Seasonal Rapid Advancement of Surging Glaciers in Karakoram Range
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Inventory and GLOF Susceptibility of Glacial Lakes in Hunza River Basin, Western Karakorum
remote sensing Article Inventory and GLOF Susceptibility of Glacial Lakes in Hunza River Basin, Western Karakorum Fakhra Muneeb 1 , Siddique Ullah Baig 2, Junaid Aziz Khan 3 and Muhammad Fahim Khokhar 1,* 1 Institute of Environmental Sciences and Engineering, National University of Sciences and Technology, Islamabad 44000, Pakistan; [email protected] 2 High Mountain Research Center, Department of Development Studies COMSATS University Islamabad, Abbottabad 22060, Pakistan; [email protected] 3 Institute of Geographical Information System, National University of Sciences and Technology, Islamabad 44000, Pakistan; [email protected] * Correspondence: [email protected]; Tel.: +92-51-90854308 Abstract: Northern latitudes of Pakistan are warming at faster rate as compared to the rest of the country. It has induced irregular and sudden glacier fluctuations leading to the progression of glacial lakes, and thus enhancing the risk of Glacier Lake Outbursts Floods (GLOF) in the mountain systems of Pakistan. Lack of up-to-date inventory, classification, and susceptibility profiles of glacier lakes and newly formed GLOFs, are few factors which pose huge hindrance towards disaster preparedness and risk reduction strategies in Pakistan. This study aims to bridge the existing gap in data and knowledge by exploiting satellite observations, and efforts are made to compile and update glacier lake inventories. GLOF susceptibility assessment is evaluated by using Analytical Hierarchy Process (AHP), a multicriteria structured technique based on three susceptibility contributing factors: Geographic, topographic, and climatic. A total of 294 glacial lakes are delineated with a total area of 7.85 ± 0.31 km2 for the year 2018. -
Executive Summary on Attabad Landslide Survey in Hunza 7-17 April 2010
Executive summary on Attabad landslide survey in Hunza 7-17 April 2010 Short introduction This report provides a summary of the key findings of a short field visit (10-13 April, 2010) to the Attabad landslide and damming site in the Hunza Valley. This report provides some risk/hazard management recommendations regarding Saret and Gogal villages, upstream and downstream of the Hunza river, elaborated based on our field observations. An international group of geologists and researchers were involved in the survey: Dr. Chiara Calligaris – Geosciences Departement (DIGEO) - Trieste University (Italy) Mr. Michele Comi – Ev-K2-CNR (Italy) Dr. Shahina Tariq – Baharia University (Islamabad – Pakistan) Mr. Furrukh Bashir – Pakistan Meteorological Department Mr. Deear Karim – FOCUS Humanitarian Assistance Mr. Hawas Khan – KIU University (Gilgit – Pakistan) Some documentation on the landslide is already available (Petley, 2010) and we begin our report based on Petley’s findings so as to avoid repeating previously made considerations. Background of potential glacial lake outburst floods in the Hunza Valley Sixty historical damburst events have been reported in the northern part of Pakistan. This gives an average recurrence frequency of about one event every 3 year. For ice-dam failures with floods exceeding 20,000 cumecs (9 events in 100 yrs), the apparent frequency is one event every 11 years. For floods exceeding 11,000 cumecs (17 events in 100 yrs) the apparent frequency is one event 1 every 6 years (POE, 1988). The majority of recorded damburst flood events over the last 200 years have been glacial lake outburst floods. A few events have resulted from the failure of landslide dams, the most well known being those of June 1841 and August 1858. -
A Case Study of Gilgit-Baltistan
The Role of Geography in Human Security: A Case Study of Gilgit-Baltistan PhD Thesis Submitted by Ehsan Mehmood Khan, PhD Scholar Regn. No. NDU-PCS/PhD-13/F-017 Supervisor Dr Muhammad Khan Department of Peace and Conflict Studies (PCS) Faculties of Contemporary Studies (FCS) National Defence University (NDU) Islamabad 2017 ii The Role of Geography in Human Security: A Case Study of Gilgit-Baltistan PhD Thesis Submitted by Ehsan Mehmood Khan, PhD Scholar Regn. No. NDU-PCS/PhD-13/F-017 Supervisor Dr Muhammad Khan This Dissertation is submitted to National Defence University, Islamabad in fulfilment for the degree of Doctor of Philosophy in Peace and Conflict Studies Department of Peace and Conflict Studies (PCS) Faculties of Contemporary Studies (FCS) National Defence University (NDU) Islamabad 2017 iii Thesis submitted in fulfilment of the requirement for Doctor of Philosophy in Peace and Conflict Studies (PCS) Peace and Conflict Studies (PCS) Department NATIONAL DEFENCE UNIVERSITY Islamabad- Pakistan 2017 iv CERTIFICATE OF COMPLETION It is certified that the dissertation titled “The Role of Geography in Human Security: A Case Study of Gilgit-Baltistan” written by Ehsan Mehmood Khan is based on original research and may be accepted towards the fulfilment of PhD Degree in Peace and Conflict Studies (PCS). ____________________ (Supervisor) ____________________ (External Examiner) Countersigned By ______________________ ____________________ (Controller of Examinations) (Head of the Department) v AUTHOR’S DECLARATION I hereby declare that this thesis titled “The Role of Geography in Human Security: A Case Study of Gilgit-Baltistan” is based on my own research work. Sources of information have been acknowledged and a reference list has been appended. -
Culturable Diversity of Psychrophilic Bacteria from Different Glaciers of Karakoram Mountain Range and Role of Cell Membrane Fatty Acids in Cold Adaptation
Culturable Diversity of Psychrophilic Bacteria from Different Glaciers of Karakoram Mountain Range and Role of Cell Membrane Fatty Acids in Cold Adaptation By Noor Hassan Department of Microbiology Faculty of Biological Sciences Quaid-I-Azam University Islamabad, Pakistan 2020 Culturable Diversity of Psychrophilic Bacteria from Different Glaciers of Karakoram Mountain Range and Role of Cell Membrane Fatty Acids in Cold Adaptation A thesis Submitted in partial fulfillment of the requirements for the Degree of DOCTOR OF PHILOSOPHY IN MICROBIOLOGY By Noor Hassan Department of Microbiology Faculty of Biological Sciences Quaid-I-Azam University Islamabad, Pakistan 2020 In the name of ALLAH, Most Gracious, Most Merciful. DEDICATION Dedicated to My Beloved Parents And Wife Author’s Declaration I Mr. Noor Hassan hereby state that my Ph.D thesis titled “Culturable Diversity of Psychrophilic Bacteria from Different Glaciers of Karakoram Mountain Range and Role of Cell Membrane Fatty Acids in Cold Adaptation” is my own work and has not been submitted previously by me for taking any degree from Quaid-i-Azam University, Islamabad, Pakistan. At any time if my statement is found to be incorrect even after I Graduate, the University has the right to withdraw my Ph.D degree. Mr. Noor Hassan Date: 22-07-2020 Plagiarism Undertaking “Culturable Diversity of Psychrophilic Bacteria from Different Glaciers of Karakoram Mountain Range and Role of Cell Membrane Fatty Acids in Cold Adaptation” is solely my research work with no significant contribution from any other person. Small contribution / help wherever taken has been duly acknowledged and that complete thesis has been written by me. -
Spatial Distribution of Debris Cover and Its Impacts in the Hunza River Basin
EGU2020-6650 https://doi.org/10.5194/egusphere-egu2020-6650 EGU General Assembly 2020 © Author(s) 2021. This work is distributed under the Creative Commons Attribution 4.0 License. Spatial distribution of debris cover and its impacts in the Hunza River Basin Yong Zhang1, Shiyin Liu2, and Xin Wang1 1Hunan University of Science and Technology, Xiangtan, China ([email protected]) 2Institute of International Rivers and Eco-Security, Yunnan University, Yunnan, China Hunza River is an important tributary of the Indus River, which contributes ~12% of the total runoff in the upper Indus River. 25% of Hunza River basin is covered by glaciers. The Karakoram Highway (KKH) connecting Pakistan and China goes from the Khunjerab Pass and down to the Gilgit, which is an important section of the Pakistan-China Economic Corridor in the high mountains. Many glaciers in this region are extensively covered by supraglacial debris, which strongly influences glacier melting and its spatial pattern. Changes in these glaciers may threaten the stability of the highway subgrade through meltwater floods, unpredictable behaviors of glacier terminals as well as potential outburst floods of glacier lakes near glaciers. Therefore, predicting runoff, response to climate change and risk of outburst floods of debris-covered glaciers requires different treatment to that of clean glaciers in the Hunza River Basin. In this study, we estimate the thermal resistance of the debris layer for the whole basin based on ASTER images. Our results reveal that debris- covered glaciers account for 69% and 30% of the total number and area in the basin. Using a physically-based debris-cover effect assessment model, we find different debris-cover effects on different glaciers, with important implications for the morphology and evolution of glacier hydrological system and associated hazards. -
Karakorum Himalaya: Sourcebook for a Protected Area
7 Karakorum Himalaya: Sourcebook for a Protected Area Nigel J. R. Allan 8 The views expressed in this publication are not necessarily those of IUCN. IUCN-The World Conservation Union, Pakistan 1 Bath Island Road, Karachi 75530 © 1995 by IUCN-The World Conservation Union, Pakistan All rights reserved ISBN 969-8141-13-8 Contents Preface v Introduction 1 1 HISTORY Natural Heritage 11 Geology 11 Glaciology 14 Associative Cultural Landscape 17 Local Ideas and Beliefs about Mountains 17 Culturally Specific Communication Networks 20 2 DESCRIPTION AND INVENTORY Physiography and Climate 23 Flora 24 Fauna 25 Juridical and Management Qualities 29 3 PHOTOGRAPHIC AND CARTOGRAPHIC DOCUMENTATION Historial Photographs 33 Large Format Books 33 Landscape Paintings 33 Maps and Nomenclature 34 4 PUBLIC AWARENESS Records of Expeditions 37 World Literature and History 43 Tourism 52 Scientific and Census Reports 56 Guidebooks 66 International Conflict 66 5 RELATED BIBLIOGRAPHIC MATERIALS 69 Author Index 71 Place Index 81 iii iv4 5 Preface This sourcebook for a protected area has its origins in a lecture I gave at the Environment and Policy Institute of the East-West Center in Honolulu in 1987. The lecture was about my seasons of field work in the Karakorum Himalaya. Norton Ginsberg, the director of the Institute, alerted me to the fact that the Encyclopedia Britannica would be revising their entries on Asian mountains shortly and suggested that I update the Karakorum entry. The eventual publication of that entry under my name (Allan 1992), however, omitted most of the literature references I had accumulated. As my reference list continued to expand I decided to order them in some coherent fashion and publish them as a sourcebook to coincide with the IUCN workshop on mountain protected areas in Skardu in September 1994. -
Pinnacle Club Journal
© Pinnacle Club and Author All Rights Reserved THE PINNACLE CLUB JOURNAL No. 20 1985 - 87 © Pinnacle Club and Author All Rights Reserved THE PINNACLE CLUB JOURNAL 1985 - 87 Edited by Stephanie Rowland © Pinnacle Club and Author All Rights Reserved THE PINNACLE CLUB Founded 1921 OFFICERS AND COMMITTEE 1987 President ANNABELLE BARKER Hafod Aur, Pont y Pant, Dolwyddelen, Gwynedd. (06906 272) Vice President Sheila Cormack Hon. Secretary Jean Drummond 10 Crichton Cottages, Crichton, Pathhead, Midlothian. (0875 32 0445) Hon. Treasurer Stella Adams Hon. Meets Secretary Denise Wilson Hon. Hut Secretary Rhona Lampard Hon. Editor Stephanie Rowland Springfield, Culbokie, Dingwall, Ross-shire. (034987 603) Committee Tansy Hardy Sheila Lockhart Geraldine Westrupp Sue Williscroft Sally Kier Betty Whithead (Dinner Organiser) Hon. Auditor Hon. Librarian Ann Wheatcroft Avis Reynolds © Pinnacle Club and Author All Rights Reserved Contents Page How I Became Brave Annabelle Barker ..................... 5 True Grit Dave Woolley and Andy Llewelyn ..................... 12 An Apology By a Mere Man Anon ..................................... 16 'Burro Perdido' and other Escapades Angela Soper .......................... 18 A Reconaissance of Ananea Belinda Swift ........................... 22 Sardines and Apricots: a month in Hunza Margaret Clennett .................... 25 The Coast to Coast Walk Dorothy Wright ....................... 29 British Gasherbrum IV Chris Watkins and Expedition 1986 Rhona Lampard .................... 31 Two Walks in Kashmir Sheila McKemmie -
Community Initiated Water Project for Irrigation and Drinking Yaz Sam Hussaini Gojal (2010-2011)
Community Initiated Water Project for Irrigation and Drinking Yaz sam Hussaini Gojal (2010-2011) ALI REHMAT Hussaini Organization for Local Development (HOLD) Hussaini Gojal, Hunza, Gilgit-Baltistan Total Population 639 Male 333 Female 306 Household 89 Altitude 2556m Source: Field Survey 2007 Gilgit-Baltistan Hussaini Village is situated in Hunza valley, 145 km North of Gilgit and 45 km from Ali Abad in Central Hunza. Hunza River flows in to the east while the Karakoram Highway (KKH) passes to its west. Hussaini Village is situated on 74°52'23.42" East longitude and 36°25'29.14" North latitude at an altitude of 2,556 meters above sea level. South of Hussaini is Gulmit (the headquarters of Gojal magistracy - tehsil), Ghulkin is to the southwest, while Passu is in the north with famous Batura glacier. Hussaini glacier is located to the west with famous Shisper peak, 7611meters. Hussaini is a small village of Gojal (Upper Hunza) in tGilgit-Baltistan. It is situated on the both banks of Hunza River. The old main village is on the western-bank and at the lateral moraine of Hussaini glacier and below Borith Lake. The newly irrigated land, called Zarabod, is on the left bank. The total population is 649 souls, living in 87 households. (2008) Hussaini is located in the center of the Karakoram Range, surrounded by high mountains having the heights of more than 7000 meters. Most of the peaks, remain snow covered throughout the year. Shishper (7611 m) is the highest peak of the study area. The rock exposed in the area is mainly Slate i.e. -
Report on Shimshal Nature Trust (SNT) Ghojal, Northern Areas, Pakistan
Report on Shimshal Nature Trust (SNT) Ghojal, Northern Areas, Pakistan Inayat Ali and Dr. David Butz 73ºE 74º 75º 76ºE TAJIKISTAN CHINA CHINA AFGHANISTAN (XINJIANG) AFGHANI-STAN (WAKHAN) NEPAL 37ºN PAKISTAN Khunjerab Pass INDIA Misgar Khunjer ab R. G h ujerab SOST R. Darkot L Indian Ocean A ISHKOMAN . J R Sh imsha O l Shimshal T GPasu Pass Shimshal R HUNZAGULMIT a . z YASIN KARIMABAD n I (Baltit) u H R r H e Chalt is E G h i z e r R i v UYUM par GUPIS G R. F G Hopar Gakuch i l NAGER g i t G Hispar R R Nomal i v A O Shandur e N L r Pass N 36º N O I T G R I ARANDU E T GILGIT N R H . T - R W a P l E n A R S e Askole T g r O i V r a Dasso B r I N C E R D BUNJI I a l d u . n d R . u s S T A h s R i v i t e g r H o Legend I a n r SAZIN d u u S r R s s R i v e r R . SHIGAR Northern Areas . h CHILAS I e Shimshal territory ASTOR R . District boundary DASU T S SKARDU I h y . n o k R Paved road d L u KHAPALU Unpaved road s A R 0 50 km 35ºN i v e B r Figure 1. Location of Shimshal in Northern Pakistan (Courtesy David Butz; drafted by Loris Gasparotto) Introduction and Context Shimshal is a farming and herding community of some 1700 inhabitants, situated at the northeastern extreme of both the former principality of Hunza (now part of Gilgit Administrative District), and the modern state of Pakistan (see Figure 1). -
Hussaini HUSSAINI Government of NWFP HUSSAINIHUSSAINI Oasis on the Karakoram Highway NA Forestry, Parks and Wildlife Department HUSSAINI NA Administration OASIS
© all photographs Matthieu Paley NWFP Wildlife Department Suspension Bridge near Hussaini HUSSAINI Government of NWFP HUSSAINIHUSSAINI Oasis on the Karakoram Highway NA Forestry, Parks and Wildlife Department HUSSAINI NA Administration OASIS. I CAN THINK OF NO BETTER WORD FOR THE STARTLING, DELIGHTFUL LITTLE PLACES, FRUITFUL AND GREEN, WHICH THE TRAVELLER “FINDS STRUNG AT INTERVALS OF TEN MILES OR SO ALONG THESE ARID KARAKORAM GORGES. Ian Stephens, “Horned Moon” ” p10 all maps by Mareile Paley. Produced with the help of WWF GIS-Lab, ESRI and ERDAS imagine all maps by Mareile Paley. HUSSAINI FACTS location Gojal, Upper Hunza, on Karakoram Highway (KKH) nearest town Gulmit, Gojal public transport any transport on KKH going between Aliabad and Passu main settlements Hussaini (also known as Sesoni), Zarabad accommodation Hussaini Village (simple guesthouse) supplies best to bring food and supplies from Sost, Aliabad or Gilgit population 81 households, 575 people indigenous language Wakhi indigenous wildlife snow leopard, Himalayan ibex, red fox, wolf, Himalayan snow cock, rock partridge common plant species juniper, willow, poplar, wild roses, seabuckthorn Hussaini village with view on Zarabad across the Hunza River INTRODUCTION INTRODUCTIONINTRODUCTIONINTRODUCTIONINTRODUCTION On its last stretch towards China, the Karakoram Highway (KKH) winds its way along the Hunza For those loving nature and wishing to forget about the stresses of every day life, nearby Borit River through the narrow gorges of Gojal, the northernmost region of Pakistan. Past Karimabad, Lake makes an ideal place to relax for a few days, to study the birds and plants or to simply enjoy the center of Hunza and farther through Gulmit and past Ghulkin, the road then passes through the peaceful environment. -
The Attabad Landslide and the Politics of Disaster in Gojal, Gilgit-Baltistan
The Attabad landslide and the politics of disaster in Gojal, Gilgit-Baltistan Martin Sökefeld 1. Introduction On 4th of January, 2010, a gigantic mass of rocks came down the slope above Attabad, a village in the high mountain area of Gilgit-Baltistan, northern Pakistan. The large-scale landslide filled the narrow valley of the Hunza-River, burying part of the village and the neighbouring hamlet of Sarat. It did not come unanticipated. Already years before widening cracks had appeared on the slope. Attabad had been evacuated but a number of families returned. The landslide claimed nineteen lives. While this was disastrous enough, a second disaster de- veloped in consequence of the first. The debris created a huge barrier of more than hundred metres height and one kilometre width which completely blocked the flow of the Hunza-River and also buried the Karakorum Highway (KKH), the only road link to the area. Consequentially, the whole area upstream, the tahsil (subdistrict) of Gojal, was cut off from access to Pakistan. In the subse- quent weeks a lake developed behind the barrier which continued to grow till August 2010. Until then it had reached a length of almost thirty kilometres. The lake inundated one village completely and four others partly. Large sections of the KKH came under water so that also communication between the villages was severely disrupted. A growing body of literature of the anthropology of disasters has pointed out that “natural disasters” are in fact not simply “natural”. Taking mostly a political ecology perspective which emphasises the close connection, interdependency and, practically, mutual constitution of “nature” and “society”, it has been ar- gued that disasters occur when events that are characterised as being “natural” (i.e. -
Investigation of Isotopes and Hydrological Processes in Indus River System, Pakistan
PINSTECH- 215 INVESTIGATION OF ISOTOPES AND HYDROLOGICAL PROCESSES IN INDUS RIVER SYSTEM, PAKISTAN Manzoor Ahmad Zahid Latif Jamil Ahmad Tariq Waheed Akram Muhammad Rafique . Isotope Application Division Directorate of Technology Pakistan Institute of Nuclear Science and Technology P.O. Nilore, Islamabad, Pakistan November, 2009 ABSTRACT Indus River, one of the longest rivers in the World, has five major eastern tributaries viz. Bias, Sutlej, Ravi, Chenab and Jhelum) while many small rivers join it from the right side among which Kabul River is the biggest with its main tributaries, the Swat, Panjkora and Kunar. All these main rivers are perennial and originate from the mountains. Basic sources of these rivers are snowmelt, rainfall and under certain conditions seepage from the formations. Different water sources are labeled with different isotope signatures which are used as fingerprints for identifying source and movement of water, geochemical and/or hydrological processes, and dynamics (age of water). Monitoring of isotopes in rivers can also enhance understanding of the water cycle of large river basins and to assess impacts of environmental and climatic changes on the water cycle. Therefore, a national network of suitable stations was established for isotopic monitoring of river waters in Indus Basin with specific objectives to study temporal variations of isotopes (2H, 18O and 3H), understand water cycles and hydrological processes in the catchments of these rivers, and to develop comprehensive database to support future isotope-based groundwater studies in the basin on recharge mechanism, water balance and monitoring of ongoing environmental changes. Water samples were collected during 2002-2006 on monthly basis from more than 20 stations at the major rivers and analyzed for 18O, 2H and 3H isotopes.