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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 -
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, -
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. -
The Role of Sherpa Culture in Nature Conservation
The Role of SHERPA CULTURE in NATURE CONSERVATION Copyright © Khumbu Sherpa Culture Conservation Society www.khumbusherpaculture.org Book : The Role of Sherpa Culture in Nature Conservation Publisher : Khumbu Sherpa Culture Conservation Society (KSCCS) Published Year : 2073 B.S. Edition : First Writer & Photographer : Tenzing Tashi Sherpa Typing & Translation : Tsherin Ongmu Sherpa Editor : Professor Stan Stevens, Ph.D. Design, Layout & Print : Digiscan Pre-press Pvt. Ltd., Naxal, Kathmandu The Role of SHERPA CULTURE in NATURE CONSERVATION Table of Contents 1. The Role of Sherpa Culture in Nature Conservation 1 Khumbu is a Sherpa Community Conserved Area 2 Sacred Himalayas 3 Sacred Lakes - Gokyo Lake 5 Springs 9 Religious Conserved Forests 10 Community Conserved Forest 11 Bird Conservation Area 12 Grazing Management Areas for Livestock 12 Conservation Tradition 13 Nawa System for Conservation 14 The Rules of Singhki Nawa (Wood Custodian) 14 The Custom of the Lhothok Nawa (Crop and Pastures Custodian) 15 The Work and the Duty Term of the Nawa and Worshyo 17 Yulthim (Community Assembly) 18 The Rules and Laws of Community 19 Short Story by Reincarnated Lama Ngawang Tenzing Zangbu about Nawa 20 The Sacred Worship Areas of Sherpas 21 Nangajong 21 Worshyo 22 Pangboche 23 Places in Between Fungi Thyanga Bridge and Pangboche Bridge 25 Khumjung and Khunde 29 Khumbu’s Chortens 33 Agriculture of Khumbu 35 Mountains Around Khumbu 38 2. The Role of KSCCS in Nature Conservation 39 A. Cultural Interaction 39 B. Cultural and ICCA Educational Tour 40 1. Community Tour 40 2. Sherpa Culture and Conservation Tour for Students Organized by Khumjung by KSCCS 41 3. -
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. -
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. -
Himalayan Glacier Mass Changes Altherr, W
Discussion Paper | Discussion Paper | Discussion Paper | Discussion Paper | The Cryosphere Discuss., 4, 2593–2613, 2010 The Cryosphere www.the-cryosphere-discuss.net/4/2593/2010/ Discussions TCD doi:10.5194/tcd-4-2593-2010 4, 2593–2613, 2010 © Author(s) 2010. CC Attribution 3.0 License. Himalayan glacier This discussion paper is/has been under review for the journal The Cryosphere (TC). mass changes Please refer to the corresponding final paper in TC if available. T. Bolch et al. Longest time series of glacier mass Title Page changes in the Himalaya based on stereo Abstract Introduction imagery Conclusions References Tables Figures T. Bolch1,3, T. Pieczonka1, and D. I. Benn2,4 1Institut fur¨ Kartographie, Technische Universitat¨ Dresden, Germany J I 2 The University Centre in Svalbard, Norway J I 3Geographisches Institut, Universitat¨ Zurich,¨ Switzerland 4University of St Andrews, UK Back Close Received: 1 December 2010 – Accepted: 9 December 2010 – Published: 20 December 2010 Full Screen / Esc Correspondence to: T. Bolch ([email protected]) Printer-friendly Version Published by Copernicus Publications on behalf of the European Geosciences Union. Interactive Discussion 2593 Discussion Paper | Discussion Paper | Discussion Paper | Discussion Paper | Abstract TCD Mass loss of Himalayan glaciers has wide-ranging consequences such as declining water resources, sea level rise and an increasing risk of glacial lake outburst floods 4, 2593–2613, 2010 (GLOFs). The assessment of the regional and global impact of glacier changes in 5 the Himalaya is, however, hampered by a lack of mass balance data for most of the Himalayan glacier range. Multi-temporal digital terrain models (DTMs) allow glacier mass balance to be mass changes calculated since the availability of stereo imagery. -
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. -
Assessment of Carbon Dynamics in Relation to Nutrient Content in Littoral
Assessment of Carbon Stock in Association with Nutrient Content in the Littoral Zone of Kalchuman Lake of Manaslu Conservation Area Thesis prepared in the partial fulfillment of the requirement for the Master of Science (M.Sc.) degree in Environment Science of Tribhuvan University Submitted to College of Applied Sciences-Nepal Kathmandu, Nepal Submitted by Anju Rana Symbol no: 12682 (TU Regd.no:5-2-37-974-2006) 2013 I Letter of Recommendation This is to certify that the dissertation entitled “Assessment of Carbon Stock in Association with Nutrient Content in the Littoral Zone of Kalchuman Lake of Manaslu Conservation Area” submitted by Ms. Anju Rana for the partial fulfillment of M.Sc. Degree in Environmental Science is based on the study carried out by her under our supervision. The dissertation or a part thereof has not been previously submitted for any other degree. Therefore I recommended this thesis. Pratima Sharma, PhD Sujen Man Shrestha, PhD Supervisor Supervisor I Letter of Approval The dissertation presented by Ms. Anju Rana entitled “Assessment of Carbon Stock in Association with Nutrient Content in the Littoral Zone of Kalchuman Lake of Manaslu Conservation Area” has been accepted as a partial fulfillment of requirement for the completion of Master‘s degree in Environmental Science. Dr. Bhupendra Devkota Dr. Sujen Man Shrestha Principal Supervisor Mr. Ram Asheshwor Mandal,MSc Mr. Rabi Bhattarai, MSc REDD+, Babarmahal, Kathmandu CAS Faculty Member External Examiner Internal Examiner II Acknowledgement At first, I would like to express my special gratitude to NCCKMC-NAST and CDKN for providing me the financial support for the study. -
Glacial Lake Outburst Floods Risk Reduction Activities in Nepal
Glacial lake outburst floods risk reduction activities in Nepal Samjwal Ratna BAJRACHARYA [email protected] International Centre for Integrated Mountain Development (ICIMOD) PO Box 3226 Kathmandu Nepal Abstract: The global temperature rise has made a tremendous impact on the high mountainous glacial environment. In the last century, the global average temperature has increased by approximately 0.75 °C and in the last three decades, the temperature in the Nepal Himalayas has increased by 0.15 to 0.6 °C per decade. From early 1970 to 2000, about 6% of the glacier area in the Tamor and Dudh Koshi sub-basins of eastern Nepal has decreased. The shrinking and retreating of the Himalayan glaciers along with the lowering of glacier surfaces became visible after early 1970 and increased rapidly after 2000. This coincides with the formation and expansion of many moraine-dammed glacial lakes, leading to the stage of glacial lake outburst flood (GLOF). The past records show that at least one catastrophic GLOF event had occurred at an interval of three to 10 years in the Himalayan region. Nepal had already experienced 22 catastrophic GLOFs including 10 GLOFs in Tibet/China that also affected Nepal. The GLOF not only brings casualties, it also damages settlements, roads, farmlands, forests, bridges and hydro-powers. The settlements that were not damaged during the GLOF are now exposed to active landslides and erosions scars making them high-risk areas. The glacial lakes are situated at high altitudes of rugged terrain in harsh climatic conditions. To carry out the mitigation work on one lake costs more than three million US dollars. -
Modeling the Glacial Lake Outburst Flood Process Chain in the Nepal
Hydrol. Earth Syst. Sci., 22, 3721–3737, 2018 https://doi.org/10.5194/hess-22-3721-2018 © Author(s) 2018. This work is distributed under the Creative Commons Attribution 4.0 License. Modeling the glacial lake outburst flood process chain in the Nepal Himalaya: reassessing Imja Tsho’s hazard Jonathan M. Lala1, David R. Rounce2, and Daene C. McKinney1 1Center for Water and the Environment, University of Texas at Austin, Austin, TX, USA 2Geophysical Institute, University of Alaska Fairbanks, Fairbanks, AK, USA Correspondence: Jonathan M. Lala ([email protected]) Received: 22 November 2017 – Discussion started: 14 December 2017 Revised: 13 June 2018 – Accepted: 26 June 2018 – Published: 13 July 2018 Abstract. The Himalayas of South Asia are home to many applicable to lakes in the greater region. Neither case re- glaciers that are retreating due to climate change and caus- sulted in flooding outside the river channel at downstream ing the formation of large glacial lakes in their absence. villages. The worst-case model resulted in some moraine ero- These lakes are held in place by naturally deposited moraine sion and increased channelization of the lake outlet, which dams that are potentially unstable. Specifically, an impulse yielded greater discharge downstream but no catastrophic wave generated by an avalanche or landslide entering the collapse. The site-specific model generated similar results, lake can destabilize the moraine dam, thereby causing a but with very little erosion and a smaller downstream dis- catastrophic failure of the moraine and a glacial lake out- charge. These results indicated that Imja Tsho is unlikely to burst flood (GLOF). -
Ecology of the Snow Leopard and the Himalayan Tahr
ECOLOGY OF THE SNOW LEOPARD AND THE HIMALAYAN TAHR IN SAGARMATHA (MT. EVEREST) NATIONAL PARK, NEPAL By SOM B. ALE M. Sc. (Zoology), Tribhuvan University, Nepal, 1992 M. S. (Ecology), University of Tromso, Norway, 1999 THESIS Submitted as partial fulfilment of the requirements for the degree of Doctor of Philosophy in the Biological Sciences in the Graduate College of the University of Illinois at Chicago, 2007 Chicago, Illinois ACKNOWLEDGMENTS My special thanks go to my supervisor, Joel Brown, whose insight and guidance made this work possible. Thanks are due to my other distinguished committee members: Mary Ashley, Henry Howe, Sandro Lovari, Steve Thompson and Chris Whelan, who were very supportive and constructive while accomplishing my research goals; extra thanks to C.W. and H. H., with whom I wrote Chapters Seven and Eight, respectively. I am grateful to my colleagues in Brown and Howe labs, in particular, A. Golubski and J. Moll, for discussions and their comments during the formative period of my work, and Mosheh Wolf who prepared maps for this work. I would like to thank colleagues and officials at the University of Illinois at Chicago (Biological Sciences, particularly Brown lab and Howe lab), USA, Department of National Parks and Wildlife Conservation (S. Bajimaya, J. Karki), National (erstwhile King Mahendra) Trust for Nature Conservation (S. B. Bajracharaya, G. J. Thapa), Resources Himalaya (P. Yonzon), in Nepal, for their help. I appreciate suggestions on arrays of matters related to this work from R. Jackson (Snow leopard Conservancy, USA), K. B. Shah (Natural History Museum, Nepal) and J. L. Fox (University of Tromos, Norway).