Changes in Imja Tsho in the Mt. Everest Region of Nepal
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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 -
Geo-Hydrological Hazards Induced by Gorkha Earthquake 2015
Geo-hydrological hazards induced by Gorkha Earthquake 2015: A Case of Pharak area, Everest Region, Nepal Buddhi Raj Shrestha, Narendra Raj Khanal, Joëlle Smadja, Monique Fort To cite this version: Buddhi Raj Shrestha, Narendra Raj Khanal, Joëlle Smadja, Monique Fort. Geo-hydrological hazards induced by Gorkha Earthquake 2015: A Case of Pharak area, Everest Region, Nepal. The Geograph- ical Journal of Nepal, Central Department of Geography, Faculty of Humanities and Social Studies, Tribhuvan University, 2020, 13, pp.91 - 106. 10.3126/gjn.v13i0.28154. halshs-02933571 HAL Id: halshs-02933571 https://halshs.archives-ouvertes.fr/halshs-02933571 Submitted on 17 Sep 2020 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. The Geographical Journal of Nepal Vol. 13: 91-106, 2020 Doi: http://doi.org/10.3126/gjn.v13i0.28154 Central Department of Geography, Tribhuvan University, Kathmandu, Nepal Geo-hydrological hazards induced by Gorkha Earthquake 2015: A Case of Pharak area, Everest Region, Nepal Buddhi Raj Shrestha1,4*, Narendra Raj Khanal1,4, Joëlle Smadja2,4, Monique Fort3,4 1 Central Department of Geography, Tribhuvan University, Kirtipur, Kathmandu Nepal 2 Centre for Himalayan Studies, UPR 299. CNRS, 7 rue Guy Môquet, 94800 Villejuif, France 3 Université Paris Diderot, GHES, Case 7001, UMR 8586 PRODIG CNRS, Paris Cedex 75013, France 4 ANR-13-SENV-0005-02 PRESHINE (* Corresponding Author: [email protected]) Received: 8 November 2019; Accepted: 22 January 2020; Published: March 2020 Abstract Nepal experienced disastrous earthquake events in 2015. -
Expeditions & Treks 2008/2009
V4362_JG_Exped Cover_AW 1/5/08 15:44 Page 1 Jagged Globe NEW! Expeditions & Treks www.jagged-globe.co.uk Our new website contains detailed trip itineraries 2008 for the expeditions and treks contained in this brochure, photo galleries and recent trip reports. / 2009 You can also book securely online and find out about new trips and offers by subscribing to our email newsletter. Jagged Globe The Foundry Studios, 45 Mowbray Street, Sheffield S3 8EN United Kingdom Expeditions Tel: 0845 345 8848 Email: [email protected] Web: www.jagged-globe.co.uk & Treks Cover printed on Take 2 Front Cover: Offset 100% recycled fibre Mingma Temba Sherpa. sourced only from post Photo: Simon Lowe. 2008/2009 consumer waste. Inner Design by: pages printed on Take 2 www.vividcreative.com Silk 75% recycled fibre. © 2007 V4362 V4362_JG_Exped_Bro_Price_Alt 1/5/08 15:10 Page 2 Ama Dablam Welcome to ‘The Matterhorn of the Himalayas.’ Jagged Globe Ama Dablam dominates the Khumbu Valley. Whether you are trekking to Everest Base Camp, or approaching the mountain to attempt its summit, you cannot help but be astounded by its striking profile. Here members of our 2006 expedition climb the airy south Expeditions & Treks west ridge towards Camp 2. See page 28. Photo: Tom Briggs. The trips The Mountains of Asia 22 Ama Dablam: A Brief History 28 Photo: Simon Lowe Porter Aid Post Update 23 Annapurna Circuit Trek 30 Teahouses of Nepal 23 Annapurna Sanctuary Trek 30 The Seven Summits 12 Everest Base Camp Trek 24 Lhakpa Ri & The North Col 31 The Seven Summits Challenge 13 -
A Statistical Analysis of Mountaineering in the Nepal Himalaya
The Himalaya by the Numbers A Statistical Analysis of Mountaineering in the Nepal Himalaya Richard Salisbury Elizabeth Hawley September 2007 Cover Photo: Annapurna South Face at sunrise (Richard Salisbury) © Copyright 2007 by Richard Salisbury and Elizabeth Hawley No portion of this book may be reproduced and/or redistributed without the written permission of the authors. 2 Contents Introduction . .5 Analysis of Climbing Activity . 9 Yearly Activity . 9 Regional Activity . .18 Seasonal Activity . .25 Activity by Age and Gender . 33 Activity by Citizenship . 33 Team Composition . 34 Expedition Results . 36 Ascent Analysis . 41 Ascents by Altitude Range . .41 Popular Peaks by Altitude Range . .43 Ascents by Climbing Season . .46 Ascents by Expedition Years . .50 Ascents by Age Groups . 55 Ascents by Citizenship . 60 Ascents by Gender . 62 Ascents by Team Composition . 66 Average Expedition Duration and Days to Summit . .70 Oxygen and the 8000ers . .76 Death Analysis . 81 Deaths by Peak Altitude Ranges . 81 Deaths on Popular Peaks . 84 Deadliest Peaks for Members . 86 Deadliest Peaks for Hired Personnel . 89 Deaths by Geographical Regions . .92 Deaths by Climbing Season . 93 Altitudes of Death . 96 Causes of Death . 97 Avalanche Deaths . 102 Deaths by Falling . 110 Deaths by Physiological Causes . .116 Deaths by Age Groups . 118 Deaths by Expedition Years . .120 Deaths by Citizenship . 121 Deaths by Gender . 123 Deaths by Team Composition . .125 Major Accidents . .129 Appendix A: Peak Summary . .135 Appendix B: Supplemental Charts and Tables . .147 3 4 Introduction The Himalayan Database, published by the American Alpine Club in 2004, is a compilation of records for all expeditions that have climbed in the Nepal Himalaya. -
Island Peak Climbing with Everest Base Camp Trek - 19 Days
GPO Box: 384, Ward No. 17, Pushpalal Path Khusibun, Nayabazar, Kathmandu, Nepal Tel: +977-01-4388659 E-Mail: [email protected] www.iciclesadventuretreks.com Island peak climbing with Everest Base Camp Trek - 19 Days Go for Island peak climbing with Everest Base Camp Trek if you are looking to jump a step ahead from trekking to mountaineering. Island peak (Imja Tse) is the most attainable climbing peak. Situated only 10 km away from Mt. Everest summit of Island peak provides 360-degree panorama of many of the highest mountains in the world. Island peak, the most climbed climbing peak of Himalaya is an extension of south end of Mt. Lhotse Shar. If you are looking for trekking in Nepal and want to test mountaineering in Nepal, then Island peak climbing is the perfect ice climbing trip to try first among the 33 "trekking peaks" of Nepal. Although Himalayan Peaks should not be underestimated, Island Peak has the potential to offer the fit and experienced hill walkers a window into the world of mountaineering in the greater ranges. Our Island Peak Climbing with Everest Base Camp provides an excellent experience for first stage mountaineering to novice adventure lovers. Our Island peak climbing with EBC Trek program starts in Kathmandu. We spend a day in Kathmandu preparing for the venture with brief UNESCO heritage sites visit. We take an exhilarating flight to Lukla and start trekking through the classic EBC trekking trail through different beautiful Sherpa villages. During the trek, we spend two nights in Namche and Dingboche to aid acclimatization. Also, we trek to Everest Base Camp to acclimatize ourselves for our Island peak climbing target. -
Debris-Covered Glacier Energy Balance Model for Imja–Lhotse Shar Glacier in the Everest Region of Nepal
The Cryosphere, 9, 2295–2310, 2015 www.the-cryosphere.net/9/2295/2015/ doi:10.5194/tc-9-2295-2015 © Author(s) 2015. CC Attribution 3.0 License. Debris-covered glacier energy balance model for Imja–Lhotse Shar Glacier in the Everest region of Nepal D. R. Rounce1, D. J. Quincey2, and D. C. McKinney1 1Center for Research in Water Resources, University of Texas at Austin, Austin, Texas, USA 2School of Geography, University of Leeds, Leeds, LS2 9JT, UK Correspondence to: D. R. Rounce ([email protected]) Received: 2 June 2015 – Published in The Cryosphere Discuss.: 30 June 2015 Revised: 28 October 2015 – Accepted: 12 November 2015 – Published: 7 December 2015 Abstract. Debris thickness plays an important role in reg- used to estimate rough ablation rates when no other data are ulating ablation rates on debris-covered glaciers as well as available. controlling the likely size and location of supraglacial lakes. Despite its importance, lack of knowledge about debris prop- erties and associated energy fluxes prevents the robust inclu- sion of the effects of a debris layer into most glacier sur- 1 Introduction face energy balance models. This study combines fieldwork with a debris-covered glacier energy balance model to esti- Debris-covered glaciers are commonly found in the Everest mate debris temperatures and ablation rates on Imja–Lhotse region of Nepal and have important implications with regard Shar Glacier located in the Everest region of Nepal. The de- to glacier melt and the development of glacial lakes. It is bris properties that significantly influence the energy bal- well understood that a thick layer of debris (i.e., > several ance model are the thermal conductivity, albedo, and sur- centimeters) insulates the underlying ice, while a thin layer face roughness. -
LIST of INDIAN CITIES on RIVERS (India)
List of important cities on river (India) The following is a list of the cities in India through which major rivers flow. S.No. City River State 1 Gangakhed Godavari Maharashtra 2 Agra Yamuna Uttar Pradesh 3 Ahmedabad Sabarmati Gujarat 4 At the confluence of Ganga, Yamuna and Allahabad Uttar Pradesh Saraswati 5 Ayodhya Sarayu Uttar Pradesh 6 Badrinath Alaknanda Uttarakhand 7 Banki Mahanadi Odisha 8 Cuttack Mahanadi Odisha 9 Baranagar Ganges West Bengal 10 Brahmapur Rushikulya Odisha 11 Chhatrapur Rushikulya Odisha 12 Bhagalpur Ganges Bihar 13 Kolkata Hooghly West Bengal 14 Cuttack Mahanadi Odisha 15 New Delhi Yamuna Delhi 16 Dibrugarh Brahmaputra Assam 17 Deesa Banas Gujarat 18 Ferozpur Sutlej Punjab 19 Guwahati Brahmaputra Assam 20 Haridwar Ganges Uttarakhand 21 Hyderabad Musi Telangana 22 Jabalpur Narmada Madhya Pradesh 23 Kanpur Ganges Uttar Pradesh 24 Kota Chambal Rajasthan 25 Jammu Tawi Jammu & Kashmir 26 Jaunpur Gomti Uttar Pradesh 27 Patna Ganges Bihar 28 Rajahmundry Godavari Andhra Pradesh 29 Srinagar Jhelum Jammu & Kashmir 30 Surat Tapi Gujarat 31 Varanasi Ganges Uttar Pradesh 32 Vijayawada Krishna Andhra Pradesh 33 Vadodara Vishwamitri Gujarat 1 Source – Wikipedia S.No. City River State 34 Mathura Yamuna Uttar Pradesh 35 Modasa Mazum Gujarat 36 Mirzapur Ganga Uttar Pradesh 37 Morbi Machchu Gujarat 38 Auraiya Yamuna Uttar Pradesh 39 Etawah Yamuna Uttar Pradesh 40 Bangalore Vrishabhavathi Karnataka 41 Farrukhabad Ganges Uttar Pradesh 42 Rangpo Teesta Sikkim 43 Rajkot Aji Gujarat 44 Gaya Falgu (Neeranjana) Bihar 45 Fatehgarh Ganges -
World Bank Document
Document of The World Bank Public Disclosure Authorized FOR OFFICIAL USE ONLY Report No: 20634 IMPLEMENTATIONCOMPLETION REPORT (23470) Public Disclosure Authorized ON A CREDIT IN THE AMOUNT OF SDR 48.1 MILLION (US$65 MILLION EQUIVALENT) TO THE GOVERNMENT OF NEPAL FORA POWER SECTOR EFFICIENCY PROJECT Public Disclosure Authorized June 27, 2000 Energy Sector Unit South Asia Sector This documenthas a restricted distribution and may be used by recipients only in the performance of their official duties. Its contents may not otherwise be disclosed without World Bank authorization. Public Disclosure Authorized CURRENCY EQUIVALENTS (ExchangeRate EffectiveFebruary 1999) Currency Unit = Nepalese Rupees (NRs) NRs 62.00 = US$ 1.00 US$ 0.0161 = NRs 1.00 FISCAL YEAR July 16 - July 15 ABBREVIATIONSAND ACRONYMS ADB Asian Development Bank CIWEC Canadian International Water and Energy Consultants DCA Development Credit Agreement DHM Department of Hydrology and Meteorology DOR Department of Roads EA Environmental Assessment EdF Electricite de France EIA Environmental Impact Assessment EIRR Economic Internal Rate of Return EWS Early Warning System GLOF Glacier Lake Outburst Flood GOF Government of France GTZ The Deutsche Gesellschaft fur Technische Zusammenarbeit GWh Gigawatt - hour HEP HydroelectricProject HMGN His Majesty's Government of Nepal HV High Voltage IDA Intemational Development Association KfW Kreditanstalt fur Wiederaufbau KV Kilovolt KWh Kilowatt - hour MCMPP Marsyangdi Catchment Management Pilot Project MHDC Multipower Hydroelectric Development Corporation MHPP Marsyangdi Hydroelectric Power Project MOI Ministiy of Industry MOWR Ministry of Water Resources MW Megawatt NEA Nepal Electricity Authority NDF Nordic Development Fund OEES Office of Energy Efficiency Services O&M Operation & Maintenance PA Performance Agreement PSEP Power Sector Efficiency Project PSR Power Subsector Review ROR Rate of Return SAR Staff Appraisal Report SFR Self Financing Ratio S&R Screening & Ranking Vice President: TMiekoNishiomizu Country Director: Hans M. -
Thermal and Physical Investigations Into Lake Deepening Processes on Spillway Lake, Ngozumpa Glacier, Nepal
water Article Thermal and Physical Investigations into Lake Deepening Processes on Spillway Lake, Ngozumpa Glacier, Nepal Ulyana Nadia Horodyskyj Science in the Wild, 40 S 35th St. Boulder, CO 80305, USA; [email protected] Academic Editors: Daene C. McKinney and Alton C. Byers Received: 15 March 2017; Accepted: 15 May 2017; Published: 22 May 2017 Abstract: This paper investigates physical processes in the four sub-basins of Ngozumpa glacier’s terminal Spillway Lake for the period 2012–2014 in order to characterize lake deepening and mass transfer processes. Quantifying the growth and deepening of this terminal lake is important given its close vicinity to Sherpa villages down-valley. To this end, the following are examined: annual, daily and hourly temperature variations in the water column, vertical turbidity variations and water level changes and map lake floor sediment properties and lake floor structure using open water side-scan sonar transects. Roughness and hardness maps from sonar returns reveal lake floor substrates ranging from mud, to rocky debris and, in places, bare ice. Heat conduction equations using annual lake bottom temperatures and sediment properties are used to calculate bottom ice melt rates (lake floor deepening) for 0.01 to 1-m debris thicknesses. In areas of rapid deepening, where low mean bottom temperatures prevail, thin debris cover or bare ice is present. This finding is consistent with previously reported localized regions of lake deepening and is useful in predicting future deepening. Keywords: glacier; lake; flood; melting; Nepal; Himalaya; Sherpas 1. Introduction Since the 1950s, many debris-covered glaciers in the Nepalese Himalaya have developed large terminal moraine-dammed supraglacial lakes [1], which grow through expansion and deepening on the surface of a glacier [2–4]. -
Everest Base Camp with Island Peak Climbing
Everest Base Camp with Island Peak Climbing Trip Facts Destination Nepal Duration 16 Days Group Size 2-12 Trip Code DWTIS1 Grade Very Strenuous Activity Everest Treks Region Everest Region Max. Altitude Island Peak (6,183m) Nature of Trek Lodge to Lodge /Camping Trekking Activity per Day Approximately 4-6 hrs walking Accomodation Lodge/Tea house/Camping during the trek/climb Start / End Point Kathmandu / Kathmandu Meals Included All Meals (Breakfast, Lunch & Dinner) during the trek Best Season Feb, Mar, Apri, May, June, Sep, Oct, Nov & Dec Transportation Domestic flight (KTM-Lukla-KTM) and private vehicle (Transportation) A Leading Himalayan Trekking & Adventure Specialists TRULY YOUR TRUSTED NEPAL’S TRIP OPERATOR. Ever dreamt of summiting a Himalayan peak like Island Peak (6,189m/20,305ft) via Everest Base Camp (5,364m/17,598ft)? The alluring Himalayas in Nepal is a sight to behold. Trekking to the renowned... Discovery World Trekking would like to recommend all our valuable clients that they should arrive in Kathmandu a day earlier in the afternoon before the day we departed and start our Island Peak Climbing via Everest Base Camp the next day, To make sure that you’ll attend our Official Briefing as an important Pre-meeting. The reason we do so is we want to make sure that you get proper mental guidance and necessary information just to have a recheck of equipment and goods for the journey to make sure you haven't forgotten anything and if forgotten, then make sure that you are provided with those things ASAP on that very day. -
Changes of Glaciation in the Sagarmatha National Park (Nepal) During the Last 30 Years
Landform Analysis, Vol. 10: 85–94 (2009) Changes of glaciation in the Sagarmatha National Park (Nepal) during the last 30 years Rudolf Midriak* Matej Bel University, Institute of Science and Research, Research Institute of Landscape and Regions, Cesta na amfiteáter 1, 974 01 Banská Bystrica, Slovak Republic Abstract: Author, as a scientific participant of the first Czech-Slovak Expedition to the Mt. Everest in 1984, focuses on the glaciation in the Sagarmatha National Park (the Central Himalayas, Nepal) in 1978 (Fig. 1 and Table 1) and compares it with the present-day state. Despite overwhelming majority of the papers bearing data on the fastest retreat of the Mt. Everest’s glaciers it can be stated that obvious changes of the covering glaciers were not recorded in the Sagarmatha National Park (34.2% in the year of 1978 and 39.8% in the year of 2009). At present, for 59 sections of 18 valley glaciers (Nangpa, Melung, Lunag, Chhule, Sumna, Langmoche, Ngozumpa, Gyubanar, Lungsampa, Khumbu, Lobuche, Changri Shar, Imja, Nuptse, Lhotse Nup, Lhotse, Lhotse Shar and Ama Dablam) their length of retreat during 30 years was recorded: at 5 sections from 267 m to 1,804m (the width of retreat on 24sections being from 1 m to 224m), while for 7 sections an increase in length from 12 m to 741m was noted (the increase of glacier width at 23 sections being from 1 m to 198 m). More important than changes in length and/or width of valley glaciers are both the depletion of ice mass and an intensive growth of the number lakes: small supraglacial ponds, as well as dam moraine lakes situated below the snowline (289 lakes compared to 165 lakes in the year of 1978). -
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.