Russia and Central Asia 1995
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Post-Monsoon in the Nepal Himalaya. in the Post-Monsoon in The
Post-Monsoon in the Nepal Himalaya. In the post-monsoon in the Nepal Himalaya, the sum mer monsoon rains and snowfall continued throughout September and into early October, several weeks beyond the normal end of the rainy season, only to be followed by a few mid- October days of more heavy snowfall resulting from a cyclone nearby in India. Many teams on Cho Oyu, Ama Dablam, Baruntse and other mountains with very limited time at their dis posal had to retreat from what they considered unsafe avalanche conditions or simply from snow too deep to manage to get through. There was very little success on Nepal’s eight 8000ers. Even on Cho Oyu, where success rates are often high, 21 expeditions did some climbing but just nine of them sent anyone to the top and all followed the normal route on the northwest side. The other 12 teams—includ ing cautiously-led commercial ones—withdrew well below the summit because of dangerous snow conditions. And those who were successful were able to reach the summit only from September 26-October 1 ; before and after those dates, snow conditions were very bad. One Japanese mountaineer, Toshiyuki Kitamura, tried to solo Cho Oyu’s seldom-climbed southwest face but had to abandon his attempt at 7400 meters in soft snow under a hot sun that defeated him. He moved over to the standard route and followed teammates to the top five days after their ascent. No one even attempted Annapurna I. Only one team out of seven (a predominantly American group that included Ginette Harrison; see below) had any summiters on Dhaulagiri I. -
Scaling the World's Most Challenging Summits Is Dangerous to Some. To
SCALING THE WORLD’S MOST CHALLENGING SUMMITS IS DANGEROUS TO SOME. TO DAVE HAHN, IT’S JUST A MATTER OF WALKING UPHILL A LITTLE LONGER THAN USUAL. KING SHEER FEAR OF THE HILLBY MICHAEL HAEDERLE photo: matthew turley matthew photo: 74 discovery channel magazine.com september 2009 75 WAS A LONG, COLD NIGHT IN After this first and most harrow- ROUTE TO THE TOP MAY 1994. CROUCHED ALONE ing success, Hahn went on to climb Hahn grew up in Kingston, New York, IIN A SNOWTSTORM 8,500 Everest a further ten times, more where his father, a former climber in than any other non-Sherpa, estab- Yosemite National Park, took him METRES UP ON THE NORTHEAST lishing himself as one of the world’s camping in the nearby Catskill and RIDGE OF MOUNT EVEREST leading high-altitude climbers. The Adirondack Mountains. As a teenag- lanky 47-year-old has also conquered er he visited his mother’s hometown – without oXYgen – DAVE the 4,897-metre Vinson Massif, the of Albuquerque, New Mexico, and HAHN HUNG ON FOR FIRST highest peak in Antarctica, a record scaled the craggy 3,255-metre Sandia LIGHT, DESPERATELY WILLING 26 times. Add to that 18 ascents of Crest. He returned to New Mexico af- Mount McKinley (also known as De- ter college to work as a ski instructor, HIMSELF TO STAY AWAKE AFTER nali) in Alaska and more than 250 but had an epiphany in 1985 when he 48 HOURS OF CONTINUOUS scalings of Mount Rainier in the US enrolled in a mountaineering course state of Washington and you have run by the Mount Rainier guide ser- CLIMBING. -
Korean Direct
AAC Publications Korean Direct The First Ascent Of Gasherbrum V Insignificant against the blinding white backdrop of Gasherbrum V’s south face, we stood like silhouettes atop a moraine, the wall before us in full view. The complex glacier leading up to the face reminded me of scaly dragon’s tail. We had spotted a snaking line that would lead us to the jagged bergschrund at the foot of the wall. Once on the face, we would have to keep left to avoid a menacing serac, then move right in the upper mixed section before finishing with a direct line to the top. Seong Nak-jong and I had never really considered a route on the south side of unclimbed Gasherbrum V until we were denied passage up the northeast face. We had started our first attempt on the 7,147- meter peak from Camp 1 on the South Gasherbrum Glacier, along the normal routes to Gasherbrums I and II. We trudged through thigh-deep snow to reach the northeast face, which was covered in loose ice and snow, and was nearly impossible to protect. Falling ice and spindrift poured down from above. We finally had no choice but to evacuate from our high point of 6,400 meters. This unsuccessful attempt quashed our desire to climb. As the leader of our small team, the quandaries of a second attempt weighed heavily on my mind. Not only were we physically weakened and our confidence shot, it was already mid-July and more snow was laying siege to the camps. We had been away from home for more than a month. -
Climbs and Expeditions, 1988
Climbs and Expeditions, 1988 The Editorial Board expresses its deep gratitude to the many people who have done so much to make this section possible. We cannot list them all here, but we should like to give particular thanks to the following: Kamal K. Guha, Harish Kapadia, Soli S. Mehta, H.C. Sarin, P.C. Katoch, Zafarullah Siddiqui, Josef Nyka, Tsunemichi Ikeda, Trevor Braham, Renato More, Mirella Tenderini. Cesar Morales Arnao, Vojslav Arko, Franci Savenc, Paul Nunn, Do@ Rotovnik, Jose Manuel Anglada, Jordi Pons, Josep Paytubi, Elmar Landes, Robert Renzler, Sadao Tambe, Annie Bertholet, Fridebert Widder, Silvia Metzeltin Buscaini. Luciano Ghigo, Zhou Zheng. Ying Dao Shui, Karchung Wangchuk, Lloyd Freese, Tom Elliot, Robert Seibert, and Colin Monteath. METERS TO FEET Unfortunately the American public seems still to be resisting the change from feet to meters. To assist readers from the more enlightened countries, where meters are universally used, we give the following conversion chart: meters feet meters feet meters feet meters feet 3300 10,827 4700 15,420 6100 20,013 7500 24,607 3400 11,155 4800 15,748 6200 20,342 7600 24,935 3500 11,483 4900 16,076 6300 20,670 7700 25,263 3600 11,811 5000 16,404 6400 20,998 7800 25,591 3700 12,139 5100 16,733 6500 21,326 7900 25,919 3800 12,467 5200 17.061 6600 21,654 8000 26,247 3900 12,795 5300 7,389 6700 21,982 8100 26,575 4000 13,124 5400 17,717 6800 22,3 10 8200 26,903 4100 13,452 5500 8,045 6900 22,638 8300 27,231 4200 13,780 5600 8,373 7000 22,966 8400 27,560 4300 14,108 5700 8,701 7100 23,294 8500 27,888 4400 14,436 5800 19,029 7200 23,622 8600 28,216 4500 14,764 5900 9,357 7300 23,951 8700 28,544 4600 15,092 6000 19,685 7400 24,279 8800 28,872 NOTE: All dates in this section refer to 1988 unless otherwise stated. -
Reconciling Drivers of Seasonal Terminus Advance and Retreat at 13
Journal of Geophysical Research: Earth Surface RESEARCH ARTICLE Reconciling Drivers of Seasonal Terminus Advance 10.1029/2018JF004628 and Retreat at 13 Central West Greenland Key Points: Tidewater Glaciers • We evaluate the correlation of seasonal terminus advance/retreat to M. J. Fried1,2 , G. A. Catania1,2 , L. A. Stearns3 , D. A. Sutherland4 , T. C. Bartholomaus5 , glacial runoff, ice mélange, and 6 6 ocean temperature E. Shroyer , and J. Nash • Runoff is the strongest predictor at 1 2 glaciers that calve via serac failures Institute for Geophysics, University of Texas at Austin, Austin, TX, USA, Department of Geosciences, University of Texas at where subglacial melt plumes locally Austin, Austin, TX, USA, 3Department of Geology, University of Kansas, Lawrence, KS, USA, 4Department of Earth Sciences, enhance retreat University of Oregon, Eugene, OR, USA, 5Department of Geology, University of Idaho, Moscow, ID, USA, 6College of Earth, • Glaciers with sporadic, Ocean, and Atmospheric Sciences, Oregon State University, Corvallis, OR, USA buoyancy-induced full-thickness calving and the largest ice fluxes are less sensitive to environmental forcings Abstract The majority of Greenland tidewater glaciers undergo a seasonal cycle in terminus position, characterized by wintertime advance and summertime retreat. Understanding mechanisms that control seasonal cycles can help elucidate how tidewater glaciers regulate dynamic ice loss on longer timescales. Supporting Information: • Supporting Information S1 However, controls on terminus position are numerous and complex. To address this, we compare time series • Movie S1 of satellite-derived terminus positions for tidewater glaciers in central west Greenland with observations of • Movie S2 environmental forcings, including runoff at the grounding line, mélange presence, and, where available, • Movie S3 ocean temperature in the proglacial fjord. -
Energy and Air Pollution
Copyright © 2006, United Nations Environment Programme ISBN: 92-807-2668-4 UNEP/GCSS.IX/INF/2 UNEP Job No. DEW/0773/NA Disclaimers The content and views expressed in this publication do not necessarily reflect the views or policies of the contributory organizations or the United Nations Environment Programme (UNEP) and neither do they imply any endorsement. The designations employed and the presentation of material in this publication do not imply the expression of any opinion whatsoever on the part of UNEP concerning the legal status of any country, territory or city or its authorities, or concerning the delimitation of its frontiers and boundaries. Mention of a commercial company or product in this publication does not imply the endorsement of UNEP. © Maps, photos and illustrations as specified. Reproduction This publication may be reproduced in whole or in part and in any form for educational or non-profit purposes without special permission from the copyright holder, provided acknowledgement of the source is made. UNEP would appreciate receiving a copy of any publication that uses this publication as a source. No use of this publication may be made for resale or any other commercial purpose whatsoever without prior permission in writing from UNEP. Applications for such permission, with a statement of purpose and intent of the reproduction, should be addressed to the Division of Communications and Public Information (DCPI), UNEP, P.O. Box 30552, Nairobi 00100, Kenya. The use of information from this publication concerning proprietary products for publicity or advertising is not permitted. Produced by Division of Early Warning and Assessment (DEWA) United Nations Environment Programme P.O. -
1976 Bicentennial Mckinley South Buttress Expedition
THE MOUNTAINEER • Cover:Mowich Glacier Art Wolfe The Mountaineer EDITORIAL COMMITTEE Verna Ness, Editor; Herb Belanger, Don Brooks, Garth Ferber. Trudi Ferber, Bill French, Jr., Christa Lewis, Mariann Schmitt, Paul Seeman, Loretta Slater, Roseanne Stukel, Mary Jane Ware. Writing, graphics and photographs should be submitted to the Annual Editor, The Mountaineer, at the address below, before January 15, 1978 for consideration. Photographs should be black and white prints, at least 5 x 7 inches, with caption and photo grapher's name on back. Manuscripts should be typed double· spaced, with at least 1 Y:z inch margins, and include writer's name, address and phone number. Graphics should have caption and artist's name on back. Manuscripts cannot be returned. Properly identified photographs and graphics will be returnedabout June. Copyright © 1977, The Mountaineers. Entered as second·class matter April8, 1922, at Post Office, Seattle, Washington, under the act of March 3, 1879. Published monthly, except July, when semi-monthly, by The Mountaineers, 719 Pike Street,Seattle, Washington 98101. Subscription price, monthly bulletin and annual, $6.00 per year. ISBN 0-916890-52-X 2 THE MOUNTAINEERS PURPOSES To explore and study the mountains, forests, and watercourses of the Northwest; To gather into permanentform the history and tra ditions of thisregion; To preserve by the encouragement of protective legislation or otherwise the natural beauty of NorthwestAmerica; To make expeditions into these regions in fulfill ment of the above purposes; To encourage a spirit of good fellowship among all loversof outdoor life. 0 � . �·' ' :···_I·:_ Red Heather ' J BJ. Packard 3 The Mountaineer At FerryBasin B. -
The American Alpine Club Guidebook to Membership Alpinist Magazine
THE AMERICAN ALPINE CLUB GUIDEBOOK TO MEMBERSHIP ALPINIST MAGAZINE ith each print edition of Alpinist, we aim to create a work of art, paying attention to every detail— from our extended photo captions to our carefully Wselected images and well-crafted stories. Inside our pages, we strive to offer our readers an experience like that of exploratory climbing, a realm of words and images where they can wander, discover surprising new viewpoints, and encounter moments of excitement, humor, awe and beauty. By publishing the work of climbers from a wide range of ages, technical abilities, nations and cultures—united by their passion for adventure and wild places—we hope to reflect and enhance the sense of community within the climbing life. Over time, back issues have become collectors’ items, serving as historical references and ongoing inspirations. Like our readers, we believe that great writing and art about climbing demand the same boldness, commitment and vision as the pursuit itself. JOIN US. Exclusive AAC Member Pricing 1 Year - $29.95 | 2 Years - $54.95 Alpinist.com/AAC ALPINIST IS A PROUD PARTNER OF THE AMERICAN ALPINE CLUB Stay Connected! @AlpinistMag @Alpinist @AlpinistMag ALP_2019_AAC Ad FIN.indd 1 6/26/19 4:14 PM WELCOME, ALL 5 You Belong Here ARTIST SPOTLIGHT 8 Brooklyn Bell on Art for the In-betweens MEMBERSHIP THROUGH THE LENS 10 Inspiration, Delivered Directly NAVAJO RISING 23 An Indigenous Emergence Story WHEN WOMEN LEAD 27 Single Pitch Instructors for the 21st Century GLACIAL VIEWS 29 A Climate Scientist Reflects & Other Research Stories CLIMBERS FOR CLIMATE 32 Taking a Stand on Climate Change, Together 1CLIMB, INFINITE POTENTIAL 34 Kevin Jorgeson Breaks Down Walls by Building Them ON PUSHING 37 24 Hours Into the Black, the AAC Grief Fund AN ODE TO MOBILITY 40 The Range of Motion Project Tackles Cotopaxi YOSEMITE'S CAMP 4 43 The Center of the Climbing Universe REWIND THE CLIMB 47 The Tragedy of the 1932 American K2 Expedition BETA 48 Everything a Club Member Needs to Know PARTING SHOT 72 Jeremiah Watt on Travel & Life a Greg Kerzhner climbing Mr. -
Glaciers of Grandes Jorasses: an Open-Air Laboratory for Glacier Monitoring Systems Development
EGU2020-9814 https://doi.org/10.5194/egusphere-egu2020-9814 EGU General Assembly 2020 © Author(s) 2021. This work is distributed under the Creative Commons Attribution 4.0 License. Glaciers of Grandes Jorasses: an open-air laboratory for glacier monitoring systems development Niccolò Dematteis1, Daniele Giordan1, and Fabrizio Troilo2 1Research Institute for Geo-Hydrological Protection, National Reasearch Council of Italy, Torino, Italy ([email protected]) 2Safe Mountain Foundation, Courmayeur, Italy Glaciological phenomena can have a strong impact on human activities in terms of hazards and freshwater supply. Therefore, a scientific observation is fundamental to investigate their current state and recent evolution. To this aim, experimenting innovative scientific survey methodologies and equipment is of primary importance. Strong efforts in this field have been spent in the glacial complex of the Grandes Jorasses massif (Mont Blanc area), where several ice break-offs glacial outburst triggered from the Planpincieux Glacier snout and the Whymper Serac and threatened the underling Planpincieux valley in the past. From 2009, the glacial complex has become an open filed laboratory where a wide set of close-range remote sensing survey systems have been developed and applied to investigate the glacial state and dynamics. Two continuous monoscopic time-lapse cameras observe the Planpincieux Glacier since 2013. Digital image correlation is applied to the photographs to measure the surface kinematics at different level of detail. During the monitoring, image analysis techniques allowed at classifying the instability processes of the terminus and at estimating the volume of the break-off events. Such investigation revealed the presence of possible break-off precursors and a monotonic relationship between glacier velocity and break-off volume, which might help for risk evaluation. -
Genre Bending Narrative, VALHALLA Tells the Tale of One Man’S Search for Satisfaction, Understanding, and Love in Some of the Deepest Snows on Earth
62 Years The last time Ken Brower traveled down the Yampa River in Northwest Colorado was with his father, David Brower, in 1952. This was the year his father became the first executive director of the Sierra Club and joined the fight against a pair of proposed dams on the Green River in Northwest Colorado. The dams would have flooded the canyons of the Green and its tributary, Yampa, inundating the heart of Dinosaur National Monument. With a conservation campaign that included a book, magazine articles, a film, a traveling slideshow, grassroots organizing, river trips and lobbying, David Brower and the Sierra Club ultimately won the fight ushering in a period many consider the dawn of modern environmentalism. 62 years later, Ken revisited the Yampa & Green Rivers to reflect on his father's work, their 1952 river trip, and how we will confront the looming water crisis in the American West. 9 Minutes. Filmmaker: Logan Bockrath 2010 Brower Youth Awards Six beautiful films highlight the activism of The Earth Island Institute’s 2011 Brower Youth Award winners, today’s most visionary and strategic young environmentalists. Meet Girl Scouts Rhiannon Tomtishen and Madison Vorva, 15 and 16, who are winning their fight to green Girl Scout cookies; Victor Davila, 17, who is teaching environmental education through skateboarding; Alex Epstein and Tania Pulido, 20 and 21, who bring urban communities together through gardening; Junior Walk, 21 who is challenging the coal industry in his own community, and Kyle Thiermann, 21, whose surf videos have created millions of dollars in environmentally responsible investments. -
Pakistan 1999
LINDSAY GRIFFIN & DAVID HAMILTON Pakistan 1999 Thanks are due to the Pakistan Ministry of Tourism, Xavier Eguskitza, andAsem Mustafa Awanfor their help in providing information. uring the summer of 1999 weather conditions in the Karakoram were Dunexceptional. Fine weather predominated from June to early July when the mid-summer deterioration set in a little earlier than usual. Unsettled conditions continued throughout late July, August and September when spells of stable weather alternated with violent storms and heavy precipitation. Ministry of Tourism statistics show that 64 expeditions received 69 permits to climb peaks over 6000m. A total of 37 permits were issued for the five 8000m peaks, resulting in 24 teams making successful ascents. The remaining 32 permits were issued to expeditions attempting 20 different peaks in the 6000m - 8000m range. Only 12 of these resulted in success. There were seven mountaineering fatalities; two on 8000m peaks and five on 7000m peaks. There was a noticeable increase in the number of expeditions visiting Pakistan despite fears that heightened tension along the Line of Control with India would cause some groups to cancel. The 8000m peaks again attracted the largest number of climbers. However there was a significant increase in the number of expeditions attempting technically challenging routes on 7000m peaks, particularly in the Hispar and Batura areas. Unfortunately few of these teams were successful. Almost 20 groups attempted high-standard big wall climbs, mostly in the Trango and Hushe areas, with a considerable amount of success. Japanese climbers were at the forefront of innovative developments on the high peaks of the Karakoram, while climbers from the USA, Germany, Spain, Italy, Norway and the Czech Republic led the way with big wall projects. -
T He M C N Eill
T he M cN eill-N ott M emorial R oute A new line on the south face of Mt. Foraker. W il l M ayo as the sky falling? The serac had avalanched with a vicious cacophony. The moment was surreal: the mind trying to recognize the cause of the roar, the delay between sight and sound too difficult for the brain to assimilate immediately. We had Wdescended merely hours before, and now we watched a serac pummel our route, filling the entire cirque at the base of Mt. Foraker’s south face with a cloud of powder blown up by debris. Thirty minutes earlier, Max and I had stood chatting with Karen McNeill and Sue Nott at the very spot where the debris had landed. After the cloud subsided, we could once again see Karen and Sue, unharmed, two dots at the bergschrund at the base of the Infinite Spur. After much swearing and exclamation, and then silence, we continued up to the shoulder, headed back to base camp. It was 8 a.m. on May 14, 2006. Maxime and I rested on the shoulder for over an hour. I sat in the blazing sun, nause ated by the irony of our mad descent in fear of a storm that hadn’t yet materialized, only to barely miss being pulverized by a serac avalanche. I was relieved to be safely off the south face; I felt like we had made the wrong decision; Maxime was disappointed, saying it was like the “Magnificent Failure.” I apologized—we had descended due to my ambivalence about the weather.