Climbing in the Indian Himalayan Region, Some More Challenging Than the Everest, and Many of Them Above 7,000M
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The Surface Energy Balance in a Cold-Arid Permafrost Environment
https://doi.org/10.5194/tc-2019-286 Preprint. Discussion started: 9 March 2020 c Author(s) 2020. CC BY 4.0 License. The surface energy balance in a cold-arid permafrost environment, Ladakh Himalaya, India John Mohd Wani1, Renoj J. Thayyen2*, Chandra Shekhar Prasad Ojha1, and Stephan Gruber3 1Department of Civil Engineering, Indian Institute of Technology (IIT) Roorkee, India, 2Water Resources System Division, National Institute of Hydrology, Roorkee, India ([email protected]; [email protected]), 3Department of Geography & Environmental Studies, Carleton University, Ottawa, Canada Abstract: Cryosphere of the cold-arid trans-Himalayan region is unique with its significant permafrost cover. While the information on the permafrost characteristics and its extent started emerging, the governing energy regimes of this cryosphere region is of particular interest. This paper present the results of Surface Energy Balance (SEB) studies carried out in the upper 5 Ganglass catchment in the Ladakh region of India, which feed directly to the River Indus. The point SEB is estimated using the one-dimensional mode of GEOtop model from 1 September 2015 to 31 August 2017 at 4727 m a.s.l elevation. The model is evaluated using field monitored radiation components, snow depth variations and one-year near-surface ground temperatures and showed good agreement with the respective simulated values. The study site has an air 10 temperature range of – 23.7 to 18.1 °C with a mean annual average temperature (MAAT) of - 2.5 and ground surface temperature range of -9.8 to 19.1 °C. For the study period, the surface energy balance characteristics of the cold-arid site show that the net radiation was the major component with mean value of 28.9 W m-2, followed by sensible heat flux (13.5 W m-2) and latent heat flux (12.8 W m-2), and the ground heat flux was equal to 0.4 W m-2. -
Status of Insectivorous Plants in Northeast India
Technical Refereed Contribution Status of insectivorous plants in northeast India Praveen Kumar Verma • Shifting Cultivation Division • Rain Forest Research Institute • Sotai Ali • Deovan • Post Box # 136 • Jorhat 785 001 (Assam) • India • [email protected] Jan Schlauer • Zwischenstr. 11 • 60594 Frankfurt/Main • Germany • [email protected] Krishna Kumar Rawat • CSIR-National Botanical Research Institute • Rana Pratap Marg • Lucknow -226 001 (U.P) • India Krishna Giri • Shifting Cultivation Division • Rain Forest Research Institute • Sotai Ali • Deovan • Post Box #136 • Jorhat 785 001 (Assam) • India Keywords: Biogeography, India, diversity, Red List data. Introduction There are approximately 700 identified species of carnivorous plants placed in 15 genera of nine families of dicotyledonous plants (Albert et al. 1992; Ellison & Gotellli 2001; Fleischmann 2012; Rice 2006) (Table 1). In India, a total of five genera of carnivorous plants are reported with 44 species; viz. Utricularia (38 species), Drosera (3), Nepenthes (1), Pinguicula (1), and Aldrovanda (1) (Santapau & Henry 1976; Anonymous 1988; Singh & Sanjappa 2011; Zaman et al. 2011; Kamble et al. 2012). Inter- estingly, northeastern India is the home of all five insectivorous genera, namely Nepenthes (com- monly known as tropical pitcher plant), Drosera (sundew), Utricularia (bladderwort), Aldrovanda (waterwheel plant), and Pinguicula (butterwort) with a total of 21 species. The area also hosts the “ancestral false carnivorous” plant Plumbago zelayanica, often known as murderous plant. Climate Lowland to mid-altitude areas are characterized by subtropical climate (Table 2) with maximum temperatures and maximum precipitation (monsoon) in summer, i.e., May to September (in some places the highest temperatures are reached already in April), and average temperatures usually not dropping below 0°C in winter. -
Arunachal Pradesh Yatra by Sanjeev Nayyar July 2014 I Spent Nearly
Arunachal Pradesh Yatra By Sanjeev Nayyar July 2014 I spent nearly three weeks in Arunachal Pradesh, drove over 3,000 kms starting from Deomali in the east to Tawang in the west the last stop being Gauhati. It was one of the most intense drives and yatras of my life. We covered touristy places, schools, war memorials and border visit. This piece gives you the route that I took, places to see along the way plus links of pictures uploaded on esamskriti. Photo captions have travel tips etc. Travel Route I took a Mumbai-Kolkatta-Dibrugarh flight. If you book tickets in advance then get a cheap fare. INDIGO was bang on time – reliable as always. From Dibrugarh took a Tata Sumo. It is about a 3-4 hour drive to Ramakrishna Mission School, Narrottamnagar in Deomali. From RKM it is about an 8 hour drive to Teju. Route was Deomali- Godumsa-Namsai-Chowkham-Wakro-Parasuram Kund-Tezu. We stopped by at Chowkham, Wakro and Parasramkund. Tezu to Roing - there was a bridge being built over river in September 2013 when we went. If completed Tezu to Roing is about 2-3 hours. We had to take a longer route, took app 4 hours. From Roing Mayurdia is a 2 hour drive, can do a day trip. From Roing takes about 2 hours to reach the banks of the Brahmaputra – crossing the river takes one hour but might need to wait longer depending on boat availability. After crossing the river it is a 1.5 to 2 hour drive to Dibrugarh. -
SURVEY in the NANDA DEVI DISTRICT. E. E. Shipton
SURVEY IN THE NANDA DEVI DISTRICT SURVEY IN THE NANDA DEVI DISTRICT BY E. E. SHIPTON Read before the Alpine Club, l\1arch g, 1937 OUNTAINEERS will have been interested to learn that the Survey of India is now engaged on a new !-inch map of the mountain regions of Kumaon and Garhwal. Previous surveys, as produced on the present !-inch sheets 53 N and 62 B, had been confined almost entirely to the popu lated and revenue-producing areas in or near to the great arterial valleys. Most of the glacier-cov~red country and the remoter valleys of these sheets are very sketchily drawn, in many places, indeed, so sketchily as to bear no resemblance whatever to the ground in question. Over much of the country, too, it has been found necessary to extend the primary triangulation. While engaged on this task in the Badrinath-Kedarnath range, Major Osmaston found that the whole trunk of the Gangotri Glacier was, in fact, several miles W. of the position allotted to it on the map. I hope that now at last we shall have a final solution to the topographical problems of this area. which have excited so much discussion as a result of the various expeditions which have recently brought back a lot of vague data about the range. The usual method employed for hill surveys in India is plane tabling by Indians, 'vho are each responsible for a section of the area. These men work with remarkable speed and neatness and, under the close supervision of their officers, they produce very good work. -
Conceptual Model for the Vulnerability Assessment of Springs in the Indian Himalayas
climate Article Conceptual Model for the Vulnerability Assessment of Springs in the Indian Himalayas Denzil Daniel 1 , Aavudai Anandhi 2 and Sumit Sen 1,3,* 1 Centre of Excellence in Disaster Mitigation and Management, Indian Institute of Technology Roorkee, Roorkee 247667, India; [email protected] 2 Biological Systems Engineering Program, College of Agriculture and Food Sciences, Florida A&M University, Tallahassee, FL 32307, USA; [email protected] 3 Department of Hydrology, Indian Institute of Technology Roorkee, Roorkee 247667, India * Correspondence: [email protected]; Tel.: +91-1332-284754 Abstract: The Indian Himalayan Region is home to nearly 50 million people, more than 50% of whom are dependent on springs for their sustenance. Sustainable management of the nearly 3 million springs in the region requires a framework to identify the springs most vulnerable to change agents which can be biophysical or socio-economic, internal or external. In this study, we conceptualize vulnerability in the Indian Himalayan springs. By way of a systematic review of the published literature and synthesis of research findings, a scheme of identifying and quantifying these change agents (stressors) is presented. The stressors are then causally linked to the characteristics of the springs using indicators, and the resulting impact and responses are discussed. These components, viz., stressors, state, impact, and response, and the linkages are used in the conceptual framework to assess the vulnerability of springs. A case study adopting the proposed conceptual model is discussed Citation: Daniel, D.; Anandhi, A.; for Mathamali spring in the Western Himalayas. The conceptual model encourages quantification Sen, S. -
Geological Society of America Bulletin
Downloaded from gsabulletin.gsapubs.org on July 5, 2010 Geological Society of America Bulletin Geologic correlation of the Himalayan orogen and Indian craton: Part 2. Structural geology, geochronology, and tectonic evolution of the Eastern Himalaya An Yin, C.S. Dubey, T.K. Kelty, A.A.G. Webb, T.M. Harrison, C.Y. Chou and Julien Célérier Geological Society of America Bulletin 2010;122;360-395 doi: 10.1130/B26461.1 Email alerting services click www.gsapubs.org/cgi/alerts to receive free e-mail alerts when new articles cite this article Subscribe click www.gsapubs.org/subscriptions/ to subscribe to Geological Society of America Bulletin Permission request click http://www.geosociety.org/pubs/copyrt.htm#gsa to contact GSA Copyright not claimed on content prepared wholly by U.S. government employees within scope of their employment. Individual scientists are hereby granted permission, without fees or further requests to GSA, to use a single figure, a single table, and/or a brief paragraph of text in subsequent works and to make unlimited copies of items in GSA's journals for noncommercial use in classrooms to further education and science. This file may not be posted to any Web site, but authors may post the abstracts only of their articles on their own or their organization's Web site providing the posting includes a reference to the article's full citation. GSA provides this and other forums for the presentation of diverse opinions and positions by scientists worldwide, regardless of their race, citizenship, gender, religion, or political viewpoint. Opinions presented in this publication do not reflect official positions of the Society. -
Volume 30 # October 2014
Summit ridge of Rassa Kangri (6250m) THE HIMALAYAN CLUB l E-LETTER l Volume 30 October 2014 CONTENTS Climbs and Explorations Climbs and Exploration in Rassa Glacier ................................................. 2 Nanda Devi East (7434m) Expedition 204 .............................................. 7 First Ascent of P6070 (L5) ....................................................................... 9 Avalanche on Shisha Pangma .................................................................. 9 First Ascent of Gashebrum V (747m) .....................................................0 First Ascent of Payu Peak (6600m) South Pillar ......................................2 Russians Climb Unclimbed 1900m Face of Thamserku .........................3 The Himalayan Club - Pune Section The story of the club’s youngest and a vibrant section. ..........................4 The Himalayan Club – Kolkata Section Commemoration of Birth Centenary of Tenzing Norgay .........................8 The Himalayan Club – Mumbai Section Journey through my Lense - Photo Exhibition by Mr. Deepak Bhimani ................................................9 News & Views The Himalayan Club Hon. Local Secretary in Kathmandu Ms. Elizabeth Hawley has a peak named after her .................................9 Climbing Fees Reduced in India ............................................................. 22 04 New Peaks open for Mountaineering in Nepal ................................ 23 Online Show on Yeti ............................................................................... -
Catalogue 48: June 2013
Top of the World Books Catalogue 48: June 2013 Mountaineering Fiction. The story of the struggles of a Swiss guide in the French Alps. Neate X134. Pete Schoening Collection – Part 1 Habeler, Peter. The Lonely Victory: Mount Everest ‘78. 1979 Simon & We are most pleased to offer a number of items from the collection of American Schuster, NY, 1st, 8vo, pp.224, 23 color & 50 bw photos, map, white/blue mountaineer Pete Schoening (1927-2004). Pete is best remembered in boards; bookplate Ex Libris Pete Schoening & his name in pencil, dj w/ edge mountaineering circles for performing ‘The Belay’ during the dramatic descent wear, vg-, cloth vg+. #9709, $25.- of K2 by the Third American Karakoram Expedition in 1953. Pete’s heroics The first oxygenless ascent of Everest in 1978 with Messner. This is the US saved six men. However, Pete had many other mountain adventures, before and edition of ‘Everest: Impossible Victory’. Neate H01, SB H01, Yak H06. after K2, including: numerous climbs with Fred Beckey (1948-49), Mount Herrligkoffer, Karl. Nanga Parbat: The Killer Mountain. 1954 Knopf, NY, Saugstad (1st ascent, 1951), Mount Augusta (1st ascent) and King Peak (2nd & 1st, 8vo, pp.xx, 263, viii, 56 bw photos, 6 maps, appendices, blue cloth; book- 3rd ascents, 1952), Gasherburm I/Hidden Peak (1st ascent, 1958), McKinley plate Ex Libris Pete Schoening, dj spine faded, edge wear, vg, cloth bookplate, (1960), Mount Vinson (1st ascent, 1966), Pamirs (1974), Aconcagua (1995), vg. #9744, $35.- Kilimanjaro (1995), Everest (1996), not to mention countless climbs in the Summarizes the early attempts on Nanga Parbat from Mummery in 1895 and Pacific Northwest. -
(A) Revised Fee Structure Is Applicable for the Climbing Season 2020 Only
ANNEXURE REDUCTION/DISCOUNTS ON PEAK FEE TO OTHERS FOR LESS CLIMBED PEAKS Height of Peak Existing Peak Fee ProposeD peak Fee for the Climbing Season 2020 Below 6500 M (1) US$ 500 for party of two 1) US$ 250 for party of two members. members. (List of peaks attacheD AppenDix “A”) (2) For additional members upto (2) For additional members twelve, US$ 225 each. upto twelve, US$ 110 each. 6501 M to 7000 M (1) US$ 700 for party of two (1) US$ 350 for party of two members. members. (List of Peaks attacheD AppenDix “B”) (2) For additional members upto (2) For additional members upto twelve, US$ 325 each. twelve, US$ 165 each. 7001 M anD above (1) US$ 1000 for party of two (1) US$ 500 for party of two members. members. (List of Peaks attacheD AppenDix “C”) (2) For additional members upto (2) For additional members upto twelve, US$ 450 each. twelve, US$ 225 each. Trekking Peaks (List of (1) US$ 100 for party of two (1) US$ 100 for party of two peak AppenDix “D”) members. members. (2) For additional members upto (2) For additional members upto twelve, US$ 50 each twelve, US$ 50 each Note : (a) Revised fee structure is applicable for the climbing season 2020 only. (b) There is no change in other terms and conditions applicable. Appendix “A” PEAKS BELOW 6500 M IN OPEN AREA J&K S.NO. Name of peak Height Longitude Latitude Remarks 1. Bobang 5971 M 76° 08’ 33° 25’ Leh-Harpass-Kijai Nala- Nagdal Lake-C-I-CII Summit Attempt 2. -
Regional, Seasonal, and Diurnal Variations of Extreme Convection in the South Asian Region
15 JANUARY 2010 R O M A T S C H K E E T A L . 419 Regional, Seasonal, and Diurnal Variations of Extreme Convection in the South Asian Region ULRIKE ROMATSCHKE University of Washington, Seattle, Washington, and University of Vienna, Vienna, Austria SOCORRO MEDINA AND ROBERT A. HOUZE JR. University of Washington, Seattle, Washington (Manuscript received 17 March 2009, in final form 2 July 2009) ABSTRACT Temporal and spatial variations of convection in South Asia are analyzed using eight years of Tropical Rainfall Measuring Mission (TRMM) Precipitation Radar (PR) data and NCEP reanalysis fields. To identify the most extreme convective features, three types of radar echo structures are defined: deep convective cores (contiguous 3D convective echo $40 dBZ extending $10 km in height) represent the most vertically pen- etrative convection, wide convective cores (contiguous convective $40 dBZ echo over a horizontal area $1000 km2) indicate wide regions of intense multicellular convection, and broad stratiform regions (strati- form echo contiguous over an area $50 000 km2) mark the mesoscale convective systems that have de- veloped the most robust stratiform regions. The preferred locations of deep convective cores change markedly from India’s east coast in the pre- monsoon to the western Himalayan foothills in the monsoon. They form preferentially in the evening and over land as near-surface moist flow is capped by dry air aloft. Continental wide convective cores show a similar behavior with an additional nocturnal peak during the monsoon along the Himalayan foothills that is associated with convergence of downslope flow from the Himalayas with moist monsoonal winds at the foothills. -
Volume 27 # June 2013
THE HIMALAYAN CLUB l E-LETTER Volume 27 l June 2013 Contents Annual Seminar February 2013 ........................................ 2 First Jagdish Nanavati Awards ......................................... 7 Banff Film Festival ................................................................. 10 Remembrance George Lowe ....................................................................................... 11 Dick Isherwood .................................................................................... 3 Major Expeditions to the Indian Himalaya in 2012 ......... 14 Himalayan Club Committee for the Year 2013-14 ........... 28 Select Contents of The Himalayan Journal, Vol. 68 ....... 30 THE HIMALAYAN CLUB l E-LETTER The Himalayan Club Annual Seminar 2013 The Himalayan Club Annual Seminar, 03 was held on February 6 & 7. It was yet another exciting Annual Seminar held at the Air India Auditorium, Nariman Point Mumbai. The seminar was kicked off on 6 February 03 – with the Kaivan Mistry Memorial Lecture by Pat Morrow on his ‘Quest for the Seven and a Half Summits’. As another first the seminar was an Audio Visual Presentation without Pat! The bureaucratic tangles had sent Pat back from the immigration counter of New Delhi Immigration authorities for reasons best known to them ! The well documented AV presentation made Pat come alive in the auditorium ! Pat is a Canadian photographer and mountain climber who was the first person in the world to climb the highest peaks of seven Continents: McKinley in North America, Aconcagua in South America, Everest in Asia, Elbrus in Europe, Kilimanjaro in Africa, Vinson Massif in Antarctica, and Puncak Jaya in Indonesia. This hour- long presentation described how Pat found the resources to help him reach and climb these peaks. Through over an hour that went past like a flash he took the audience through these summits and how he climbed them in different parts of the world. -
List of Famous Cricketers of All Time
Follow Us FAMOUS SPORTS PERSONALITIES List of Famous Cricketers of All time “You can also try the quiz on Famous Sports Personalities here – Quiz Link” Name of the Cricketer Famous for/ Known as Sachin Tendulkar Holds most of the batting records Sunil Gavaskar The little master Rahul Dravid The Wall Sourav Ganguly The best Indian captain Virender Sehwag India's finest opener Anil Kumble India's highest wicket taker Kapil Dev India's best all-rounder Javagal Srinath India's leading pacer for a long time Harbhajan Singh Best Indian off-spinner Zaheer Khan India's best left-handed fast bowler Aggressive captain and an equally Mohammad Azharuddin good player VVS Laxman One of the most elegant batsman MS Dhoni The best finisher Mohinder Amarnath Scored first test century for India Bishan Singh Bedi An effective spinner of his era Navjot Singh Siddhu Explosive batsman of his era Virat Kohli Next legend in making Vinod Kambli Short but marvellous career Ajay Jadeja A fine middle order batsman • First player to take a 5-wicket haul and score a 50 in the World Yuvraj Cup matches. • First player to hit 6 sixes in a T20 World Cup www.recruitment.guru/general-knowledge/| 1 Follow Us FAMOUS SPORTS PERSONALITIES Known for his slower deliveries and Venkatesh Prasad was one of its first proponents in world cricket The fastest Indian bowler to the milestone of 100 wickets in 18 test Ashwin matches and the fastest in the world in over 80 years Only Indian batsman to have scored Gambhir more than 300 runs in four consecutive Test series He has a record of fastest 100 wickets Erapalli Prasanna in Tests by an Indian Bowler (in 20 Tests) at this time.