FLUCTUATIONS of GLACIERS 2005–2010 (Vol

Total Page:16

File Type:pdf, Size:1020Kb

FLUCTUATIONS of GLACIERS 2005–2010 (Vol FLUCTUATIONS OF GLACIERS 2005–2010 (Vol. X) A contribution to the Global Terrestrial Network for Glaciers (GTN-G) as part of the Global Terrestrial/Climate Observing System (GTOS/GCOS), the Division of Early Warning and Assessment and the Global Environment Outlook as part of the United Nations Environment Programme (DEWA and GEO, UNEP), and the International Hydrological Programme (IHP, UNESCO) Prepared by the World Glacier Monitoring Service (WGMS) ICSU (WDS) – IUGG (IACS) – UNEP – UNESCO – WMO 2012 FLUCTUATIONS OF GLACIERS 2005–2010 with addenda from earlier years This publication was made possible by support and funds from the Swiss Federal Office for the Environment (FOEN), the Swiss National Science Foundation (SNF; WGMS Bridging Credit), the Cryospheric Commission of the Swiss Academy of Sciences (CC, SCNAT), the Swiss GCOS Office at the Federal Office of Meteorology and Climatology (MeteoSwiss), and the Department of Geography, University of Zurich, Switzerland (GIUZ, UZH). This publication is the most recent volume in the series: FLUCTUATIONS OF GLACIERS 1959–1965 Paris, IAHS (ICSI) – UNESCO, 1967 FLUCTUATIONS OF GLACIERS 1965–1970 Paris, IAHS (ICSI) – UNESCO, 1973 FLUCTUATIONS OF GLACIERS 1970–1975 Paris, IAHS (ICSI) – UNESCO, 1977 FLUCTUATIONS OF GLACIERS 1975–1980 Paris, IAHS (ICSI) – UNESCO, 1985 FLUCTUATIONS OF GLACIERS 1980–1985 Paris, IAHS (ICSI) – UNEP – UNESCO, 1988 FLUCTUATIONS OF GLACIERS 1985–1990 Paris, IAHS (ICSI) – UNEP – UNESCO, 1993 FLUCTUATIONS OF GLACIERS 1990–1995 Paris, IAHS (ICSI) – UNEP – UNESCO, 1998 FLUCTUATIONS OF GLACIERS 1995–2000 Zurich, IUGG (CCS) – UNEP – UNESCO, 2005 FLUCTUATIONS OF GLACIERS 2000–2005 Zurich, ICSU (FAGS) – IUGG (IACS) – UNEP – UNESCO – WMO, 2008 FLUCTUATIONS OF GLACIERS 2005–2010 (Vol. X) A contribution to the Global Terrestrial Network for Glaciers (GTN-G) as part of the Global Terrestrial/Climate Observing System (GTOS/GCOS), the Division of Early Warning and Assessment and the Global Environment Outlook as part of the United Nations Environment Programme (DEWA and GEO, UNEP), and the International Hydrological Programme (IHP, UNESCO) Compiled for the World Glacier Monitoring Service by Michael Zemp, Holger Frey, Isabelle Gärtner-Roer, Samuel U. Nussbaumer, Martin Hoelzle, Frank Paul and Wilfried Haeberli Department of Geography University of Zurich Switzerland Under the auspices of the World Data System of the International Council for Science (WDS/ICSU) and the International Association of Cryospheric Sciences of the International Union of Geodesy and Geophysics (IACS/IUGG) and the United Nations Environment Programme (UNEP) and the United Nations Educational, Scientific and Cultural Organization (UNESCO) and the World Meteorological Organization (WMO) 2012 Imprint World Glacier Monitoring Service c/o Department of Geography University of Zurich Winterthurerstr. 190 8057 Zurich Switzerland http://www.wgms.ch [email protected] Editorial Board Michael Zemp, Dept. Geography, University of Zurich, Switzerland Holger Frey, Dept. Geography, University of Zurich, Switzerland Isabelle Gärtner-Roer, Dept. Geography, University of Zurich, Switzerland Samuel U. Nussbaumer, Dept. Geography, University of Zurich, Switzerland Martin Hoelzle, Dept. Geosciences, University of Fribourg, Switzerland Frank Paul, Dept. Geography, University of Zurich, Switzerland Wilfried Haeberli, Dept. Geography, University of Zurich, Switzerland Contributors Principal Investigators (see pages 5–20): data measurements, submission, and review of press proof National Correspondents (see pages 35–39): data compilation, submission, and review of press proof A. Barrueto, U. Gloor, B. Naegeli, K. Naegeli, A. Paszkowski, D. Raulin, M. Stainsby, D. Stumm, and S. Würmli: assistance with data collection and table editing Susan Braun-Clarke (Translations & Proofreading, Eichenau, Germany): language editing Printed by Staffel Druck AG 8045 Zurich Switzerland For bibliographic and reference purposes this publication should be referred to as: WGMS (2012): Fluctuations of Glaciers 2005–2010, Volume X. Zemp, M., Frey, H., Gärtner-Roer, I., Nussbaumer, S.U., Hoelzle, M., Paul, F., and Haeberli, W. (eds.), ICSU(WDS)/ IUGG(IACS)/UNEP/UNESCO/WMO, World Glacier Monitoring Service, Zurich, Switzer- land: 336 pp. Publication based on database version: doi:10.5904/wgms-fog-2012-11 ISSN 1997-910X (printed issues) ISSN 1997-9118 (online issues) The designations employed and the presentation of the material in this publication do not imply the expression of any opinion whatsoever on the part of the publishers concerning the legal status of any country or territory, or of its authorities, or concerning the frontiers of any country or territory. PREFACE by UNEP Climate change and its impacts on ecosystems and human well-being is one of the biggest challenges for mankind in the 21st century. Consistent trends in glacier changes are key indicators of ongoing climate change. Moreover, glaciers are an important component of the Earth’s hydrological system and the current accelerated melting has significant impacts on the environment and human activities, including natural hazards, water and energy supply, and global sea level rise. The long-term monitoring of glaciers is therefore a basic requirement for a scientific assessment of global glacier distribution, changes and related impacts. The standardized compilation and free dissemination of glacier data from all over the world, as undertaken by the World Glacier Monitoring Service and its predecessor organi- zations, is a major contribution in support of the work of organizations such as the United Nations Framework Convention on Climate Change (UNFCCC) and the Intergovernmen- tal Panel on Climate Change (IPCC). Glacier changes are also among the most prominent indicators used by the United Nations Environment Programme (UNEP) in assessment reports such as the Global Environment Outlook (GEO), the UNEP Yearbook series, or various editions of Global Environmental Alert Service (GEAS) bulletins. The tenth volume of the Fluctuations of Glaciers, covering the observation period be- tween 2005 and 2010, continues the series of detailed reports on measurements of glacier fluctuations reaching back to the late 19th century. It presents the latest compilation of scientific data on glacier changes in length, area, volume and mass from more than 800 glaciers around the globe. The report points out a continued overall ice loss at high rates which is consistent with ongoing global warming and corresponding energy fluxes to- wards the surface of the earth. The comprehensive Fluctuations of Glaciers reports represent the backbone of the scien- tific data compilation which comes with full meta-information on principal investigators, national correspondents, their sponsoring agencies and publication related to the reported data series. These five-yearly reports are complemented by the bi-annual Glacier Mass Balance Bulletin which presents the data in summary form for non-specialists through the use of graphic presentations rather than as purely numerical data. Together these series built the scientific background for concise and illustrated UNEP publications such as the Global Outlook for Ice and Snow (2007), Global Glacier Changes: facts and figures (2008), or Measuring Glacier Change in the Himalayas (2012) which were published for a wide range of audiences. UNEP commends the work of the WGMS and partners on this very important global issue and is grateful to all those who have supported and contributed to this long-term, global effort. Peter Gilruth, Dr. Director, Division of Early Warning and Assessment I II PREFACE by GCOS In 2012 the Global Climate Observing System (GCOS) celebrated its 20th anniversary. In 1992, when it was founded upon recommendation of the Second World Climate Confer- ence (WCC-2), certain fundamental climate records were already in place. The establish- ment of the GCOS was a response to the need to improve the understanding of the climate system observations in all its domains, i.e., atmosphere, ocean and land, in a coordinated and standardized way. Together the intergovernmental and international organizations most involved in observing the climate system, namely the WMO, the Intergovernmen- tal Oceanographic Organization (IOC) of UNESCO, the United Nations Environment Programme (UNEP) and the International Council for Science (ICSU) joined forces to establish the GCOS as a co-sponsored program coordinating a system of observing sys- tems for climate. A similar process followed in the terrestrial domain, as the need increased for a deeper understanding of global change in the Earth System. This led to the establishment of the Global Terrestrial Observing System (GTOS) jointly sponsored by UNEP, UNESCO, FAO, ICSU and WMO which is a program for observations, modelling, and analysis of terrestrial ecosystems to support sustainable development. GTOS facilitates access to information on terrestrial ecosystems so that researchers and policymakers can detect and manage global and regional environmental change. As of today five Global Terrestrial Networks (GTNs) have been defined for mountains, permafrost (GTN-P), glaciers (GTN-G), hydrology (GTN-H), and river discharge (GTN- R) to better structure some of the terrestrial observations and to improve networking among the contributing and responsible institutions. Each of these terrestrial networks is a joint, multi-institution effort. Through GCOS’ strong partnerships with users and providers of climate-related observa-
Recommended publications
  • Moüjmtaiim Operations
    L f\f¿ áfó b^i,. ‘<& t¿ ytn) ¿L0d àw 1 /1 ^ / / /This publication contains copyright material. *FM 90-6 FieW Manual HEADQUARTERS No We DEPARTMENT OF THE ARMY Washington, DC, 30 June 1980 MOÜJMTAIIM OPERATIONS PREFACE he purpose of this rUanual is to describe how US Army forces fight in mountain regions. Conditions will be encountered in mountains that have a significant effect on. military operations. Mountain operations require, among other things^ special equipment, special training and acclimatization, and a high decree of self-discipline if operations are to succeed. Mountains of military significance are generally characterized by rugged compartmented terrain witn\steep slopes and few natural or manmade lines of communication. Weather in these mountains is seasonal and reaches across the entireSspectrum from extreme cold, with ice and snow in most regions during me winter, to extreme heat in some regions during the summer. AlthoughNthese extremes of weather are important planning considerations, the variability of weather over a short period of time—and from locality to locahty within the confines of a small area—also significantly influences tactical operations. Historically, the focal point of mountain operations has been the battle to control the heights. Changes in weaponry and equipment have not altered this fact. In all but the most extreme conditions of terrain and weather, infantry, with its light equipment and mobility, remains the basic maneuver force in the mountains. With proper equipment and training, it is ideally suited for fighting the close-in battfe commonly associated with mountain warfare. Mechanized infantry can\also enter the mountain battle, but it must be prepared to dismount and conduct operations on foot.
    [Show full text]
  • European Alps Destination Guide the European Alps Breathtaking Mountain Adventures
    ss Alps Swi es | mit olo an D Tour du Mont Blanc | Itali EUROPEANDESTINATION GUIDE ALPS THE EUROPEAN ALPS BREATHTAKING MOUNTAIN ADVENTURES The European Alps are a vibrant part of If you love vast landscapes, the great outdoors, the world, overflowing with mesmerising experiencing new cultures, taking in nature, mountains. From the thrilling Tour du Mont breathing in fresh alpine air, and the company Blanc and mighty Italian Dolomites to the of like-minded walkers, then trekking in the impressive valleys and trails of the Swiss European Alps should be the next adventure Alps, they are as enticing in summer as on your list! they are under three feet of snow. I’d love to help you plan your journey. I lived in the French Alps for two years and It’s what I do best! have recently completed the Dolomites Circular Trek and the the Tour du Mont Blanc. Jodie This region holds a special place in my heart. The feeling of waking up to towering mountains each day will invoke a deep happiness in your soul. Trekking over and around these spectacular mountain ranges will give you a great sense of achievement. And at the end of each day as you enjoy a 3-course meal prepared by our local hosts you will have time to reflect on your time on the trail. All our guided treks are led by experienced and passionate International Mountain Leaders European Alps Destination Expert who have an intimate knowledge of the region. [email protected] They take safety very seriously so you know Phone: (03) 5976 3763 you will be in good hands.
    [Show full text]
  • Calving Processes and the Dynamics of Calving Glaciers ⁎ Douglas I
    Earth-Science Reviews 82 (2007) 143–179 www.elsevier.com/locate/earscirev Calving processes and the dynamics of calving glaciers ⁎ Douglas I. Benn a,b, , Charles R. Warren a, Ruth H. Mottram a a School of Geography and Geosciences, University of St Andrews, KY16 9AL, UK b The University Centre in Svalbard, PO Box 156, N-9171 Longyearbyen, Norway Received 26 October 2006; accepted 13 February 2007 Available online 27 February 2007 Abstract Calving of icebergs is an important component of mass loss from the polar ice sheets and glaciers in many parts of the world. Calving rates can increase dramatically in response to increases in velocity and/or retreat of the glacier margin, with important implications for sea level change. Despite their importance, calving and related dynamic processes are poorly represented in the current generation of ice sheet models. This is largely because understanding the ‘calving problem’ involves several other long-standing problems in glaciology, combined with the difficulties and dangers of field data collection. In this paper, we systematically review different aspects of the calving problem, and outline a new framework for representing calving processes in ice sheet models. We define a hierarchy of calving processes, to distinguish those that exert a fundamental control on the position of the ice margin from more localised processes responsible for individual calving events. The first-order control on calving is the strain rate arising from spatial variations in velocity (particularly sliding speed), which determines the location and depth of surface crevasses. Superimposed on this first-order process are second-order processes that can further erode the ice margin.
    [Show full text]
  • 4000 M Peaks of the Alps Normal and Classic Routes
    rock&ice 3 4000 m Peaks of the Alps Normal and classic routes idea Montagna editoria e alpinismo Rock&Ice l 4000m Peaks of the Alps l Contents CONTENTS FIVE • • 51a Normal Route to Punta Giordani 257 WEISSHORN AND MATTERHORN ALPS 175 • 52a Normal Route to the Vincent Pyramid 259 • Preface 5 12 Aiguille Blanche de Peuterey 101 35 Dent d’Hérens 180 • 52b Punta Giordani-Vincent Pyramid 261 • Introduction 6 • 12 North Face Right 102 • 35a Normal Route 181 Traverse • Geogrpahic location 14 13 Gran Pilier d’Angle 108 • 35b Tiefmatten Ridge (West Ridge) 183 53 Schwarzhorn/Corno Nero 265 • Technical notes 16 • 13 South Face and Peuterey Ridge 109 36 Matterhorn 185 54 Ludwigshöhe 265 14 Mont Blanc de Courmayeur 114 • 36a Hörnli Ridge (Hörnligrat) 186 55 Parrotspitze 265 ONE • MASSIF DES ÉCRINS 23 • 14 Eccles Couloir and Peuterey Ridge 115 • 36b Lion Ridge 192 • 53-55 Traverse of the Three Peaks 266 1 Barre des Écrins 26 15-19 Aiguilles du Diable 117 37 Dent Blanche 198 56 Signalkuppe 269 • 1a Normal Route 27 15 L’Isolée 117 • 37 Normal Route via the Wandflue Ridge 199 57 Zumsteinspitze 269 • 1b Coolidge Couloir 30 16 Pointe Carmen 117 38 Bishorn 202 • 56-57 Normal Route to the Signalkuppe 270 2 Dôme de Neige des Écrins 32 17 Pointe Médiane 117 • 38 Normal Route 203 and the Zumsteinspitze • 2 Normal Route 32 18 Pointe Chaubert 117 39 Weisshorn 206 58 Dufourspitze 274 19 Corne du Diable 117 • 39 Normal Route 207 59 Nordend 274 TWO • GRAN PARADISO MASSIF 35 • 15-19 Aiguilles du Diable Traverse 118 40 Ober Gabelhorn 212 • 58a Normal Route to the Dufourspitze
    [Show full text]
  • A Hydrographic Approach to the Alps
    • • 330 A HYDROGRAPHIC APPROACH TO THE ALPS A HYDROGRAPHIC APPROACH TO THE ALPS • • • PART III BY E. CODDINGTON SUB-SYSTEMS OF (ADRIATIC .W. NORTH SEA] BASIC SYSTEM ' • HIS is the only Basic System whose watershed does not penetrate beyond the Alps, so it is immaterial whether it be traced·from W. to E. as [Adriatic .w. North Sea], or from E. toW. as [North Sea . w. Adriatic]. The Basic Watershed, which also answers to the title [Po ~ w. Rhine], is short arid for purposes of practical convenience scarcely requires subdivision, but the distinction between the Aar basin (actually Reuss, and Limmat) and that of the Rhine itself, is of too great significance to be overlooked, to say nothing of the magnitude and importance of the Major Branch System involved. This gives two Basic Sections of very unequal dimensions, but the ., Alps being of natural origin cannot be expected to fall into more or less equal com­ partments. Two rather less unbalanced sections could be obtained by differentiating Ticino.- and Adda-drainage on the Po-side, but this would exhibit both hydrographic and Alpine inferiority. (1) BASIC SECTION SYSTEM (Po .W. AAR]. This System happens to be synonymous with (Po .w. Reuss] and with [Ticino .w. Reuss]. · The Watershed From .Wyttenwasserstock (E) the Basic Watershed runs generally E.N.E. to the Hiihnerstock, Passo Cavanna, Pizzo Luceridro, St. Gotthard Pass, and Pizzo Centrale; thence S.E. to the Giubing and Unteralp Pass, and finally E.N.E., to end in the otherwise not very notable Piz Alv .1 Offshoot in the Po ( Ticino) basin A spur runs W.S.W.
    [Show full text]
  • Pdf Dokument
    Udskriftsdato: 2. oktober 2021 BEK nr 517 af 23/05/2018 (Historisk) Bekendtgørelse om ændring af den fortegnelse over valgkredse, der indeholdes i lov om folketingsvalg i Grønland Ministerium: Social­ og Indenrigsministeriet Journalnummer: Økonomi­ og Indenrigsmin., j.nr. 2017­5132 Senere ændringer til forskriften LBK nr 916 af 28/06/2018 Bekendtgørelse om ændring af den fortegnelse over valgkredse, der indeholdes i lov om folketingsvalg i Grønland I medfør af § 8, stk. 1, i lov om folketingsvalg i Grønland, jf. lovbekendtgørelse nr. 255 af 28. april 1999, fastsættes: § 1. Fortegnelsen over valgkredse i Grønland affattes som angivet i bilag 1 til denne bekendtgørelse. § 2. Bekendtgørelsen træder i kraft den 1. juni 2018. Stk. 2. Bekendtgørelse nr. 476 af 17. maj 2011 om ændring af den fortegnelse over valgkredse, der indeholdes i lov om folketingsvalg i Grønland, ophæves. Økonomi- og Indenrigsministeriet, den 23. maj 2018 Simon Emil Ammitzbøll-Bille / Christine Boeskov BEK nr 517 af 23/05/2018 1 Bilag 1 Ilanngussaq Fortegnelse over valgkredse i hver kommune Kommuneni tamani qinersivinnut nalunaarsuut Kommune Valgkredse i Valgstedet eller Valgkredsens område hver kommune afstemningsdistrikt (Tilknyttede bosteder) (Valgdistrikt) (Afstemningssted) Kommune Nanortalik 1 Nanortalik Nanortalik Kujalleq 2 Aappilattoq (Kuj) Aappilattoq (Kuj) Ikerasassuaq 3 Narsaq Kujalleq Narsaq Kujalleq 4 Tasiusaq (Kuj) Tasiusaq (Kuj) Nuugaarsuk Saputit Saputit Tasia 5 Ammassivik Ammassivik Qallimiut Qorlortorsuaq 6 Alluitsup Paa Alluitsup Paa Alluitsoq Qaqortoq
    [Show full text]
  • The Eiger Myth Compiled by Marco Bomio
    The Eiger Myth Compiled by Marco Bomio Compiled by Marco Bomio, 3818 Grindelwald 1 The Myth «If the wall can be done, then we will do it – or stay there!” This assertion by Edi Rainer and Willy Angerer proved tragically true for them both – they stayed there. The first attempt on the Eiger North Face in 1936 went down in history as the most infamous drama surrounding the North Face and those who tried to conquer it. Together with their German companions Andreas Hinterstoisser and Toni Kurz, the two Austrians perished in this wall notorious for its rockfalls and suddenly deteriorating weather. The gruesome image of Toni Kurz dangling in the rope went around the world. Two years later, Anderl Heckmair, Ludwig Vörg, Heinrich Harrer and Fritz Kasparek managed the first ascent of the 1800-metre-high face. 70 years later, local professional mountaineer Ueli Steck set a new record by climbing it in 2 hours and 47 minutes. 1.1 How the Eiger Myth was made In the public perception, its exposed north wall made the Eiger the embodiment of a perilous, difficult and unpredictable mountain. The persistence with which this image has been burnt into the collective memory is surprising yet explainable. The myth surrounding the Eiger North Face has its initial roots in the 1930s, a decade in which nine alpinists were killed in various attempts leading up to the successful first ascent in July 1938. From 1935 onwards, the climbing elite regarded the North Face as “the last problem in the Western Alps”. This fact alone drew the best climbers – mainly Germans, Austrians and Italians at the time – like a magnet to the Eiger.
    [Show full text]
  • Ilulissat Icefjord
    World Heritage Scanned Nomination File Name: 1149.pdf UNESCO Region: EUROPE AND NORTH AMERICA __________________________________________________________________________________________________ SITE NAME: Ilulissat Icefjord DATE OF INSCRIPTION: 7th July 2004 STATE PARTY: DENMARK CRITERIA: N (i) (iii) DECISION OF THE WORLD HERITAGE COMMITTEE: Excerpt from the Report of the 28th Session of the World Heritage Committee Criterion (i): The Ilulissat Icefjord is an outstanding example of a stage in the Earth’s history: the last ice age of the Quaternary Period. The ice-stream is one of the fastest (19m per day) and most active in the world. Its annual calving of over 35 cu. km of ice accounts for 10% of the production of all Greenland calf ice, more than any other glacier outside Antarctica. The glacier has been the object of scientific attention for 250 years and, along with its relative ease of accessibility, has significantly added to the understanding of ice-cap glaciology, climate change and related geomorphic processes. Criterion (iii): The combination of a huge ice sheet and a fast moving glacial ice-stream calving into a fjord covered by icebergs is a phenomenon only seen in Greenland and Antarctica. Ilulissat offers both scientists and visitors easy access for close view of the calving glacier front as it cascades down from the ice sheet and into the ice-choked fjord. The wild and highly scenic combination of rock, ice and sea, along with the dramatic sounds produced by the moving ice, combine to present a memorable natural spectacle. BRIEF DESCRIPTIONS Located on the west coast of Greenland, 250-km north of the Arctic Circle, Greenland’s Ilulissat Icefjord (40,240-ha) is the sea mouth of Sermeq Kujalleq, one of the few glaciers through which the Greenland ice cap reaches the sea.
    [Show full text]
  • Picturing France
    Picturing France Classroom Guide VISUAL ARTS PHOTOGRAPHY ORIENTATION ART APPRECIATION STUDIO Traveling around France SOCIAL STUDIES Seeing Time and Pl ace Introduction to Color CULTURE / HISTORY PARIS GEOGRAPHY PaintingStyles GOVERNMENT / CIVICS Paris by Night Private Inve stigation LITERATURELANGUAGE / CRITICISM ARTS Casual and Formal Composition Modernizing Paris SPEAKING / WRITING Department Stores FRENCH LANGUAGE Haute Couture FONTAINEBLEAU Focus and Mo vement Painters, Politics, an d Parks MUSIC / DANCENATURAL / DRAMA SCIENCE I y Fontainebleau MATH Into the Forest ATreebyAnyOther Nam e Photograph or Painting, M. Pa scal? ÎLE-DE-FRANCE A Fore st Outing Think L ike a Salon Juror Form Your Own Ava nt-Garde The Flo ating Studio AUVERGNE/ On the River FRANCHE-COMTÉ Stream of Con sciousness Cheese! Mountains of Fra nce Volcanoes in France? NORMANDY “I Cannot Pain tan Angel” Writing en Plein Air Culture Clash Do-It-Yourself Pointillist Painting BRITTANY Comparing Two Studie s Wish You W ere Here Synthétisme Creating a Moo d Celtic Culture PROVENCE Dressing the Part Regional Still Life Color and Emo tion Expressive Marks Color Collectio n Japanese Prin ts Legend o f the Château Noir The Mistral REVIEW Winds Worldwide Poster Puzzle Travelby Clue Picturing France Classroom Guide NATIONAL GALLERY OF ART, WASHINGTON page ii This Classroom Guide is a component of the Picturing France teaching packet. © 2008 Board of Trustees of the National Gallery of Art, Washington Prepared by the Division of Education, with contributions by Robyn Asleson, Elsa Bénard, Carla Brenner, Sarah Diallo, Rachel Goldberg, Leo Kasun, Amy Lewis, Donna Mann, Marjorie McMahon, Lisa Meyerowitz, Barbara Moore, Rachel Richards, Jennifer Riddell, and Paige Simpson.
    [Show full text]
  • Alpine Adventures 2019 68
    RYDER WALKER THE GLOBAL TREKKING SPECIALISTS ALPINE ADVENTURES 2019 68 50 RYDER WALKER ALPINE ADVENTURES CONTENTS 70 Be the first to know. Scan this code, or text HIKING to 22828 and receive our e-newsletter. We’ll send you special offers, new trip info, RW happenings and more. 2 RYDERWALKER.COM | 888.586.8365 CONTENTS 4 Celebrating 35 years of Outdoor Adventure 5 Meet Our Team 6 Change and the Elephant in the Room 8 Why Hiking is Important – Watching Nature 10 Choosing the Right Trip for You 11 RW Guide to Selecting Your Next Adventure 12 Inspired Cuisine 13 First Class Accommodations 14 Taking a Closer Look at Huts 15 Five Reasons Why You Should Book a Guided Trek 16 Self-Guided Travel 17 Guided Travel & Private Guided Travel EASY TO MODERATE HIKING 18 Highlights of Switzerland: Engadine, Lago Maggiore, Zermatt 20 England: The Cotswolds 22 Isola di Capri: The Jewel of Southern Italy NEW 24 French Alps, Tarentaise Mountains: Bourg Saint Maurice, Sainte Foy, Val d’Isère 26 Sedona, Arches & Canyonlands 28 Croatia: The Dalmatian Coast 28 30 Engadine Trek 32 Scotland: Rob Roy Way 34 Montenegro: From the Durmitor Mountain Range to the Bay of Kotor 36 New Mexico: Land of Enchantment, Santa Fe to Taos NEW 38 Slovakia: Discover the Remote High Tatras Mountains NEW MODERATE TO CHALLENGING HIKING 40 Heart of Austria 42 Italian Dolomites Trek 44 High Peaks of the Bavarian Tyrol NEW 46 Sicily: The Aeolian Islands 48 Rocky Mountain High Life: Aspen to Telluride 50 New Brunswick, Canada: Bay of Fundy 52 Via Ladinia: Italian Dolomites 54 Dolomiti di
    [Show full text]
  • Articles, Only Recently
    Nat. Hazards Earth Syst. Sci., 16, 2085–2106, 2016 www.nat-hazards-earth-syst-sci.net/16/2085/2016/ doi:10.5194/nhess-16-2085-2016 © Author(s) 2016. CC Attribution 3.0 License. Climate anomalies associated with the occurrence of rockfalls at high-elevation in the Italian Alps Roberta Paranunzio1, Francesco Laio1, Marta Chiarle2, Guido Nigrelli2, and Fausto Guzzetti3 1Department of Environment, Land and Infrastructure Engineering, Politecnico di Torino, Torino, Italy 2Research Institute for Geo-hydrological Protection, National Research Council (CNR IRPI), Torino, Italy 3Research Institute for Geo-hydrological Protection, National Research Council (CNR IRPI), Perugia, Italy Correspondence to: Roberta Paranunzio ([email protected]) Received: 29 March 2016 – Published in Nat. Hazards Earth Syst. Sci. Discuss.: 4 April 2016 Revised: 13 July 2016 – Accepted: 22 August 2016 – Published: 12 September 2016 Abstract. Climate change is seriously affecting the 1 Introduction cryosphere in terms, for example, of permafrost thaw, al- teration of rain=snow ratio, and glacier shrinkage. There is concern about the increasing number of rockfalls at high el- The recent decades have seen a pronounced warming in evation in the last decades. Nevertheless, the exact role of global climate, primarily at high elevations and high latitudes climate parameters in slope instability at high elevation has (Schär et al., 2004). Temperature across European Alps has ◦ not been fully explored yet. In this paper, we investigate 41 increased of about 1.4 K per century over the period 1906– rockfalls listed in different sources (newspapers, technical re- 2005, which is more than double the global average (Brunetti ports, and CNR IRPI archive) in the elevation range 1500– et al., 2009) and further increases are expected according to 4200 m a.s.l.
    [Show full text]
  • The Role of Sherpa Culture in Nature Conservation
    The Role of SHERPA CULTURE in NATURE CONSERVATION Copyright © Khumbu Sherpa Culture Conservation Society www.khumbusherpaculture.org Book : The Role of Sherpa Culture in Nature Conservation Publisher : Khumbu Sherpa Culture Conservation Society (KSCCS) Published Year : 2073 B.S. Edition : First Writer & Photographer : Tenzing Tashi Sherpa Typing & Translation : Tsherin Ongmu Sherpa Editor : Professor Stan Stevens, Ph.D. Design, Layout & Print : Digiscan Pre-press Pvt. Ltd., Naxal, Kathmandu The Role of SHERPA CULTURE in NATURE CONSERVATION Table of Contents 1. The Role of Sherpa Culture in Nature Conservation 1 Khumbu is a Sherpa Community Conserved Area 2 Sacred Himalayas 3 Sacred Lakes - Gokyo Lake 5 Springs 9 Religious Conserved Forests 10 Community Conserved Forest 11 Bird Conservation Area 12 Grazing Management Areas for Livestock 12 Conservation Tradition 13 Nawa System for Conservation 14 The Rules of Singhki Nawa (Wood Custodian) 14 The Custom of the Lhothok Nawa (Crop and Pastures Custodian) 15 The Work and the Duty Term of the Nawa and Worshyo 17 Yulthim (Community Assembly) 18 The Rules and Laws of Community 19 Short Story by Reincarnated Lama Ngawang Tenzing Zangbu about Nawa 20 The Sacred Worship Areas of Sherpas 21 Nangajong 21 Worshyo 22 Pangboche 23 Places in Between Fungi Thyanga Bridge and Pangboche Bridge 25 Khumjung and Khunde 29 Khumbu’s Chortens 33 Agriculture of Khumbu 35 Mountains Around Khumbu 38 2. The Role of KSCCS in Nature Conservation 39 A. Cultural Interaction 39 B. Cultural and ICCA Educational Tour 40 1. Community Tour 40 2. Sherpa Culture and Conservation Tour for Students Organized by Khumjung by KSCCS 41 3.
    [Show full text]