India: Ladakh, Strategic Scenery-I
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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. -
OU1901 092-099 Feature Cycling Ladakh
Cycling Ladakh Catching breath on the road to Rangdum monastery PICTURE CREDIT: Stanzin Jigmet/Pixel Challenger Breaking the There's much more to Kate Leeming's pre- Antarctic expeditions than preparation. Her journey in the Indian Himalaya was equally about changing peoples' lives. WORDS Kate Leeming 92 93 Cycling Ladakh A spectacular stream that eventually flows into the Suru River, on the 4,000m plains near Rangdum nergy was draining from my legs. My heart pounded hard and fast, trying to replenish my oxygen deficit. I gulped as much of the rarified air as I could, without great success; at 4,100m, the atmospheric oxygen is at just 11.5 per cent, compared to 20.9 per cent at sea level. As I continued to ascend towards the snow-capped peaks around Sirsir La pass, the temperature plummeted and my body, drenched in a lather of perspiration, Estarted to get cold, further sapping my energy stores. Sirsir La, at 4,828m, is a few metres higher than Europe’s Mont Blanc, and I was just over half way up the continuous 1,670m ascent to get there. This physiological response may have been a reality check, but it was no surprise. The ride to the remote village of Photoksar on the third day of my altitude cycling expedition in the Indian Himalaya had always loomed as an enormous challenge, and I was not yet fully acclimatised. I drew on experience to pace myself: keeping the pedals spinning in a low gear, trying to relax as much as possible and avoiding unnecessary exertion. -
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. -
Delhi at Airport Nothing 2 20.08. Flight Delhi
day date activity next night sevice by Overland Escape 1 19.08. flight Zürich - Delhi at airport nothing flight Delhi Jet Air rest day 2 20.08. Lotus Hotel, Leh hotel flight Delhi - Leh, transfer to Lotus Hotel, half board 3 21.08. acclimatisation at Leh and surroundings, no special program hotel Lotus hotel half board Jeep tour with tents, picknick at daytime, cooking in the evening, Leh - Phyang - Taroo valley - Indus/Zanskar junction - Basgo 4 22.08. valley tent jeep, driver, cook, tent, kitchen, full board 5 23.08. Basgo valley - Alchi visit - Likir tent jeep, driver, cook, tent, kitchen, full board Exploring surroundings of Likir, walk to Saspochey 6 24.08. jeep goes on jeep road to Saspochey tent jeep, driver, cook, tent, kitchen, full board Walk to Hemis Shukpachan, 7 25.08. jeep goes on jeep road to Hemis Shukpachan tent jeep, driver, cook, tent, kitchen, full board walk to Ang, Tingmosgang Gompa jeep goes back to Indus valley and enters valley to Tingmosgang 8 26.08. gompa (Nurla) tent jeep, driver, cook, tent, kitchen, full board Jeep drive to Lamayuru gompa, visit jeep drive to Futu La until crossing with Kanji gorge meeting with horseman and horses / donkeys jeep, driver, cook, tent, kitchen, new: horses, horseman, kitchen 9 27.08. they bring fresh food, jeep goes back to Leh tent helper, full bord 10 28.08. Start trek Kanji La - Ringdom gompa, until Kanji village tent cook, horseman, kitchen helper, horses, tents, full board 11 29.08. Kanji villag - Ampultun - camp 2 tent cook, horseman, kitchen helper, horses, tents, full board 12 30.08. -
Demilitarization of the Siachen Conflict Zone: Concepts for Implementation and Monitoring
SANDIA REPORT SAND2007-5670 Unlimited Release Printed September 2007 Demilitarization of the Siachen Conflict Zone: Concepts for Implementation and Monitoring Brigadier (ret.) Asad Hakeem Pakistan Army Brigadier (ret.) Gurmeet Kanwal Indian Army with Michael Vannoni and Gaurav Rajen Sandia National Laboratories Prepared by Sandia National Laboratories Albuquerque, New Mexico 87185 and Livermore, California 94550 Sandia is a multiprogram laboratory operated by Sandia Corporation, a Lockheed Martin Company, for the United States Department of Energy’s National Nuclear Security Administration under Contract DE-AC04-94AL85000. Approved for public release; further dissemination unlimited. Issued by Sandia National Laboratories, operated for the United States Department of Energy by Sandia Corporation. NOTICE: This report was prepared as an account of work sponsored by an agency of the United States Government. Neither the United States Government, nor any agency thereof, nor any of their employees, nor any of their contractors, subcontractors, or their employees, make any warranty, express or implied, or assume any legal liability or responsibility for the accuracy, completeness, or usefulness of any information, apparatus, product, or process disclosed, or represent that its use would not infringe privately owned rights. Reference herein to any specific commercial product, process, or service by trade name, trademark, manufacturer, or otherwise, does not necessarily constitute or imply its endorsement, recommendation, or favoring by the United States Government, any agency thereof, or any of their contractors or subcontractors. The views and opinions expressed herein do not necessarily state or reflect those of the United States Government, any agency thereof, or any of their contractors. Printed in the United States of America. -
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. -
6 Nights & 7 Days Leh – Nubra Valley (Turtuk Village)
Jashn E Navroz | Turtuk, Ladakh | Dates 25March-31March’18 |6 Nights & 7 Days Destinations Leh Covered – Nubra : Leh Valley – Nubra (Turtuk Valley V illage)(Turtuk– Village Pangong ) – Pangong Lake – Leh Lake – Leh Trip starts from : Leh airport Trip starts at: LehTrip airport ends at |: LehTrip airport ends at: Leh airport “As winter gives way to spring, as darkness gives way to light, and as dormant plants burst into blossom, Nowruz is a time of renewal, hope and joy”. Come and experience this festive spirit in lesser explored gem called Turtuk. The visual delights would be aptly complemented by some firsthand experiences of the local lifestyle and traditions like a Traditional Balti meal combined with Polo match. During the festival one get to see the flamboyant and vibrant tribe from Balti region, all dressed in their traditional best. Day 01| Arrive Leh (3505 M/ 11500 ft.) Board a morning flight and reach Leh airport. Our representative will receive you at the terminal and you then drive for about 20 minutes to reach Leh town. Check into your room. It is critical for proper acclimatization that people flying in to Leh don’t indulge in much physical activity for at least the first 24hrs. So the rest of the day is reserved for relaxation and a short acclimatization walk in the vicinity. Meals Included: L & D Day 02| In Leh Post breakfast, visit Shey Monastery & Palace and then the famous Thiksey Monastery. Drive back and before Leh take a detour over the Indus to reach Stok Village. Enjoy a traditional Ladakhi meal in a village home later see Stok Palace & Museum. -
Igophey Canal, Leh Ladakh ( Joint Vernture of Irrigation Division Igophey and CAD Leh) (1979 – 2011)
Government of Jammu & Kashmir Evaluation Report On Igophey Canal, Leh Ladakh ( Joint Vernture of Irrigation Division Igophey and CAD Leh) (1979 – 2011) Irrigated Land in sample farms before and after Irrigated Land in sample villages before and after the commissioing of Igophey Canal Project the commissioing of Igophey Canal Project Before commissioning of project Before commissioning of project After commissioning of project After commissioning of project 576.00 600.00 423.00 6000.00 5061.12 400.00 4000.00 3178.12 171.00 161.00 141.00 80.00 128.00 123.00 2090.00 200.00 116.00 1648.12 1648.12 79.00 1530.00 2000.00 1073.00 250.00 0.00 0.00 - Area inHectarres Area inHectarres 0.00 SKUAST Matho Fodder Equine Total Dev. farm sample Farm Farms Stakna Sample Villages Sample Farms Directorate of Economics and Statistics, J&K Planning and Development Department Contents S.no Description of the Chapter Page Nos I Introduction 1-4 II Scheme & Its Progress 5-13 III Field Findings 14-35 IV Summary of Main Findings 36-39 Difficulties/Bottlenecks faced 40 Suggestions 41_____ Highlights of Evaluation Study on Igophey Canal, Leh. 1. The Igophey Irrigation project situated in Leh District of J & K state was started in the year 1979. The objective of the scheme was to facilitate irrigation in the Command Area of the Canal and bring more un-irrigated land under irrigation for raising the productivity and production of the area. The ultimate aim was to decrease excessive dependence of the area on import of foodgrains from other parts of the country. -
`15,999/-(Per Person)
BikingLEH Adventure 06 DAYS OF THRILL STARTS AT `15,999/-(PER PERSON) Leh - Khardungla Pass - Nubra Valley - Turtuk - Pangong Tso - Tangste [email protected] +91 9974220111 +91 7283860777 1 ABOUT THE PLACES Leh, a high-desert city in the Himalayas, is the capital of the Leh region in northern India’s Jammu and Kashmir state. Originally a stop for trading caravans, Leh is now known for its Buddhist sites and nearby trekking areas. Massive 17th-century Leh Palace, modeled on the Dalai Lama’s former home (Tibet’s Potala Palace), overlooks the old town’s bazaar and mazelike lanes. Khardung La is a mountain pass in the Leh district of the Indian union territory of Ladakh. The local pronunciation is "Khardong La" or "Khardzong La" but, as with most names in Ladakh, the romanised spelling varies. The pass on the Ladakh Range is north of Leh and is the gateway to the Shyok and Nubra valleys. Nubra is a subdivision and a tehsil in Ladakh, part of Indian-administered Kashmir. Its inhabited areas form a tri-armed valley cut by the Nubra and Shyok rivers. Its Tibetan name Ldumra means "the valley of flowers". Diskit, the headquarters of Nubra, is about 150 km north from Leh, the capital of Ladakh. Turtuk is one of the northernmost villages in India and is situated in the Leh district of Ladakh in the Nubra Tehsil. It is 205 km from Leh, the district headquarters, and is on the banks of the Shyok River. Pangong Tso or Pangong Lake is an endorheic lake in the Himalayas situated at a height of about 4,350 m. -
A Sub Range of the Hindu Kush Himalayan Range. Ladakh Range Is a Mountain Range in Central Ladakh
A sub range of the Hindu Kush Himalayan range. Ladakh Range is a mountain range in central Ladakh. Karakoram range span its border between Pakistan, India & china. It lies between the Indus and Shyok river valleys, stretching to 230 miles. Karakoram serve as a watershed for the basin of the Indus and Yarkand river. Ladakh range is regarded as southern extension of the Karakoram range. K2, the second highest peak in the world is located here. Extension of the Ladakh range into china is known as Kailash range. Glacier like Siachen, and Biafo are found in this range. Ladakh Range Karakoram Range Mountain Ranges in India Pir panjal Range Zaskar Range Group of mountains in the Himalayas. Group of mountains in the Lesser Himalayan region, near They extended southeastward for some 400 mile from Karcha river the bank of Sutlej river. to the upper Karnali river. Separates Jammu hills to the south from the vale of Kashimr Lies here coldest place in India, Dras. (the gateway to Ladakh) beyond which lie the Great Himalayas. Kamet Peak is the highest point. Highest points Indrasan. Famous passes- Shipki, Lipu Lekh and Mana pass. Famous passes- Pir Panjal, Banihal pass, Rohtang pass. Part of lesser Himalayan chain of Mountains. Mountain range of the outer Himalayas that stretches from the Indus river about It rise from the Indian plains to the north of Kangra and Mandi. 2400 km eastwards close to the Brahmaputra river. The highest peak in this range is the Hanuman Tibba or 'White Mountain' A gap of about 90 km between the Teesta and Raidak river in Assam known approaches from Beas kund.