Late Holocene Glacier Change in the Eastern Nyainqêntanglha Range, SE Tibet

Total Page:16

File Type:pdf, Size:1020Kb

Late Holocene Glacier Change in the Eastern Nyainqêntanglha Range, SE Tibet Late Holocene glacier change in the eastern Nyainqêntanglha Range, SE Tibet Von der Fakultät für Georessourcen und Materialtechnik der Rheinisch‐Westfälischen Technischen Hochschule Aachen zur Erlangung des akademischen Grades eines Doktors der Naturwissenschaften genehmigte Dissertation vorgelegt von M.A. David Loibl aus Aachen Berichter: Univ.‐Prof. Dr. rer. nat. Frank Lehmkuhl Univ.‐Prof. Dr. rer. nat. Achim Bräuning Tag der mündlichen Prüfung: 06. Juli 2015 Diese Dissertation ist auf den Internetseiten der Hochschulbibliothek online verfügbar. Table of contents List of figures .................................................................................................................................... i List of tables .................................................................................................................................... ii List of abbreviations ....................................................................................................................... iii 1 Introduction ................................................................................................................................. 1 1.1 Motivation ..................................................................................................................................... 1 1.2 Objectives and approach ............................................................................................................... 2 1.3 Thesis outline................................................................................................................................. 3 2 Current state of research .............................................................................................................. 5 2.1 Atmospheric circulation patterns .................................................................................................. 5 2.2 Paleoclimate and glacier fluctuations ........................................................................................... 7 2.2.1 Paleoclimate reconstruction ................................................................................................................. 7 2.2.2 Holocene paleoclimate on the Tibetan Plateau .................................................................................. 10 2.2.3 Glaciers and climate change ................................................................................................................ 13 2.2.4 Late Holocene glacier fluctuations and climatic forcing ...................................................................... 14 2.2.5 Human perspective: risks and challenges ........................................................................................... 15 2.3 Methodological background ....................................................................................................... 15 2.3.1 Remote sensing of glaciers .................................................................................................................. 15 2.3.2 Equilibrium line altitude calculation .................................................................................................... 17 2.3.3 Dating of Holocene glacier deposits .................................................................................................... 19 3 Regional setting .......................................................................................................................... 22 3.1 Geology ........................................................................................................................................ 22 3.2 Climate ......................................................................................................................................... 23 3.3 Geomorphology ........................................................................................................................... 25 3.4 Glaciers ........................................................................................................................................ 26 3.5 Vegetation ................................................................................................................................... 27 4 Reconstructing glacier retreat since the Little Ice Age in SE Tibet by glacier mapping and equilibrium line altitude calculation .............................................................................................. 28 4.1 Introduction ................................................................................................................................. 28 4.2 Regional setting and glacier distribution ..................................................................................... 30 4.3 Methods and materials ............................................................................................................... 33 4.3.1 Data selection ...................................................................................................................................... 33 4.3.2 Glacier mapping .................................................................................................................................. 35 4.3.3 Glacier classification ............................................................................................................................ 36 4.3.4 Calculation of ELA estimates ............................................................................................................... 38 4.3.5 Fieldwork ............................................................................................................................................. 39 4.4 Results ......................................................................................................................................... 40 4.4.1 Glacier case studies ............................................................................................................................. 40 4.4.2 Glacier types and spatial distribution .................................................................................................. 41 4.4.3 Length change analysis ........................................................................................................................ 44 4.4.4 ELA calculations ................................................................................................................................... 46 4.5 Discussion .................................................................................................................................... 50 4.5.1 Quality assessment .............................................................................................................................. 50 4.5.2 Influences of topography and climate ................................................................................................. 51 4.5.3 Glacier change ..................................................................................................................................... 52 4.5.4 Monsoon and glaciers ......................................................................................................................... 53 4.6 Conclusions .................................................................................................................................. 55 5 Glaciers and equilibrium line altitudes of the eastern Nyainqêntanglha Range, SE Tibet ............. 58 5.1 Introduction ................................................................................................................................. 58 5.2 Study area .................................................................................................................................... 59 5.3 Methods ...................................................................................................................................... 62 5.3.1 Data and glacier mapping .................................................................................................................... 62 5.3.2 Glacier classification ............................................................................................................................ 64 5.3.3 ELA calculation .................................................................................................................................... 64 5.3.4 Post‐processing ................................................................................................................................... 66 5.4 Map Design .................................................................................................................................. 66 5.5 Interpretation .............................................................................................................................. 67 5.6 Conclusions .................................................................................................................................. 69 5.7 Software ...................................................................................................................................... 69 6 Toward a late Holocene glacial chronology for the eastern Nyainqêntanglha Range, southeastern Tibet ............................................................................................................................................. 70 6.1 Introduction ................................................................................................................................. 70 6.2 Regional setting ..........................................................................................................................
Recommended publications
  • Jean Kingdon-Ward F
    HILL SO STRONG JEAN KINGDON-WARD F. R. G. S. And in my prosperity I said, I shall never be removed: thou, Lord, of Thy goodness hast made my hill so strong. Psalm 30, v 6 JONATHAN CAPE THIRTY BEDFORD SQUARE LONDON FIRST PUBLISHED I952 PRINTED IN OREAT BRITAIN IN THE cInOF OXFORD AT THE ALDEN PRESS BOUND BY A. W. BAIN & CO. LTD., LONDON ILLUSTRATIONS THE RIMA ROPE BRIDGE Frontispiece A ZACKRING PEASANT facing P* 44 TIBETAN PORTER (note goitre) 44 AKKEY AND PHAG TSERING 44 A MIJU MISHMI 44 THE RIMA BASIN (before the earthquake) 76 THE V-SIDED VALLEY OF THE DI CHU I I4 THE PEAKS OF DONG, NEAR WALONG "4 TIBETANS CARRYING 100 LB. LOADS IN THE DI CHU GORGE 142 THE DIPHU LA PATROL PASSING THE WRECKAGE OF CAPTAIN SAILO'S CAMP I 76 HAV. INDRA BAHADUR LIMBU 208 HAV. PAHAL SING RANA 208 JEM. BIR BAHADUR GURUNG 208 RFM. TAKEM ABOR 208 NOT SNOW BUT BARE ROCK (photo: N. E. B. Warner) 232 10,000 FT. PEAK IN THE LOHIT VALLEY * 32 All of these illustrations are reproduced from photographs taken by Mr. and Mrs. Kingdon-Ward with the one exception noted above. MAP THE LOHIT VALLEY facing fi. 13 PREFACE As this book is not a scientific one, it may be of interest to readers to know where they can find a more technical descrip- tion of matters discussed in it. Plant Hunting in the Lohit Valley by F. Kingdon-Ward discusses the botanical and horticultural aspects of the expedition (it is to be found in the Jounzal of the Royal Horticultural Society, June 1952); while an account of the Great Assam Earthquake of 1950, from the seismologist's point of view, appeared in Nature on January 27th, 1951, together with an eye-witness account of the earthquake and its after effects by F.
    [Show full text]
  • Channel Morphology and Bedrock River Incision: Theory, Experiments, and Application to the Eastern Himalaya
    Channel morphology and bedrock river incision: Theory, experiments, and application to the eastern Himalaya Noah J. Finnegan A dissertation submitted in partial fulfillment of the requirements for the degree of Doctor of Philosophy University of Washington 2007 Program Authorized to Offer Degree: Department of Earth and Space Sciences University of Washington Graduate School This is to certify that I have examined this copy of a doctoral dissertation by Noah J. Finnegan and have found that it is complete and satisfactory in all respects, and that any and all revisions required by the final examining committee have been made. Co-Chairs of the Supervisory Committee: ___________________________________________________________ Bernard Hallet ___________________________________________________________ David R. Montgomery Reading Committee: ____________________________________________________________ Bernard Hallet ____________________________________________________________ David R. Montgomery ____________________________________________________________ Gerard Roe Date:________________________ In presenting this dissertation in partial fulfillment of the requirements for the doctoral degree at the University of Washington, I agree that the Library shall make its copies freely available for inspection. I further agree that extensive copying of the dissertation is allowable only for scholarly purposes, consistent with “fair use” as prescribed in the U.S. Copyright Law. Requests for copying or reproduction of this dissertation may be referred
    [Show full text]
  • Recent Glacier Mass Balance and Area Changes in the Kangri Karpo Mountains from Dems and Glacier Inventories
    1 Recent glacier mass balance and area changes in the 2 Kangri Karpo Mountains from DEMs and glacier inventories 3 4 Wu Kunpeng 1, 2, Liu Shiyin 2, 3*, Jiang Zongli 4, Xu Junli 5, Wei Junfeng 4, Guo Wanqin 2 5 1School of Resources and Environment, Anqing Normal University, Anqing, Anhui, China 6 2State key Laboratory of Cryospheric Sciences, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou, China 7 3Institute of International Rivers and Eco-Security, Yunnan University, Yunnan, China 8 4Department of Geography, Hunan University of Science and Technology, Xiangtan, China 9 5Department of Surveying and Mapping, Yancheng Teachers University, Yancheng, China 10 Correspondence to LIU Shiyin at [email protected] or WU Kunpeng at [email protected] 11 12 Abstract. Influenced by the Indian monsoon, the Kangri Karpo mountains, in the southeast of the Tibetan 13 Plateau, are the most humid region there, and one of the most important and concentrated regions with 14 maritime (temperate) glaciers. Glacier mass loss in the Kangri Karpo is an important contributor to global 15 mean sea level rise, and changes runoff distribution, increasing the risk of glacial-lake outburst floods 16 (GLOFs). Because of its inaccessibility and high labor costs, information about the Kangri Karpo glaciers is 17 still limited. Using geodetic methods based on digital elevation models (DEM), derived from 1980 topographic 18 maps, from the Shuttle Radar Topography Mission (SRTM) (2000), and from TerraSAR-X/TanDEM-X (2014), 19 this study has determined glacier elevation changes here. Glacier area and length changes between 1980 and 20 2015 were derived from topographical maps and Landsat TM/ETM+/OLI images.
    [Show full text]
  • Eastern Tibet (Kham) 241
    © Lonely Planet Publications 241 EASTERN TIBET (KHAM) E a s t e r n T i b e t ( K h a m ) The eastern region of Tibet, known as Kham, is a land apart. Its climate, geography, flora and fauna all lend it a unique, almost magical atmosphere. The stone villages have more in common with neighbouring Bhutan, the chörtens (stupas) seem lifted from Mustang in Nepal and the forested scenery is more Swiss Alps than high Tibetan plateau. The traditional Tibetan province of Kham incorporates the eastern Tibetan Autonomous Region (TAR), western Si- chuan and northwest Yunnan. This chapter covers only the eastern TAR, where travel permits are required. For information on overland travel through western Sichuan, see p267. Geographically the region varies from the lush subtropical jungle and raging rivers of the southern borderlands to the arid plateau and purple gorges of the east, where the head- waters of some of Asia’s greatest rivers – the Mekong, Salween and Yangzi – tumble off the Tibetan plateau. The glaciated peaks of Namche Barwa (7756m) and the remote gorges of the Yarlung Tsangpo, the world’s deepest, form one of Asia’s last secret corners. Kham gains much of its charm from its people. Khampa cowboys, dressed in sheepskin cloaks and braided hair, cruise the region’s highways on their motorbikes. Kham sometimes feels like the America’s Wild West, with the cowboys and buffalos replaced by Khampas and yaks. There are two main routes through the region, offering a once-in-a-lifetime route in or out of Tibet.
    [Show full text]
  • Spatiotemporal Dynamic Characteristics of Typical Temperate Glaciers in China Wang Shijin1,2*, Che Yanjun1,3 & Wei Yanqiang1
    www.nature.com/scientificreports OPEN Spatiotemporal dynamic characteristics of typical temperate glaciers in China Wang Shijin1,2*, Che Yanjun1,3 & Wei Yanqiang1 China’s temperate glaciers have a relatively warm and humid climate and hydrothermal conditions at low latitudes. Temperate glaciers, however, have larger ablation, higher ice temperatures, relatively fast movement speeds, and a signifcant sliding process at the bottom. As a result, these glaciers are more signifcantly afected by climate change. On the basis of topographic maps, aerial photography, and Landsat OLI images, and combined with existing research results, this paper systematically analyzed the temporal and spatial dynamic characteristics of typical temperate glaciers. The results are as follows: (1) From the 1950s to the 1970s, compared with other types of glaciers, temperate glaciers showed strong retreat and ablation trends in terms of area, length, speed, and mass balance. (2) The reduction rates of glacier areas of Kangri Garpo, Dagu Snow Mountain, Yulong Snow Mountain (YSM), and Meili Snow Mountain (MSM) in China’s temperate glacier areas all exceeded 38%, which was far above the national average of 18% from the 1950s to the 2010s. (3) The recent length retreat rates of Azha Glacier, Kangri Garpo, and Mingyong Glacier, MSM, Hailuogou Glacier (HG), Gongga Snow Mountain (GSM), and Baishui River Glacier No. 1 (BRGN1), YSM were above 22 m/a, which was faster than the retreat rates of other regions. (4) Consistent with glacier retreat, temperate glaciers also had a faster ice fow speed. The ice fow velocities of the BGN1, HG, Parlung River Glaciers No. 4 and 94, and Nyainqêntanglha were, respectively, 6.33–30.78 m/a, 41–205 m/a, 15.1–86.3 m/a, and 7.5–18.4 m/a, which was much faster than the velocity of other types of glaciers.
    [Show full text]
  • Harris 2010 Rangeland Degradation on the Tibetan Plateau.Pdf
    This article appeared in a journal published by Elsevier. The attached copy is furnished to the author for internal non-commercial research and education use, including for instruction at the authors institution and sharing with colleagues. Other uses, including reproduction and distribution, or selling or licensing copies, or posting to personal, institutional or third party websites are prohibited. In most cases authors are permitted to post their version of the article (e.g. in Word or Tex form) to their personal website or institutional repository. Authors requiring further information regarding Elsevier’s archiving and manuscript policies are encouraged to visit: http://www.elsevier.com/copyright Author's personal copy Journal of Arid Environments 74 (2010) 1–12 Contents lists available at ScienceDirect Journal of Arid Environments journal homepage: www.elsevier.com/locate/jaridenv Review Rangeland degradation on the Qinghai-Tibetan plateau: A review of the evidence of its magnitude and causes R.B. Harris* Department of Ecosystem and Conservation Sciences, College of Forestry, University of Montana, Missoula, MT 59812, USA article info abstract Article history: Rangelands of the Qinghai-Tibetan plateau (QTP), although sparsely populated and contributing little to Received 24 November 2008 China’s overall economy, play an important environmental role throughout Asia. They contain high Received in revised form biodiversity values and can also potentially provide China with a source of cultural and geographic 9 June 2009 variety in the future. Chinese government reports paint a gloomy picture, considering vast portions of the Accepted 15 June 2009 QTP degraded and blaming irrational overstocking of livestock as the principal culprit.
    [Show full text]
  • Interannual and Seasonal Variability of Glacier Surface Velocity in the Parlung Zangbo Basin, Tibetan Plateau
    remote sensing Article Interannual and Seasonal Variability of Glacier Surface Velocity in the Parlung Zangbo Basin, Tibetan Plateau Jing Zhang 1,2 , Li Jia 1,*, Massimo Menenti 1,3 and Shaoting Ren 1,2 1 State Key Laboratory of Remote Sensing Science, Aerospace Information Research Institute, Chinese Academy of Sciences, Beijing 100101, China; [email protected] (J.Z.); [email protected] (M.M.); [email protected] (S.R.) 2 University of Chinese Academy of Sciences, Beijing 100049, China 3 Faculty of Civil Engineering and Earth Sciences, Delft University of Technology, 2628 CN Delft, The Netherlands * Correspondence: [email protected]; Tel.: +86-10-6480-7982 Abstract: Monitoring glacier flow is vital to understand the response of mountain glaciers to envi- ronmental forcing in the context of global climate change. Seasonal and interannual variability of surface velocity in the temperate glaciers of the Parlung Zangbo Basin (PZB) has attracted significant attention. Detailed patterns in glacier surface velocity and its seasonal variability in the PZB are still uncertain, however. We utilized Landsat-8 (L8) OLI data to investigate in detail the variability of glacier velocity in the PZB by applying the normalized image cross-correlation method. On the basis of satellite images acquired from 2013 to 2020, we present a map of time-averaged glacier surface velocity and examined four typical glaciers (Yanong, Parlung No.4, Xueyougu, and Azha) in the PZB. Next, we explored the driving factors of surface velocity and of its variability. The results show that the glacier centerline velocity increased slightly in 2017–2020.
    [Show full text]
  • DEBRIS FLOWS: Disasters, Risk, Forecast, Protection
    DEBRIS FLOWS: Disasters, Risk, Forecast, Protection Proceedings of the 5th International Conference Tbilisi, Georgia, 1-5 October 2018 Editors S.S. Chernomorets, G.V. Gavardashvili Publishing House “Universal” Tbilisi 2018 СЕЛЕВЫЕ ПОТОКИ: катастрофы, риск, прогноз, защита Труды 5-й Международной конференции Тбилиси, Грузия, 1-5 октября 2018 г. Ответственные редакторы С.С. Черноморец, Г.В. Гавардашвили Издательство Универсал Тбилиси 2018 ღვარცოფები: კატასტროფები, რისკი, პროგნოზი, დაცვა მე–5 საერთაშორისო კონფერენციის მასალები თბილისი, საქართველო, 1–5 ოქტომბერი, 2018 რედაქტორები ს.ს. ჩერნომორეც, გ.ვ. გავარდაშვილი გამომცემლობა "უნივერსალი" თბილისი 2018 УДК 551.311.8 ББК 26.823 Селевые потоки: катастрофы, риск, прогноз, защита. Труды 5-й Международной конференции. Тбилиси, Грузия, 1-5 октября 2018 г. – Отв. ред. С.С. Черноморец, Г.В. Гавардашвили. – Тбилиси: Универсал, 2018, 671 с. Debris Flows: Disasters, Risk, Forecast, Protection. Proceedings of the 5th International Conference. Tbilisi, Georgia, 1-5 October 2018. – Ed. by S.S. Chernomorets, G.V. Gavardashvili. – Tbilisi: Publishing House “Universal”, 2018, 671 p. ღვარცოფები: კატასტროფები, რისკი, პროგნოზი, დაცვა. მე–5 საერთაშორისო კონფერენციის მასალები. თბილისი, საქართველო, 1–5 ოქტომბერი, 2018. გამომცემლობა "უნივერსალი", თბილისი 2018, 671 გვ. პასუხისმგებელი რედაქტორები ს.ს. ჩერნომორეც, გ.ვ. გავარდაშვილი. Ответственные редакторы С.С. Черноморец, Г.В. Гавардашвили Edited by S.S. Chernomorets, G.V. Gavardashvili Верстка: С.С. Черноморец, К.С. Висхаджиева, Е.А. Савернюк Page-proofs: S.S. Chernomorets, K.S. Viskhadzhieva, E.A. Savernyuk При создании логотипа конференции использован рисунок из книги С.М. Флейшмана «Селевые потоки» (Москва: Географгиз, 1951, с. 51). Conference logo is based on a figure from S.M. Fleishman’s book on Debris Flows (Moscow: Geografgiz, 1951, p.
    [Show full text]
  • Different Glacier Status with Atmospheric Circulations in Tibetan Plateau and Surroundings
    LETTERS PUBLISHED ONLINE: 15 JULY 2012 | DOI: 10.1038/NCLIMATE1580 Different glacier status with atmospheric circulations in Tibetan Plateau and surroundings Tandong Yao1,2*, Lonnie Thompson1,3, Wei Yang1, Wusheng Yu1, Yang Gao1, Xuejun Guo1, Xiaoxin Yang1, Keqin Duan1,2, Huabiao Zhao1, Baiqing Xu1, Jiancheng Pu2, Anxin Lu1,2, Yang Xiang1, Dambaru B. Kattel1 and Daniel Joswiak1 3,000 The Tibetan Plateau and surroundings contain the largest 3,200 1 3,400 number of glaciers outside the polar regions . These glaciers 45° N 3,600 3,800 are at the headwaters of many prominent Asian rivers and 3,800 2 4,000 4,000 are largely experiencing shrinkage , which affects the water 4,400 3,4 4,200 discharge of large rivers such as the Indus . The resulting 40° N 5,6 potential geohazards merit a comprehensive study of glacier 4,800 5,100 5,000 5,200 5,200 5,400 status in the Tibetan Plateau and surroundings. Here we 5,500 5,300 4,600 5,200 5,600 4,700 report on the glacier status over the past 30 years by ° 5,000 35 N 5,700 4,800 4,800 5,90 0 5 5,400 ,8 4,900 investigating the glacial retreat of 82 glaciers, area reduction 0 0 0 0 0 Latitude 5,8 of 7,090 glaciers and mass-balance change of 15 glaciers. 5,60 5,000 Systematic differences in glacier status are apparent from 30° N region to region, with the most intensive shrinkage in the 4,800 5,000 5,000 4,600 Himalayas (excluding the Karakorum) characterized by the ELA (m a.s.l.) 4,400 Westerlies greatest reduction in glacial length and area and the most 25° N Indian monsoon negative mass balance.
    [Show full text]
  • Asian Alpine E-News Issue No.57
    ASIAN ALPINE E-NEWS Issue No 57. December 2019 Contents East Tibet – Autumn 2019 Tamotsu Nakamura Page 2~27 The Himalayan Journal 2019 Himalayan Club Page 28~33 Dharamsara 2017, India HC & T. Nakamura Page 34~43 1 TIBET NOW – UNDERGOING A DRAMATIC CHANGE Return to Kangri Garpo “No Longer Frontier” Journey Autumn 2019 Tamotsu (Tom) Nakamura I have returned to the Tibet Autonomous Region after three years. Qinghai Province was targeted in 2017 and 2018 for expeditions. Dramatic change in Tibet has been taking place far faster than imagined. China is a nation of “Civil Construction”. All Chinese territories covering the borderlands of the west China including Tibet is in a hive of changes and developments. Frontier no longer exists. Railway and highway network 1s expanding. The present Ji administration announcing that the 50,000km railways network will connect the major cities in near future. The right is a highway from Lhasa to Nagchu in parallel with the railway. Nyainqentanglha (from left: P1 7162m, P2, P3 and P4 each 7000m and Qinghai-Tibet Plateau Railway 4500m), P1 first climbed by Tohoku University in 1986. Others climbed too. 1 Holy city, a provincial capital of the Tibet Autonomous region has a population of 750,000 rapidly increased recently and town has been modernized. Department stores, shopping malls are clouded with Tibetan. Right is a picture of lighted up Potala Palace viewed from top floor of a shopping mall. Main objectives were to survey changes in ten years of the Lhagu Glaciers of Kangri Garpo Range. Time flies! A quarter century has lapsed since I first glimpsed this mountain in 1995 Before stating my Odyssey the mountain ranges is summarized below Geography of Kangri Garpo The hardly known mountain range of Kangri Garpo stretches about 280 km from northwest to southeast 28° 30’ - 30° 00’ N and 95° 30’ – 97° 30’ E.
    [Show full text]
  • Potential Danger of Dammed Lakes Induced by the 2017 Ms6.9 Milin Earthquake in the Tsangpo Gorge
    Селевые потоки: катастрофы, риск, прогноз, защита DF18 Debris Flows: Disasters, Risk, Forecast, Protection Potential danger of dammed lakes induced by the 2017 Ms6.9 Milin earthquake in the Tsangpo gorge K. Hu1,2, X. Zhang3, J. Tang1,2, W. Liu1,2 1Key Laboratory of Mountain Hazards and Earth Surface Processes, Chinese Academy of Sciences, Chengdu, China, [email protected] 2Institute of Mountain Hazards and Environment, Chinese Academy of Sciences, Chengdu, China 3University of Chinese Academy of Sciences, Beijing, China A Ms6.9 Milin Earthquake on November 18, 2017 triggered a great deal of new slope failures along the Yarlung Tsangpo gorge. By compared the pre- and post-quake remote sensing images, 529 landslides including rock slides, avalanches, rock falls were identified. The total area of the landslides is 32.42 km2, and the sediment volume caused by the landslides is estimated to be 0.1 km3. The landslides also yield 7 dammed lakes of which three large-scale dammed lakes are also affected by nearby debris-flow events in future. A methodology integrating remote sensing, GIS, numerical simulation and hydrological calculation is developed to predict the potential danger of the dammed lakes once large- scale debris flows increase the height of the dams. Preliminary analysis indicates that the storage capacity of the dammed lakes will increase in two cases of debris-flow magnitudes, but the outburst floods may not result in big impact on downstream human settlements. dammed lake, Milin earthquake, potential danger, risk assessment, Tsangpo gorge, debris flow Потенциальная опасность подпрудных озёр, образовавшихся в ущелье Цангпо вследствие Милиньского землетрясения магнитудой 6.9 К.
    [Show full text]
  • China-India Data Sharing for Early Flood Warning in the Brahmaputra: a Critique
    DECEMBER 2019 ISSUE NO. 328 China-India Data Sharing for Early Flood Warning in the Brahmaputra: A Critique NILANJAN GHOSH JAYANTA BANDYOPADHYAY SAYANANGSHU MODAK ABSTRACT This brief makes an assessment of the data-sharing arrangement between China and India as outlined in the Memorandum of Understanding for sharing hydrological information on the Brahmaputra river system, aimed at facilitating advance warning for floods in India during monsoon. Using hydro-meteorological data, this brief assesses the arrangement and identifies its limitations, primary of which is the wrong choice for the location of measuring stations on the upstream of the Brahmaputra (or the Yarlung Tsangpo in the Tibetan plateau), whose contribution to total flows of the Brahmaputra in India during monsoon is of little significance. In the process, the brief questions the perception that upstream intervention within the basin in the north of the Himalayan crestline can have a negative impact on downstream nations of India and Bangladesh. It calls for a more comprehensive advanced warning system, utilising data from measuring stations in the greater endowed rainfall areas within the south aspect of the Himalaya up to the China-India border, downstream of Mêdog. (This brief is part of ORF’s series, ‘Emerging Themes in Indian Foreign Policy’. Find other research in the series here: https://www.orfonline.org/series/emerging-themes-in-indian-foreign-policy/) Attribution: Nilanjan Ghosh, Jayanta Bandyopadhyay and Sayanangshu Modak, “China-India Data Sharing for Early Flood Warning in the Brahmaputra: A Critique”, ORF Issue Brief No. 328, December 2019, Observer Research Foundation. Observer Research Foundation (ORF) is a public policy think tank that aims to influence the formulation of policies for building a strong and prosperous India.
    [Show full text]