Glacier Monitoring in Ladakh and Zanskar, Northwestern India
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REPORT on ACCIDENT to M/S AERIAL SERVICES Pvt
REPORT ON ACCIDENT TO M/S AERIAL SERVICES Pvt. Ltd. SUPER KINGAIR B-200 AIRCRAFT , VT-EIE , ON JULY 29, 2000 , NEAR VILLAGE JHUGGI , H.P. BY A.K.CHOPRA INSPECTOR OF ACCIDENTS CONTENTS II*11 Important`timings 0. Summary 00. Previous History 1. Factual Information 1.1 History of f ight 1.2 Injuries to Person 1.3 Damage to Aircraft 1.4 Other Dama ;-,es 1.5 Personnel Ir,formation 1.6 Aircraft Information 1.7 Meteorolopical Information 1.8 Aids to Nay gation 1.9 Communication 1.10 Aerodrome information 1.11 Flight Rece,.der 1.12 Wreckage and Impact Information 1.13 Medical anc. Pathological Information 1.14 Fire 1.15 Survival pects 1.16 Tests 2. ANALYST, 2.1 Aircraft Serviceability 2.2 Pre-flight Preparations 2.3 Enroute Weather 2.4 Flight Path 2.5 Purpose of Flight 2.6 Regulatorj Control 2.7 Facilities at Kullu Airport 2.8 Chandigarli- Kullu Route 2.9 ATC Control 2.10 Coordination with Airforce 2.11 Role of PoEice 2.12 Maintenam Practices - 2.13 Investigation Process 3. FINDINGS 4. CAUSE OF ACCIDENT 5. RECOMMENDATIONS COMPLIANCE WITH REGULATIONS 2 Important Timings 0657 - Start up asked from Delhi Ground. Message from Kullu about weather given. 0704 - Again asked for start up as emergency evacuation is there. 0708 - Taxying 0712 - Airborne 0725 - First contact with Chandigarh ATC 0728 - 36 miles from SP Radar F 170 0730 - 28 miles from SP Radar, changed over by Delhi Radar. 0731 - Asked 5 - 7 miles deviation left of track from Chandigarh ATC 0736 - Asked descent from Chandigarh ATC to F 105 0738 - Ow-head SP F 170 0739 - Set course directly to Kullu 0741 - Reported F 105 requested descent to F 90 - 22 miles East abeam ,Chandigarh 0750 - Reported F 90 0755 - HF contact with Kullu passed ETA 0808 - position 42 miles descending F 90 0758 - LG;t Chandigarh VOR - 35 miles to Kullu - requested change over from Chandigarh ATC. -
Identification of Glacial Flood Hazards in Karakoram Range Using Remote Sensing Technique and Risk Analysis
IDENTIFICATION OF GLACIAL FLOOD HAZARDS IN Arshad Ashraf*† , Rakhshan Roohi*, Rozina Naz* KARAKORAM RANGE USING REMOTE SENSING and Naveed Mustafa* TECHNIQUEAND RISK ANALYSIS ABSTRACT importance of this situation has magnified over the past decades due to increase in numbers of glacial Glacial Lake Outburst Floods (GLOFs) are great lakes that are formed at the glacier terminus. Thirty- hazard for the downstream communities in context of five destructive out-burst floods have been recorded changing climatic conditions in the glaciated region of for the Karakoram Range during the past two hundred Pakistan. The remote sensing data of Landsat ETM+ years (Hewitt, 1982). Some of the ice dams may have was utilized for the identification of glacial lakes been the result of glacier surges. There is susceptible to posing GLOF hazard in Karakoram unambiguous evidence of large reservoirs ponded by Range. Overall, 887 glacial lakes are identified in 18 glaciers. Kelly (1988) outlines the historical different river-basins of Karakoram Range, out of development and disappearance of Virjerab lake in which 16 lakes are characterized as potentially Hunza due to glacial motion. There occurred a series dangerous in terms of GLOF. The analysis of of GLOF events in upper Hunza valley, central community’s response to GLOF events of 2008 in the Karakoram Range, within short time periods during central Karakoram Range indicated gaps in 2008 that had a devastating effect on the nearby coordination and capacity of the local communities to communities (Roohi, Ashraf, Mustafa and Mustafa, cope with such natural hazards. A regular monitoring 2008). The people residing at considerable distances of hot spots and potential GLOF lakes along with downstream from the unstable lakes are facing a capacity-building of local communities and institutions serious threat to their lives and property. -
Impact of Climatic Change on Agro-Ecological Zones of the Suru-Zanskar Valley, Ladakh (Jammu and Kashmir), India
Journal of Ecology and the Natural Environment Vol. 3(13), pp. 424-440, 12 November, 2011 Available online at http://www.academicjournals.org/JENE ISSN 2006 - 9847©2011 Academic Journals Full Length Research Paper Impact of climatic change on agro-ecological zones of the Suru-Zanskar valley, Ladakh (Jammu and Kashmir), India R. K. Raina and M. N. Koul* Department of Geography, University of Jammu, India. Accepted 29 September, 2011 An attempt was made to divide the Suru-Zanskar Valley of Ladakh division into agro-ecological zones in order to have an understanding of the cropping system that may be suitably adopted in such a high altitude region. For delineation of the Suru-Zanskar valley into agro-ecological zones bio-physical attributes of land such as elevation, climate, moisture adequacy index, soil texture, soil temperature, soil water holding capacity, slope, vegetation and agricultural productivity have been taken into consideration. The agricultural productivity of the valley has been worked out according to Bhatia’s (1967) productivity method and moisture adequacy index has been estimated on the basis of Subrmmanyam’s (1963) model. The land use zone map has been superimposed on moisture adequacy index, soil texture and soil temperature, soil water holding capacity, slope, vegetation and agricultural productivity zones to carve out different agro-ecological boundaries. The five agro-ecological zones were obtained. Key words: Agro-ecology, Suru-Zanskar, climatic water balance, moisture index. INTRODUCTION Mountain ecosystems of the world in general and India in degree of biodiversity in the mountains. particular face a grim reality of geopolitical, biophysical Inaccessibility, fragility, diversity, niche and human and socio economic marginality. -
Distribution of Bufotes Latastii (Boulenger, 1882), Endemic to the Western Himalaya
Alytes, 2018, 36 (1–4): 314–327. Distribution of Bufotes latastii (Boulenger, 1882), endemic to the Western Himalaya 1* 1 2,3 4 Spartak N. LITVINCHUK , Dmitriy V. SKORINOV , Glib O. MAZEPA & LeO J. BORKIN 1Institute Of Cytology, Russian Academy Of Sciences, Tikhoretsky pr. 4, St. Petersburg 194064, Russia. 2Department of Ecology and EvolutiOn, University of LauSanne, BiOphOre Building, 1015 Lausanne, Switzerland. 3 Department Of EvOlutiOnary BiOlOgy, EvOlutiOnary BiOlOgy Centre (EBC), Uppsala University, Uppsala, Sweden. 4ZoOlOgical Institute, Russian Academy Of Sciences, Universitetskaya nab. 1, St. PeterSburg 199034, Russia. * CorreSpOnding author <[email protected]>. The distribution of Bufotes latastii, a diploid green toad species, is analyzed based on field observations and literature data. 74 localities are known, although 7 ones should be confirmed. The range of B. latastii is confined to northern Pakistan, Kashmir Valley and western Ladakh in India. All records of “green toads” (“Bufo viridis”) beyond this region belong to other species, both to green toads of the genus Bufotes or to toads of the genus Duttaphrynus. B. latastii is endemic to the Western Himalaya. Its allopatric range lies between those of bisexual triploid green toads in the west and in the east. B. latastii was found at altitudes from 780 to 3200 m above sea level. Environmental niche modelling was applied to predict the potential distribution range of the species. Altitude was the variable with the highest percent contribution for the explanation of the species distribution (36 %). urn:lSid:zOobank.Org:pub:0C76EE11-5D11-4FAB-9FA9-918959833BA5 INTRODUCTION Bufotes latastii (fig. 1) iS a relatively cOmmOn green toad species which spreads in KaShmir Valley, Ladakh and adjacent regiOnS Of nOrthern India and PakiStan. -
Monsoon-Influenced Glacier Retreat in the Ladakh Range, Jammu And
Geophysical Research Abstracts Vol. 18, EGU2016-166, 2016 EGU General Assembly 2016 © Author(s) 2015. CC Attribution 3.0 License. Monsoon-influenced glacier retreat in the Ladakh Range, Jammu and Kashmir Tom Chudley, Evan Miles, and Ian Willis Scott Polar Research Institute, University of Cambridge ([email protected]) While the majority of glaciers in the Himalaya-Karakoram mountain chain are receding in response to climate change, stability and even growth is observed in the Karakoram, where glaciers also exhibit widespread surge- type behaviour. Changes in the accumulation regime driven by mid-latitude westerlies could explain such stability relative to the monsoon-fed glaciers of the Himalaya, but a lack of detailed meteorological records presents a challenge for climatological analyses. We therefore analyse glacier changes for an intermediate zone of the HKH to characterise the transition between the substantial retreat of Himalayan glaciers and the surging stability of Karakoram glaciers. Using Landsat imagery, we assess changes in glacier area and length from 1991-2014 across a ∼140 km section of the Ladakh Range, Jammu and Kashmir. Bordering the surging, stable portion of the Karakoram to the north and the Western Himalaya to the southeast, the Ladakh Range represents an important transitional zone to identify the potential role of climatic forcing in explaining differing glacier behaviour across the region. A total of 878 glaciers are semi-automatically identified in 1991, 2002, and 2014 using NDSI (thresholds chosen between 0.30 and 0.45) before being manually corrected. Ice divides and centrelines are automatically derived using an established routine. Total glacier area for the study region is in line with that Randolph Glacier Inventory (RGI) and ∼25% larger than the GLIMS Glacier Database, which is apparently more conservative in assigning ice cover in the accumulation zone. -
Photographic Archives in Paris and London Pascale Dollfus
Photographic archives in Paris and London Pascale Dollfus To cite this version: Pascale Dollfus. Photographic archives in Paris and London. European bulletin of Himalayan research, University of Cambridge ; Südasien-Institut (Heidelberg, Allemagne)., 1999, Special double issue on photography dedicated to Corneille Jest, pp.103-106. hal-00586763 HAL Id: hal-00586763 https://hal.archives-ouvertes.fr/hal-00586763 Submitted on 10 Feb 2018 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. EBHR 15- 16. 1998- 1999 PHOTOGRAPHIC ARCHIVES IN PARIS AND epal among the Limbu. Rai. Chetri. Sherpa, Bhotiya and Sunuwar. LONDO ' Both these collections encompa'\s pictures of land flY PA CALE DOLL FUSS scapes. architecture. techniques. agriculture. herding, lrade, feslivals. shaman practices. rites or passage. etc. In addition to these major collecti ons. once can find I. PUOTOGRAPfIIC ARCIUVES IN PARIS 350 photographs taken in 1965 by Jaeques Millot. (director of the RCP epal) in the Kathmandu Valley. Photographic Library ("Phototheque"), Musee de approx. 110 photographs (c. 1966-67) by Mireille Helf /'lIommc. fer. related primari Iy to musicians caSles, 45 photo 1'1. du Trocadero. Paris 750 16. graphs (1967-68) by Marc Gaborieau. -
Leh Highlights
LEH HIGHLIGHTS 08 NIGHTS / 09 DAYS DELHI – LEH – SHEY – HEMIS – THIKSEY – LEH – NUBRA – ALCHI – LIKIR – LAMAYURU – PANGONG - LEH – DEPARTURE TOUR PROGRAMME: Day 01 ARRIVE DELHI Arrive at Delhi International airport. Upon arrival, you will be met by your car with chauffeur for the short transfer to your hotel for night stay. Rest of the day free. Night in Delhi Day 02: Fly to Leh (via Flight) (11562 i.e. 3524 mts) After breakfast, in time fly to Leh. On arrival you will be met our representative and drive towards the hotel. Welcome drink on arrival. We recommend you completely relax for the rest of the day to enable yourselves to acclimatize to the rarefied air at the high altitude. Dinner and night stay at Hotel in Leh. Day 03: Leh to Shey/Hemis/ Thiksey – Leh (70 Km. (3-4 hours Approx.) After breakfast visit Shey, Hemis, & Thiksey Monastery.Hemis – which is dedicated to Padmasambhava, what a visitor can observes a series of scenes in which the lamas, robed in gowns of rich, brightly colored brocade and sporting masks sometimes bizarrely hideous, parade in solemn dance and mime around the huge flag pole in the center of the courtyard to the plaintive melody of the Shawn. Thiksey –is one of the largest and most impressive Gompas. There are several temples in this Gompa containing images, stupas and exquisite wall paintings. It also houses a two ‐ storied statue of Buddha which has the main prayer hall around its shoulder. Shey – it was the ancient capital of Ladakh and even after Singe Namgyal built the more imposing palace at Leh, the kings continued to regard Shey, as their real home. -
Statistical Handbook District Kargil 2018-19
Statistical Handbook District Kargil 2018-19 “STATISTICAL HANDBOOK” DISTRICT KARGIL UNION TERRITORY OF LADAKH FOR THE YEAR 2018-19 RELEASED BY: DISTRICT STATISTICAL & EVALUATION OFFICE KARGIL D.C OFFICE COMPLEX BAROO KARGIL J&K. TELE/FAX: 01985-233973 E-MAIL: [email protected] Statistical Handbook District Kargil 2018-19 THE ADMINISTRATION OF UNION TERRITORY OF LADAKH, Chairman/ Chief Executive Councilor, LAHDC Kargil Phone No: 01985 233827, 233856 Message It gives me immense pleasure to know that District Statistics & Evaluation Agency Kargil is coming up with the latest issue of its ideal publication “Statistical Handbook 2018-19”. The publication is of paramount importance as it contains valuable statistical profile of different sectors of the district. I hope this Hand book will be useful to Administrators, Research Scholars, Statisticians and Socio-Economic planners who are in need of different statistics relating to Kargil District. I appreciate the efforts put in by the District Statistics & Evaluation Officer and the associated team of officers and officials in bringing out this excellent broad based publication which is getting a claim from different quarters and user agencies. Sd/= (Feroz Ahmed Khan ) Chairman/Chief Executive Councilor LAHDC, Kargil Statistical Handbook District Kargil 2018-19 THE ADMINISTRATION OF UNION TERRITORY OF LADAKH District Magistrate, (Deputy Commissioner/CEO) LAHDC Kargil Phone No: 01985-232216, Tele Fax: 232644 Message I am glad to know that the district Statistics and Evaluation Office Kargil is releasing its latest annual publication “Statistical Handbook” for the year 2018- 19. The present publication contains statistics related to infrastructure as well as Socio Economic development of Kargil District. -
Passupassu Passu
NWFP Wildlife Department Government of NWFP NA Forestry, Parks and Wildlife Department NA Administration PASSUPASSUPASSUPASSU MagnificentPASSU Glaciers & Mighty Peaks Rock flutes near Fatima Hil © all photographs Matthieu Paley p12 PASSU IS MAGNIFICENTLY SITUATED, IN A COUNTRY WHERE NATURE HAS DESIGNED EVERYTHING ON A NOBLE AND LAVISH SCALE. “Col. R. C. F. Schomberg, “Between the Oxus and the Indus” ” all maps by Mareile Paley. Created with the help of WWF GIS-Lab, ESRI and ERDAS imagine all maps by Mareile Paley. PASSU FACTS location Gojal, Upper Hunza, on the Karakoram Highway main settlements Passu, Janabad public transport any transport on Karakoram Highway going between Aliabad and Sost accommodation several small guesthouses in Passu, guesthouses and hotels in Janabad supplies best to buy all your trekking food in Sost, Aliabad or Gilgit population 98 households, 880 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 View of Passu from Avdegar INTRODUCTION INTRODUCTIONINTRODUCTIONINTRODUCTIONINTRODUCTION With the completion of the Karakoram Highway (KKH) in 1978, the previously inaccessible maze of high mountains, glaciers and hidden valleys which make up the Karakoram Range, suddenly opened its doors to the world. An area of unspoiled mountain beauty with rugged glaciers, unclimbed peaks and pristine wildlife, Gojal, the region north of Hunza, has since become a popular spot for ecotourism. The sun-drenched summits Passu village with its small rural Wakhi community lays in the heart of Gojal. Passu’s idyllic Despite its popularity as a opposite Passu are commonly trekking destination, Passu known as the Cathedral Peaks. -
LONG and MEDIUM RANGE TARBELA INFLOW FORECAST METHODOLOGY Mr
Pakistan Journal of Meteorology Vol. 3, Issue 6, December 2006 LONG AND MEDIUM RANGE TARBELA INFLOW FORECAST METHODOLOGY Mr. Abdul Majid∗, Mr. Tajdar Hussain*, Mr. Rizwan Malik* Abstract: The Indus has been truly called a life line of Pakistan. It is the river through which most of the water flows down to the plain of Punjab and Sindh. Most of the flows north of Tarbela are caused by the snowmelt over the elevated catchments of the northern areas. Further more melt water yield of upper Indus basin indicates large scale variation. For example the range of variation of the discharge at Bisham Qila for the month of June during the period 1965-1988 range from 1310 cusecs to about 12800 cusecs.The above two facts alone necessitate a system to predict the variability of flows of such a large extent. A methodology through which the seasonal and the monthly inflows at Tarbela could be forecast, shall constitute an important technical development since the judicial use of the available water for power and irrigation largely depend upon the advance knowledge of the incoming inflows. WAPDA attempted to tackle the problem through the technical assistance from Canada as a cooperative research program with “Wilfred Laurier University (WLU)” Waterlov and International Development research centre (IDRC). A project called Snow and Ice hydrography project came into existence for this proposal. The project is in existence since early eighties. The approach adopted in computing the seasonal and ten daily inflow is essentially based upon the use of a snow melt model called the university of British Columbia (UBS) model. -
B.A. 6Th Semester Unit IV Geography of Jammu and Kashmir
B.A. 6th Semester Unit IV Geography of Jammu and Kashmir Introduction The state of Jammu and Kashmir constitutes northern most extremity of India and is situated between 32o 17′ to 36o 58′ north latitude and 37o 26′ to 80o 30′ east longitude. It falls in the great northwestern complex of the Himalayan Ranges with marked relief variation, snow- capped summits, antecedent drainage, complex geological structure and rich temperate flora and fauna. The state is 640 km in length from north to south and 480 km from east to west. It consists of the territories of Jammu, Kashmir, Ladakh and Gilgit and is divided among three Asian sovereign states of India, Pakistan and China. The total area of the State is 222,236 km2 comprising 6.93 per cent of the total area of the Indian territory including 78,114 km2 under the occupation of Pakistan and 42,685 km2 under China. The cultural landscape of the state represents a zone of convergence and diffusion of mainly three religio-cultural realms namely Muslims, Hindus and Buddhists. The population of Hindus is predominant in Jammu division, Muslims are in majority in Kashmir division while Buddhists are in majority in Ladakh division. Jammu is the winter capital while Srinagar is the summer capital of the state for a period of six months each. The state constitutes 6.76 percent share of India's total geographical area and 41.83 per cent share of Indian Himalayan Region (Nandy, et al. 2001). It ranks 6th in area and 17th in population among states and union territories of India while it is the most populated state of Indian Himalayan Region constituting 25.33 per cent of its total population. -
Glacier Characteristics and Retreat Between 1991 and 2014 in the Ladakh Range, Jammu and Kashmir
February 24, 2017 Remote Sensing Letters chudley-ladakh-manuscript To appear in Remote Sensing Letters Vol. 00, No. 00, Month 20XX, 1{17 Glacier characteristics and retreat between 1991 and 2014 in the Ladakh Range, Jammu and Kashmir THOMAS R. CHUDLEYy∗, EVAN S. MILESy and IAN C. WILLISy yScott Polar Research Institute, University of Cambridge, Cambridge, UK (Received 29th November 2016) The Ladakh Range is a liminal zone of meteorological conditions and glacier changes. It lies between the monsoon-forced glacier retreat of the Himalaya and Zanskar ranges to the south and the anomalous stability observed in the Karakoram to the north, driven by mid-latitude westerlies. Given the climatic context of the Ladakh Range, the glaciers in the range might be expected to display intermediate behaviour between these two zones. However, no glacier change data have been compiled for the Ladakh Range itself. Here, we examine 864 glaciers in the central section of the Ladakh range, covering a number of smaller glaciers not included in alternative glacier inventories. Glaciers in the range are small (median 0.25 km2; maximum 6.58 km2) and largely distributed between 5000-6000 m above sea level (a.s.l.). 657 glaciers are available for multitemporal analysis between 1991 to 2014 using data from Landsat multispectral sensors. We find glaciers to have retreated -12.8% between 1991{2014. Glacier changes are consistent with observations in the Western Himalaya (to the south) and in sharp contrast with the Karakoram (to the north) in spite of its proximity to the latter. We suggest this sharp transition must be explained at least in part by non-climatic mechanisms (such as debris covering or hypsometry), or that the climatic factors responsible for the Karakoram behaviour are extremely localised.