A Distant View of a Snowy Range: Freshfield and Sella on the Tour of Kangchenjunga, 1899
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Rapid Climate Vulnerability Assessment of Gangtok, Sikkim
February, 2018 RAPID CLIMATE VULNERABILITY ASSESSMENT OF GANGTOK, SIKKIM Developing Disaster Resilience Action Plan Through GIS & Prioritising Actions for Natural Disaster Risk Reduction in Urban Agglomerations of Shillong & Gangtok Gangtok City, Sikkim Gangtok, the capital city of Sikkim, is located in the eastern Himalayan range. The city is flanked on east and west by two streams, namely Roro Chu and Ranikhola, respectively, comprising 17 municipal wards. These two rivers divide the natural drainage into two parts, the eastern and western parts. Fig 1: Gangtok City map Gangtok City Characteristics Indicators Characteristics Classification of the city Hill Location 27°20’N 88°37’E Area 19.016 sq.km Climate Type Subtropical highland climate Temperature Average Annual Maximum Temperature - 27°C Average Annual Minimum Temperature - 19°C Rainfall Average annual : 3494 mm Height above Mean Sea Level 1,676 m above MSL Fig2: The main road connecting Gangtok to other cities Fig3: Gangtok M G Marg and towns Steep slopes, vulnerability to landslides, large forest cover and inadequate access to most areas characterize Gangtok. Unplanned urbanization and rapid construction on the hill slopes has increased the risk of environmental degradation in Gangtok. Hazard Exposure Sl. No Hazard Type Exposure 1 Flash Flood Y 2 Drought/ Heat Wave N 3 Earthquakes Y 4 Landslides Y 5 Forest Fires Y 6 Heavy Rainfall Y 7 Hailstorms/thundering Y Hazard Timeline Index Jan Feb Mar Apr May Jun Jul Aug Sept Oct Nov Dec Landslides Flash Flood Hailstorm/thundering Forest -
Probabilistic Travel Model of Gangtok City, Sikkim, India FINAL.Pdf
European Journal of Geography Volume 4, Issue2: 46-54, 2013 © Association of European Geographers ANALYSIS OF TOURISM ATTRACTIVENESS USING PROBABILISTIC TRAVEL MODEL: A STUDY ON GANGTOK AND ITS SURROUNDINGS Suman PAUL Krishnagar Govt. College, Department of Geography Nadia, West Bengal, India. Pin-741101 http://www.krishnagargovtcollege.org/ [email protected] Abstract: Tourism is now one of the largest industries in the world that has developed alongside the fascinating concept of eco-tourism. The concept of tourism could be traced back to ancient times when people travelled with a view to acquiring knowledge of unknown lands and people, for the development of trade and commerce, for religious preaching and also for the sheer adventure of discovery. In fact the system of tourism involves a combination of travel, destination and marketing, which lead to a process of its cultural dimension. Gangtok as a core centre of Sikkim has potential command area over different tourist spots in East Sikkim, which are directly linked by a network of roads centering Gangtok and are perfectly accessible for one-day trips. The tourist attractions of East Sikkim are clustered mostly in and around Gangtok, the state capital. This study shows the tourism infrastructure as well as seasonal arrival of tourists in the Gangtok city and to develop the probabilistic travel model on the basis of tourist perception which will help the tourism department for the further economic development of the area. KeyWords: Eco-tourism, command area, tourist attractions, probabilistic travel model 1. INTRODUCTION Tourism is now one of the largest industries in the world that has developed alongside the fascinating concept of eco-tourism. -
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. -
Khangchendzonga National Park
ASIA / PACIFIC KHANGCHENDZONGA NATIONAL PARK INDIA Sacred site in the Khangchendzonga National Park - © IUCN Tilman Jaeger India - Khangchendzonga National Park WORLD HERITAGE NOMINATION – IUCN TECHNICAL EVALUATION KHANGCHENDZONGA NATIONAL PARK (INDIA) – ID 1513 IUCN RECOMMENDATION TO WORLD HERITAGE COMMITTEE: To inscribe the property under natural criteria. Key paragraphs of Operational Guidelines: Paragraph 77: Nominated property meets World Heritage criteria. Paragraph 78: Nominated property meets integrity and protection and management requirements. 1. DOCUMENTATION Kangchenjunga Transboundary Conservation and Development Initiative in the Hindu Kush Himalayas. a) Date nomination received by IUCN: 16 March Prepared for TBPA. Krishna AP, Chhetri S, Singh KK 2015 (2002) Human Dimensions of Conservation in the Khangchendzonga Biosphere Reserve: The Need for b) Additional information officially requested from Conflict Prevention. Mountain Research and and provided by the State Party: Khangchendzonga Development 22(4):328-331. Lachungpa U (2009) National Park is nominated as a mixed site. ICOMOS Indigenous Lifstyles and Biodiversity Conservation wrote to the State Party in September, 2015 Issues in North Sikkim. Indian Journal of Traditional requesting supplementary information on a range of Knowledge 8(1): 51-55. Oli KP, Chaudhary S, Sharma issues related to the evaluation of cultural values. A UR (2013) Are Governance and Management Effective joint IUCN / ICOMOS progress report was then sent on within Protected Areas of the Kanchenjunga 17 December 2015 following the respective ICOMOS Landscape (Bhutan, India And Nepal)? PARKS 19(1): and IUCN Panel meetings. Requests were made of the 25-36. Sathyakumar S, Bashir T, Bhattacharya T, State Party to update the biodiversity inventory for Poudyal K (2011b) Mammals of the Khangchendzonga species within the property; consider changes to the Biosphere Reserve, Sikkim, India. -
INTRODUCTION 1 1 Lepcha Is a Tibeto-Burman Language Spoken In
CHAPTER ONE INTRODUCTION 11 Lepcha is a Tibeto-Burman language spoken in Sikkim, Darjeeling district in West Bengal in India, in Ilm district in Nepal, and in a few villages of Samtsi district in south-western Bhutan. The tribal home- land of the Lepcha people is referred to as ne mayLe VÎa ne máyel lyáng ‘hidden paradise’ or ne mayLe malUX VÎa ne máyel málúk lyáng ‘land of eternal purity’. Most of the areas in which Lepcha is spoken today were once Sikkimese territory. The kingdom of Sikkim used to com- prise all of present-day Sikkim and most of Darjeeling district. Kalim- pong, now in Darjeeling district, used to be part of Bhutan, but was lost to the British and became ‘British Bhutan’ before being incorpo- rated into Darjeeling district. The Lepcha are believed to be the abo- riginal inhabitants of Sikkim. Today the Lepcha people constitute a minority of the population of modern Sikkim, which has been flooded by immigrants from Nepal. Although the Lepcha themselves estimate their number of speakers to be over 50,000, the total number is likely to be much smaller. Accord- ing to the 1991 Census of India, the most recent statistical profile for which the data have been disaggregated, the total number of mother tongue Lepcha speakers across the nation is 29,854. While their dis- tribution is largely in Sikkim and the northern districts of West Ben- gal, there are no reliable speaker numbers for these areas. In the Dar- jeeling district there are many Lepcha villages particularly in the area surrounding the small town of Kalimpong. -
Inscribed 6 (2).Pdf
Inscribed6 CONTENTS 1 1. AVIATION 33 2. MILITARY 59 3. NAVAL 67 4. ROYALTY, POLITICIANS, AND OTHER PUBLIC FIGURES 180 5. SCIENCE AND TECHNOLOGY 195 6. HIGH LATITUDES, INCLUDING THE POLES 206 7. MOUNTAINEERING 211 8. SPACE EXPLORATION 214 9. GENERAL TRAVEL SECTION 1. AVIATION including books from the libraries of Douglas Bader and “Laddie” Lucas. 1. [AITKEN (Group Captain Sir Max)]. LARIOS (Captain José, Duke of Lerma). Combat over Spain. Memoirs of a Nationalist Fighter Pilot 1936–1939. Portrait frontispiece, illustrations. First edition. 8vo., cloth, pictorial dust jacket. London, Neville Spearman. nd (1966). £80 A presentation copy, inscribed on the half title page ‘To Group Captain Sir Max AitkenDFC. DSO. Let us pray that the high ideals we fought for, with such fervent enthusiasm and sacrifice, may never be allowed to perish or be forgotten. With my warmest regards. Pepito Lerma. May 1968’. From the dust jacket: ‘“Combat over Spain” is one of the few first-hand accounts of the Spanish Civil War, and is the only one published in England to be written from the Nationalist point of view’. Lerma was a bomber and fighter pilot for the duration of the war, flying 278 missions. Aitken, the son of Lord Beaverbrook, joined the RAFVR in 1935, and flew Blenheims and Hurricanes, shooting down 14 enemy aircraft. Dust jacket just creased at the head and tail of the spine. A formidable Vic formation – Bader, Deere, Malan. 2. [BADER (Group Captain Douglas)]. DEERE (Group Captain Alan C.) DOWDING Air Chief Marshal, Lord), foreword. Nine Lives. Portrait frontispiece, illustrations. First edition. -
The PLATEAU – North Sikkim
JAPANESE ALPINE NEWS 2013 ● HARISH KAPADIA THE PLATEAU Mountains of Sikkim – China Border This was my fifth visit to the mountains of Sikkim. As a young student I was part of the training course of the Himalayan Mountaineering Institute in 1964. The mountains of west Sikkim, like Kabru, Rathong, Pandim and host of others were attractive to my young eyes. I returned in 1976. No sooner Sikkim became a state on India two us, Zerksis Boga and I obtained permits and roamed the valleys for more than a month in the northwest Sikkim, covering Zemu glacier, Lhonak valley Muguthang, Lugnak la, Sebu la and returned via the Lachung valley. I returned a few times to Darjeeling and Sikkim valleys visiting the Singalila ridge, lakes of lower Sikkim and surroundings of Gangtok and Kalimpong. If you stretch the area to the south, I made several visits to Darjeeling and nearby hills over the years. Moreover in Sikkim the approach to different valleys is so varied that it gives a feeling of trekking in different Himalayan zones. 1 High Himalayan Unknown Valleys, by Harish Kapadia, p.156. (Indus Books, New Delhi, 2001). Also Himalayan Journal, Vol.35, p.181 57 ● JAPANESE ALPINE NEWS 2013 In no other country on earth can one find such a variety of micro-climates within such a short distance as Sikkim, declared the eminent English botanist and explorer Joseph Hooker in his Himalayan Journals (1854), which documented his work collecting and classifying thousands of plants in the Himalaya in the mid-19th century. In the shadow of the Himalayas, by John Claude White, 1883 – 1908. -
13 Protection: a Means for Sustainable Development? The
13 Protection: A Means for Sustainable Development? The Case of the Jungfrau- Aletsch-Bietschhorn World Heritage Site in Switzerland Astrid Wallner1, Stephan Rist2, Karina Liechti3, Urs Wiesmann4 Abstract The Jungfrau-Aletsch-Bietschhorn World Heritage Site (WHS) comprises main- ly natural high-mountain landscapes. The High Alps and impressive natu- ral landscapes are not the only feature making the region so attractive; its uniqueness also lies in the adjoining landscapes shaped by centuries of tra- ditional agricultural use. Given the dramatic changes in the agricultural sec- tor, the risk faced by cultural landscapes in the World Heritage Region is pos- sibly greater than that faced by the natural landscape inside the perimeter of the WHS. Inclusion on the World Heritage List was therefore an opportunity to contribute not only to the preservation of the ‘natural’ WHS: the protected part of the natural landscape is understood as the centrepiece of a strategy | downloaded: 1.10.2021 to enhance sustainable development in the entire region, including cultural landscapes. Maintaining the right balance between preservation of the WHS and promotion of sustainable regional development constitutes a key chal- lenge for management of the WHS. Local actors were heavily involved in the planning process in which the goals and objectives of the WHS were defined. This participatory process allowed examination of ongoing prob- lems and current opportunities, even though present ecological standards were a ‘non-negotiable’ feature. Therefore the basic patterns of valuation of the landscape by the different actors could not be modified. Nevertheless, the process made it possible to jointly define the present situation and thus create a basis for legitimising future action. -
Glacier Fluctuations During the Past 2000 Years
Quaternary Science Reviews 149 (2016) 61e90 Contents lists available at ScienceDirect Quaternary Science Reviews journal homepage: www.elsevier.com/locate/quascirev Invited review Glacier fluctuations during the past 2000 years * Olga N. Solomina a, , Raymond S. Bradley b, Vincent Jomelli c, Aslaug Geirsdottir d, Darrell S. Kaufman e, Johannes Koch f, Nicholas P. McKay e, Mariano Masiokas g, Gifford Miller h, Atle Nesje i, j, Kurt Nicolussi k, Lewis A. Owen l, Aaron E. Putnam m, n, Heinz Wanner o, Gregory Wiles p, Bao Yang q a Institute of Geography RAS, Staromonetny-29, 119017 Staromonetny, Moscow, Russia b Department of Geosciences, University of Massachusetts, Amherst, MA 01003, USA c Universite Paris 1 Pantheon-Sorbonne, CNRS Laboratoire de Geographie Physique, 92195 Meudon, France d Department of Earth Sciences, University of Iceland, Askja, Sturlugata 7, 101 Reykjavík, Iceland e School of Earth Sciences and Environmental Sustainability, Northern Arizona University, Flagstaff, AZ 86011, USA f Department of Geography, Brandon University, Brandon, MB R7A 6A9, Canada g Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales (IANIGLA), CCT CONICET Mendoza, CC 330 Mendoza, Argentina h INSTAAR and Geological Sciences, University of Colorado Boulder, USA i Department of Earth Science, University of Bergen, Allegaten 41, N-5007 Bergen, Norway j Uni Research Climate AS at Bjerknes Centre for Climate Research, Bergen, Norway k Institute of Geography, University of Innsbruck, Innrain 52, 6020 Innsbruck, Austria l Department of Geology, -
19Th Century Glacier Representations and Fluctuations in the Central and Western European Alps: an Interdisciplinary Approach ⁎ ⁎ H.J
Available online at www.sciencedirect.com Global and Planetary Change 60 (2008) 42–57 www.elsevier.com/locate/gloplacha 19th century glacier representations and fluctuations in the central and western European Alps: An interdisciplinary approach ⁎ ⁎ H.J. Zumbühl , D. Steiner , S.U. Nussbaumer Institute of Geography, University of Bern, Hallerstrasse 12, CH-3012 Bern, Switzerland Received in revised form 22 August 2006; accepted 24 August 2006 Available online 22 February 2007 Abstract European Alpine glaciers are sensitive indicators of past climate and are thus valuable sources of climate history. Unfortunately, direct determinations of glacier changes (length variations and mass changes) did not start with increasing accuracy until just before the end of the 19th century. Therefore, historical and physical methods have to be used to reconstruct glacier variability for preceeding time periods. The Lower Grindelwald Glacier, Switzerland, and the Mer de Glace, France, are examples of well-documented Alpine glaciers with a wealth of different historical sources (e.g. drawings, paintings, prints, photographs, maps) that allow reconstruction of glacier length variations for the last 400–500 years. In this paper, we compare the length fluctuations of both glaciers for the 19th century until the present. During the 19th century a majority of Alpine glaciers – including the Lower Grindelwald Glacier and the Mer de Glace – have been affected by impressive glacier advances. The first maximum extent around 1820 has been documented by drawings from the artist Samuel Birmann, and the second maximum extent around 1855 is shown by photographs of the Bisson Brothers. These pictorial sources are among the best documents of the two glaciers for the 19th century. -
Ernest Shackleton and the Epic Voyage of the Endurance
9-803-127 REV: DECEMBER 2, 2010 NANCY F. KOEHN Leadership in Crisis: Ernest Shackleton and the Epic Voyage of the Endurance For scientific discovery give me Scott; for speed and efficiency of travel give me Amundsen; but when disaster strikes and all hope is gone, get down on your knees and pray for Shackleton. — Sir Raymond Priestley, Antarctic Explorer and Geologist On January 18, 1915, the ship Endurance, carrying a highly celebrated British polar expedition, froze into the icy waters off the coast of Antarctica. The leader of the expedition, Sir Ernest Shackleton, had planned to sail his boat to the coast through the Weddell Sea, which bounded Antarctica to the north, and then march a crew of six men, supported by dogs and sledges, to the Ross Sea on the opposite side of the continent (see Exhibit 1).1 Deep in the southern hemisphere, it was early in the summer, and the Endurance was within sight of land, so Shackleton still had reason to anticipate reaching shore. The ice, however, was unusually thick for the ship’s latitude, and an unexpected southern wind froze it solid around the ship. Within hours the Endurance was completely beset, a wooden island in a sea of ice. More than eight months later, the ice still held the vessel. Instead of melting and allowing the crew to proceed on its mission, the ice, moving with ocean currents, had carried the boat over 670 miles north.2 As it moved, the ice slowly began to soften, and the tremendous force of distant currents alternately broke apart the floes—wide plateaus made of thousands of tons of ice—and pressed them back together, creating rift lines with huge piles of broken ice slabs. -
Modeling Glacier Thickness Distribution and Bed Topography Over Entire Mountain Ranges with Glabtop: Application of a Fast and Robust Approach
Zurich Open Repository and Archive University of Zurich Main Library Strickhofstrasse 39 CH-8057 Zurich www.zora.uzh.ch Year: 2012 Modeling glacier thickness distribution and bed topography over entire mountain ranges with GlabTop: Application of a fast and robust approach Linsbauer, Andreas ; Paul, Frank ; Haeberli, Wilfried Abstract: The combination of glacier outlines with digital elevation models (DEMs) opens new dimen- sions for research on climate change impacts over entire mountain chains. Of particular interest is the modeling of glacier thickness distribution, where several new approaches were proposed recently. The tool applied herein, GlabTop (Glacier bed Topography) is a fast and robust approach to model thickness distribution and bed topography for large glacier samples using a Geographic Information System (GIS). The method is based on an empirical relation between average basal shear stress and elevation range of individual glaciers, calibrated with geometric information from paleoglaciers, and validated with radio echo soundings on contemporary glaciers. It represents an alternative and independent test possibility for approaches based on mass-conservation and flow. As an example for using GlabTop in entire mountain ranges, we here present the modeled ice thickness distribution and bed topography for all Swiss glaciers along with a geomorphometric analysis of glacier characteristics and the overdeepenings found in the modeled glacier bed. These overdeepenings can be seen as potential sites for future lake formation and are thus highly relevant in connection with hydropower production and natural hazards. The thickest ice of the largest glaciers rests on weakly inclined bedrock at comparably low elevations, resulting in a limited potential for a terminus retreat to higher elevations.