. In these disciplines, he has involved in project planning, design, estimate and construction supervision, monitoring and evaluation, contractor and consultant hiring, research works etc. Now Mr. Pokhrel is a Ph.D. student of Agricultural Economics at Louisiana State University, Baton Rouge, He has served government of Nepal as a senior divisional hydrologist in the Department of Hydrology and Meteorology. He has comprehensive experiences in hydro-meteorology and involving in hydrological evaluation, covering Deterministic and Stochastic hydrology, with particular expertise in water resources planning, flood estimation, rainfall intensity and flood frequency analysis, rainfall- runoff hydrological modeling, flood forecasting, flood zoning, reservoir sedimentation, spillway design flood estimation and evaluation, Hydropower design flood estimation and evaluation, design, estimate and supervision of civil works. Similarly, Hydro-meteorological network design, hydro-meteorological data collection, processing and publication, GIS and Remote Sensing. Mr. Pokhrel was involved as a resource person of DHM for the research work namely "Impact of Climate Change on Snow and Glacier at Nepalese Himalaya" was carried out with the IRD, France and Nagoya University, of Japan. Mr. Pokhrel was a key person for joint research work with WWf Nepal and DHM for Impact of Climate change on surface flow of Koshi Basin of Nepal. -
Drainage System
CHAPTER DRAINAGE SYSTEM ou have observed water flowing through 2006) in this class . Can you, then, explain the the rivers, nalas and even channels reason for water flowing from one direction to Yduring rainy season which drain the the other? Why do the rivers originating from the excess water. Had these channels not been Himalayas in the northern India and the Western there, large-scale flooding would have Ghat in the southern India flow towards the east occurred. Wherever channels are ill-defined or and discharge their waters in the Bay of Bengal? choked, flooding is a common phenomenon. The flow of water through well-defined channels is known as ‘drainage’ and the network of such channels is called a ‘drainage system’. The drainage pattern of an area is the outcome of the geological time period, nature and structure of rocks, topography, slope, amount of water flowing and the periodicity of the flow. Do you have a river near your village or city? Have you ever been there for boating or bathing? Figure 3.1 : A River in the Mountainous Region Is it perennial (always with water) or ephemeral (water during rainy season, and dry, otherwise)? A river drains the water collected from a Do you know that rivers flow in the same specific area, which is called its ‘catchment area’. direction? You have studied about slopes in the An area drained by a river and its tributaries other two textbooks of geography (NCERT, is called a drainage basin. The boundary line Important Drainage Patterns (i) The drainage pattern resembling the branches of a tree is known as “dendritic” the examples of which are the rivers of northern plain.