Fluctuations Glaciers

Total Page:16

File Type:pdf, Size:1020Kb

Fluctuations Glaciers FLUCTUATIONS OF GLACIERS 1995–2000 (Vol. VIII) 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) IUGG (CCS) – UNEP – UNESCO 2005 FLUCTUATIONS OF GLACIERS 1995–2000 with addenda from earlier years This publication was made possible by support and funds from the Federation of Astronomical and Geophysical Data Analysis Services (FAGS), the Swiss Academy of Sciences (SCNAT), the United Nations Environment Programme (UNEP), the United Nations Educational, Science and Cultural Organisation (UNESCO), and the University of Zurich (UNIZ) This volume continues the earlier works published under the titles 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 (Vol. VIII) 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 (DEWA and GEO, UNEP), and the International Hydrological Programme (IHP, UNESCO) Compiled for the World Glacier Monitoring Service by Wilfried Haeberli, Michael Zemp, Regula Frauenfelder, Martin Hoelzle and Andreas Kääb Department of Geography University of Zurich Zurich International Union of Geodesy and Geophysics (Commission on Cryospheric Sciences) and United Nations Environment Programme and United Nations Educational, Scientific and Cultural Organisation 2005 Published jointly by the Commission on Cryospheric Sciences of the International Union of Geodesy and Geophysics and the United Nations Environment Programme P.O. Box 30552, Nairobi, Kenya and the United Nations Educational, Scientific and Cultural Organisation 7 Place de Fontenoy, 75700 Paris, France Printed by FOTOROTAR Egg/ZH, Switzerland The designations employed and the presentation of the material in this publication do not imply the expression of any opinion what- soever 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. For bibliographic and reference purposes this publication should be referred to as: IUGG (CCS) – UNEP – UNESCO (2005). Fluctuations of Glaciers 1995–2000, Volume VIII. World Glacier Monitoring Service, Zurich. IUGG UNEP UNESCO PREFACE UNEP Fluctuations of glaciers have been reported and documented in an internationally coordi- nated way for more than a century. They have now become a key indication of global climate and environmental change. The possibility to observe the often dramatic changes in the geometry of perennial surface ice within a lifetime period, combined with the easily understandable principle of ice melting under the influence of high air tempera- tures, makes the retreat of glacier tongues and ice margins a unique climate change demonstration object for the public at large. In fact, future generations will be able to judge what climate scenario will have taken place by looking at the form, size and sheer existence of glaciers around the world. Modern worldwide glacier monitoring as coordinated by the World Glacier Monitoring Service (WGMS) with its Global Terrestrial Network for Glaciers (GTN-G) as part of the Global Climate Observing System/Global Terrestrial Observing System (GCOS/GTOS) aims at the quantification of the changes in terrestrial glaciers. The monitoring system uses a multilevel strategy, which combines a) in-situ measurements for process under- standing and model calibration with b) remote sensing and geo-informatics for large/ representative sampling and c) numerical simulations for extrapolation of measured data in space and time. Through WGMS, scientifically-sound data and information on the state and trends of glaciers are provided, required as a basis for global environmental assessments in support of decision-making processes. As such, this effort also contributes to the strengthening of the scientific basis of UNEP’s assessment activities, requiring that sound assessments must be based on reliable data. As a key component, the Global Environment Outlook reporting process greatly benefits from the continued data collection on changes in glacier mass and volume. UNEP very much welcomes the possibility to use such infor- mation in its reporting activities in support of improved information availability and better informed decision-making. The present volume “Fluctuations of Glaciers 1995–2000” continues the series of reports about in-situ measurements of glacier fluctuations and completes the reports for the 20th century. It mainly presents data measured in the field, but also contains a number of high-precision maps from various regions of the earth. In addition, summary comments and references can be found about results from numerical modelling and satellite-based glacier inventory work. The latter is now being strengthened – in close collaboration with WGMS and GTN-G – by the international “Global Land Ice Measurement from Space” (GLIMS) project led by the US Geological Survey in Flagstaff, Arizona, USA. In view of recent scientific insights and modern technological means, the development of new formats for data collection and presentation is one of the primary challenges for the first years of our century. Marion Cheatle Officer-in-Charge Division of Early Warning and Assessment, UNEP I II PREFACE UNESCO Glaciers contribute significantly to the human needs for good quality water. They are also highly sensitive indicators of global climate change and fresh water reservoirs. Our knowledge of the state of glaciers worldwide remains very incomplete despite considerable publicity to accelerating melting rates in various global climate change scenarios. However, increased melting rates will have disastrous consequences to flood- ing and sea level rise as glaciers react in a complex manner to climatic variations. Their advances leave behind landscape markers as moraines, which serve to help us reconstruct past glacial conditions and past climate. As water reservoirs they are essential to region- al water supply. The understanding of their changes with changing climate is vital for future water policy and water management. To understand and interpret these different aspects it is necessary to study the mass exchange and growth/shrinkage of glaciers. Despite such important contributions there are many parts of the world where either too few glaciers are monitored or where glaciers are not monitored at all. In the last few years UNESCO has initiated a programme of mass balance measurements in both the Hindu Kush Himalayas and the Andes to improve our knowledge of the glaciers. The Inter- national Hydrological Programme (IHP) of UNESCO, now in its 6th phase aims to improve our knowledge of the complex scientific processes that govern the interactions within the water cycle. Under the theme devoted to Mountains, activities have been promoted in several regions of the world. Obviously the complex nature of glaciers and their inaccessibility make it a necessity that the global scientific community cooperate in planning and organising activities. The contribution of the WGMS is greatly recognised and appreciated. It is only through the efforts of such scientific bodies that we can mobilise global efforts to improve our scientific knowledge. UNESCO is pleased to support this publication. Wilfried Haeberli and his team are to be congratulated for accomplishing this task. This volume will be a major contribution towards providing information for interpreting the health of glaciers for the period 1995–2000. Lalji Mandalia Programme Specialist in Water Sciences International Hydrological Programme, UNESCO III IV FOREWORD The Intergovernmental Panel on Climate Change (IPCC) has recently pointed out that glaciers and ice caps are one of the key indicators of ongoing climatic change. Glaciers and ice caps are components of the Earth’s Cryosphere and the continual wasting of these ice bodies contributes to global sea level rise. Glaciers are also an integral part of the hydrological cycle in mountainous regions and the discharge from higher rates of melt water production can lead to an increase in the occurrence of natural hazards in glacier-fed basins. Knowledge of the changes in the balance of glacier ice is thus of prime importance in modelling the interactive processes between climate and the Earth’s global dynamic systems, and in the prediction of water availability in more specific re- gions of the Earth’s surface. Fluctuations of glaciers and ice caps in cold mountain areas have been systematically observed for more than a century in various parts of the world. Change in glacier extent is a strongly enhanced and easily measured parameter, which provides an indirect, filtered signal of climate
Recommended publications
  • PROGETTO ANTARTIDE Rapporto Sulla Campagna Antartica Estate Australe 1996
    PROGRAMMA NAZIONALE DI RICERCHE IN ANTARTIDE Rapporto sulla Campagna Antartica Estate Australe 1996 - 97 Dodicesima Spedizione PROGETTO ANTARTIDE ANT 97/02 PROGRAMMA NAZIONALE DI RICERCHE IN ANTARTIDE Rapporto sulla Campagna Antartica Estate Australe 1996 - 97 Dodicesima Spedizione A cura di J. Mϋller, T. Pugliatti, M.C. Ramorino, C.A. Ricci PROGETTO ANTARTIDE ENEA - Progetto Antartide Via Anguillarese,301 c.p.2400,00100 Roma A.D. Tel.: 06-30484816,Fax:06-30484893,E-mail:[email protected] I N D I C E Premessa SETTORE 1 - EVOLUZIONE GEOLOGICA DEL CONTINENTE ANTARTICO E DELL'OCEANO MERIDIONALE Area Tematica 1a Evoluzione Geologica del Continente Antartico Progetto 1a.1 Evoluzione del cratone est-antartico e del margine paleo-pacifico del Gondwana.3 Progetto 1a.2 Evoluzione mesozoica e cenozoica del Mare di Ross ed aree adiacenti..............11 Progetto 1a.3 Magmatismo Cenozoico del margine occidentale antartico..................................17 Progetto 1a.4 Cartografia geologica, geomorfologica e geofisica ...............................................18 Area Tematica 1b-c Margini della Placca Antartica e Bacini Periantartici Progetto 1b-c.1 Strutture crostali ed evoluzione cenozoica della Penisola Antartica e del margine coniugato cileno ......................................................................................25 Progetto 1b-c.2 Indagini geofisiche sul sistema deposizionale glaciale al margine pacifico della Penisola Antartica.........................................................................................42
    [Show full text]
  • The Commonwealth Trans-Antarctic Expedition 1955-1958
    THE COMMONWEALTH TRANS-ANTARCTIC EXPEDITION 1955-1958 HOW THE CROSSING OF ANTARCTICA MOVED NEW ZEALAND TO RECOGNISE ITS ANTARCTIC HERITAGE AND TAKE AN EQUAL PLACE AMONG ANTARCTIC NATIONS A thesis submitted in fulfilment of the requirements for the Degree PhD - Doctor of Philosophy (Antarctic Studies – History) University of Canterbury Gateway Antarctica Stephen Walter Hicks 2015 Statement of Authority & Originality I certify that the work in this thesis has not been previously submitted for a degree nor has it been submitted as part of requirements for a degree except as fully acknowledged within the text. I also certify that the thesis has been written by me. Any help that I have received in my research and the preparation of the thesis itself has been acknowledged. In addition, I certify that all information sources and literature used are indicated in the thesis. Elements of material covered in Chapter 4 and 5 have been published in: Electronic version: Stephen Hicks, Bryan Storey, Philippa Mein-Smith, ‘Against All Odds: the birth of the Commonwealth Trans-Antarctic Expedition, 1955-1958’, Polar Record, Volume00,(0), pp.1-12, (2011), Cambridge University Press, 2011. Print version: Stephen Hicks, Bryan Storey, Philippa Mein-Smith, ‘Against All Odds: the birth of the Commonwealth Trans-Antarctic Expedition, 1955-1958’, Polar Record, Volume 49, Issue 1, pp. 50-61, Cambridge University Press, 2013 Signature of Candidate ________________________________ Table of Contents Foreword ..................................................................................................................................
    [Show full text]
  • Late Pleistocene Interactions of East and West Antarctic Ice-Flow Regim.Es: Evidence From
    J oumal oJ Glaciology, r·ol. 42, S o. 142, 1996 Late Pleistocene interactions of East and West Antarctic ice-flow regim.es: evidence from. the McMurdo Ice Shelf THO}'IAS B . KELLOGG, TERRY H UG HES AND D .\VJD!\ E. KELLOGG Depa rtmen t oJ Geo logical Sciences alld Institute for QJlatemm) Studies, UI/ iversilj' oJ ,\Jail/ e, Orono , "faine 04469. [j.S. A. ABSTRACT. \Ve prese nt new interpreta ti ons of d eglacia tion in M cMurdo Sound and the wes tern R oss Sea, with o bservati onall y based reconstructi ons of interacti ons between Eas t a nd \Ves t Antarcti c ice a t the las t glacial maximum (LG YI ), 16 000, 12 000, 8000 a nd 4000 BP. At the LG M , East Anta rctic ice fr om Muloek Glacier spli t; one bra nch turned wes tward south of R oss Tsland b ut the other bra nch rounded R oss Island before fl owing south"'est in to lVf cMurdo Sound. This fl ow regime, constrained b y a n ice sa ddle north of R n. s Isla nd, is consisten t wi th the reconstruc ti on of Stuiyer a nd others (198I a ) . After the LG lVI. , grounding-line retreat was m ost ra pid in areas \~ ' i th greates t wa ter d epth, es pecially a long th e Vic toria Land coast. By 12 000 BP , the ice-flow regime in :'.1cMurdo Sound c ha nged to through-flowing l\1ulock G lacier ice, with lesse r contributions from K oettlitz, Blue a nd F crra r Glaciers, because the formcr ice saddle north of R oss Isla nd was repl aced by a d om e.
    [Show full text]
  • Rapporto Sulla Campagna Antartica Estate Australe 1998-99 PROGETTO ANTARTIDE
    PROGRAMMA NAZIONALE DI RICERCHE IN ANTARTIDE Rapporto sulla Campagna Antartica Estate Australe 1998-99 Quattordicesima Spedizione PROGETTO ANTARTIDE ANT 99/04 PROGRAMMA NAZIONALE DI RICERCHE IN ANTARTIDE Rapporto sulla Campagna Antartica Estate Australe 1998-99 Quattordicesima Spedizione A cura di Tiziana Pugliatti e M. Chiara Ramorino PROGETTO ANTARTIDE ENEA - Progetto Antartide Via Anguillarese, 301 c.p. 2400, 00100 Roma A.D. Tel.: 0630484816, Fax: 0630484893, E-mail:[email protected] Sito WEB: http://www2.pnra.it Indice I N D I C E PREMESSA........................................................................................................................................................v ATTIVITA’ A BAIA TERRA NOVA E PRESSO ALTRE BASI SETTORE 1 - EVOLUZIONE GEOLOGICA DEL CONTINENTE ANTARTICO E DELL'OCEANO MERIDIONALE Area Tematica 1a Evoluzione Geologica del Continente Antartico Progetto 1a.2 Evoluzione mesozoica e cenozoica del Mare di Ross e aree adiacenti..................3 Progetto 1a.4 Cartografia geologica, geomorfologica e geofisica .................................................3 Progetto 1a.5 Cape Roberts ..........................................................................................................6 SETTORE 2 - GLOBAL CHANGE Sottosettore 2a - Glaciologia e Paleoclima Area Tematica 2a.1 Glaciologia e Paleoclima Progetto 2a.1.1 Bilancio di massa, monitoraggio e studio paleoclimatico della calotta antartica orientale - settore pacifico ......................................................................11
    [Show full text]
  • S41467-018-05625-3.Pdf
    ARTICLE DOI: 10.1038/s41467-018-05625-3 OPEN Holocene reconfiguration and readvance of the East Antarctic Ice Sheet Sarah L. Greenwood 1, Lauren M. Simkins2,3, Anna Ruth W. Halberstadt 2,4, Lindsay O. Prothro2 & John B. Anderson2 How ice sheets respond to changes in their grounding line is important in understanding ice sheet vulnerability to climate and ocean changes. The interplay between regional grounding 1234567890():,; line change and potentially diverse ice flow behaviour of contributing catchments is relevant to an ice sheet’s stability and resilience to change. At the last glacial maximum, marine-based ice streams in the western Ross Sea were fed by numerous catchments draining the East Antarctic Ice Sheet. Here we present geomorphological and acoustic stratigraphic evidence of ice sheet reorganisation in the South Victoria Land (SVL) sector of the western Ross Sea. The opening of a grounding line embayment unzipped ice sheet sub-sectors, enabled an ice flow direction change and triggered enhanced flow from SVL outlet glaciers. These relatively small catchments behaved independently of regional grounding line retreat, instead driving an ice sheet readvance that delivered a significant volume of ice to the ocean and was sustained for centuries. 1 Department of Geological Sciences, Stockholm University, Stockholm 10691, Sweden. 2 Department of Earth, Environmental and Planetary Sciences, Rice University, Houston, TX 77005, USA. 3 Department of Environmental Sciences, University of Virginia, Charlottesville, VA 22904, USA. 4 Department
    [Show full text]
  • Washington Geology, V, 21, No. 2, July 1993
    WASHINGTON GEOLOGY Washington Department of Natural Resources, Division of Geology and Earth Resources Vol. 21, No. 2, July 1993 , Mount Baker volcano from the northeast. Bagley Lakes, in the foreground, are on a Pleistocene recessional moraine that is now the parking lot for Mount Baker Ski Area. Just below Sherman Peak, an erosional remnant on the left skyline, is Boulder Glacier. Park and Rainbow Glaciers share the area below the main summit (Grant Peak, 10,778 ft) . Boulder, Park, and Rainbow Glaciers drain into Baker Lake, which is out of the photo on the left. Mazama Glacier forms under the ridge that extends to Hadley Peak on the right. (See related article, p. 3 and Fig. 2, p. 5.) Table Mountain, the flat area just above and to the right of center, is a truncated lava flow. Lincoln Peak is just visible over the right shoulder of Mount Baker. Photo taken in 1964. In This Issue: Current behavior of glaciers in the North Cascades and its effect on regional water supplies, p. 3; Radon potential of Washington, p. 11; Washington areas selected for water quality assessment, p. 14; The changing role of cartogra­ phy in OGER-Plugging into the Geographic Information System, p. 15; Additions to the library, p. 16. Revised State Surface Minin!Jf Act-1993 by Raymond Lasmanls WASHINGTON The 1993 regular session of the 53rd Le:gislature passed a major revision of the surface mine reclamation act as En­ GEOLOGY grossed Second Substitute Senate Bill No. 5502. The new law takes effect on July 1, 1993. Both environmental groups and surface miners testified in favor of the act.
    [Show full text]
  • ICE FLOW VELOCITY MAPPING in EAST ANTARCTICA USING HISTORICAL IMAGES from 1960S to 1980S: RECENT PROGRESS
    The International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences, Volume XLIII-B3-2021 XXIV ISPRS Congress (2021 edition) ICE FLOW VELOCITY MAPPING IN EAST ANTARCTICA USING HISTORICAL IMAGES FROM 1960s TO 1980s: RECENT PROGRESS S. Luo 1,2, Y. Cheng 1,2, Z. Li 1,2, Y. Wang 1,2, K. Wang 1,2, X. Wang 1,2, G. Qiao 1,2, W. Ye 1,2, Y. Li 1,2, M. Xia 1,2, X. Yuan 1,2, Y. Tian 1,2, X. Tong 1,2, R. Li 1,2* 1Center for Spatial Information Science and Sustainable Development Applications, Tongji University, 1239 Siping Road, Shanghai, China - (shulei, chengyuan_1994, tjwkl, wxfjj620, qiaogang, menglianxia, 1996yuanxiaohan, tianyixiang, xhtong, rli) @tongji.edu.cn, (zhenli_0324, yanjunli_1995) @outlook.com, [email protected], [email protected] 2 College of Surveying and Geo-Informatics, Tongji University, 1239 Siping Road, Shanghai, China Commission TCIII, WG III/9 KEY WORDS: East Antarctica, Ice Flow, Historical Image, Velocity Validation, Ice Flux, Mass Balance ABSTRACT: Recent research indicates that the estimated elevation changes and associated mass balance in East Antarctica are of some degree of uncertainty; a light accumulation has occurred in its vast inland regions, while mass loss in Wilkes Land appears significant. It is necessary to study the mass change trend in the context of a long period of the East Antarctic Ice Sheet (EAIS). The input-output method based on surface ice flow velocity and ice thickness is one of the most important ways to estimate the mass balance, which can provide longer-term knowledge of mass balance because of the availability of the early satellites in 1960s.
    [Show full text]
  • Drainage Structures and Transit-Time Distributions in Conduit-Dominated
    Drainage structures and transit-time distributions in conduit-dominated and fissured karst aquifer systems Zur Erlangung des akademischen Grades einer DOKTORIN DER NATURWISSENSCHAFTEN von der Fakultät für Bauingenieur-, Geo- und Umweltwissenschaften des Karlsruher Instituts für Technologie (KIT) genehmigte DISSERTATION von Dipl.-Geol. Ute Lauber aus Dachau Tag der mündlichen Prüfung: 21.11.2014 Referent: Prof. Dr. Nico Goldscheider Korreferent: Prof. Dr. Tim Bechtel Karlsruhe 2014 Abstract Abstract Abstract Karst aquifers are widely distributed across the world and are important groundwater resources. Solutionally-enlarged conduits embedded in fissured rock matrix result in a highly heterogene- ous underground drainage pattern that makes karst aquifers difficult to characterize. To ensure sustainable protection and management of karst water resources, hydrogeologic knowledge of karst systems is required. However, the quantitative characterization of groundwater flow in karst systems remains a major challenge. Specific investigating techniques and approaches are needed to account for the complexity of drainage. This thesis emphasizes the identification of drainage structures and the quantification of related transit-time distributions and hydraulic pa- rameters. To account for the strong heterogeneities of different types of catchment areas, three diverse karst aquifer systems are investigated: a conduit-dominated karst system, a fissured karst system and an aquifer system that comprises a karst and a porous-media (alluvial/rockfall) aquifer. For a detailed hydrogeologic assessment of the different catchment areas, adapted methods applied include a combination of artificial tracer tests, natural tracer analysis, and dis- charge analysis. The first two parts of this thesis describe a conduit-dominated karst system, the catchment area of the Blautopf (Swabian Alb, Germany).
    [Show full text]
  • Scientific Information 2001/2002 Annual New Zealand
    Scientific Information 2001/2002 Annual New Zealand Forward Plans LGP The Latitudinal Gradient Project (LGP) is aimed at increasing the understanding of the coastal marine, freshwater and terrestrial ecosystems that exist along the Victoria Land coastline in the Ross Sea region, and describing potential environmental variability that may occur in the future. Antarctica New Zealand is providing the logistical capabilities for research camps to be located at specific sites along the Victoria Land coast. Thus, the opportunity to work at particular locations in collaboration with other scientists from various disciplines and National Antarctic Programmes is provided. LGP has been formally incorporated into the SCAR programme RiSCC (Regional Sensitivity to Climate Change). Certain data collected within the LGP will be housed and made available within the RiSCC database framework. Details on how the data will be shared and the timing of when the data will be made available have yet to be decided. It is intended that publications arising from the LGP will be published in a special issue of a refereed journal. Research under the LGP will be both ship-based and land-based. At present, ship-based research, funded under the Ministry of Fisheries’ BioRoss programme and the Italian Antarctic Programme, has been scheduled for January to March 2004 with a research voyage planned using two vessels aimed at supporting near-shore and deep-water marine research. The vessels dedicated to this research are NIWA’s RV Tangaroa, and the Italian Antarctic Programme’s RV Italica. Further information about the ship-based research can be found in the BioRoss research plan and in the BioRoss call for statements of interest.
    [Show full text]
  • Report November 1996
    International Council of Scientific Unions No13 report November 1996 Contents SCAR Group of Specialists on Global Change and theAntarctic (GLOCHANT) Report of bipolar meeting of GLOCHANT / IGBP-PAGES Task Group 2 on Palaeoenvironments from Ice Cores (PICE), 1995 1 Report of GLOCHANTTask Group 3 on Ice Sheet Mass Balance and Sea-Level (ISMASS), 1995 6 Report of GLOCHANT IV meeting, 1996 16 GLOCHANT IV Appendices 27 Published by the SCIENTIFIC COMMITTEE ON ANTARCTIC RESEARCH at the Scott Polar Research Institute, Cambridge, United Kingdom INTERNATIONAL COUNCIL OF SCIENTIFIC UNIONS SCIENTIFIC COMMITfEE ON ANTARCTIC RESEARCH SCAR Report No 13, November 1996 Contents SCAR Group of Specialists on Global Change and theAntarctic (GLOCHANT) Report of bipolar meeting of GLOCHANT / IGBP-PAGES Task Group 2 on Palaeoenvironments from Ice Cores (PICE), 1995 1 Report of GLOCHANT Task Group 3 on Ice Sheet Mass Balance and Sea-Level (ISMASS), 1995 6 Report of GLOCHANT IV meeting, 1996 16 GLOCHANT IV Appendices 27 Published by the SCIENTIFIC COMMITfEE ON ANT ARCTIC RESEARCH at the Scott Polar Research Institute, Cambridge, United Kingdom SCAR Group of Specialists on Global Change and the Antarctic (GLOCHANT) Report of the 1995 bipolar meeting of the GLOCHANT I IGBP-PAGES Task Group 2 on Palaeoenvironments from Ice Cores. (PICE) Boston, Massachusetts, USA, 15-16 September; 1995 Members ofthe PICE Group present Dr. D. Raynaud (Chainnan, France), Dr. D. Peel (Secretary, U.K.}, Dr. J. White (U.S.A.}, Mr. V. Morgan (Australia), Dr. V. Lipenkov (Russia), Dr. J. Jouzel (France), Dr. H. Shoji (Japan, proxy for Prof. 0. Watanabe). Apologies: Prof. 0.
    [Show full text]
  • 1 Compiled by Mike Wing New Zealand Antarctic Society (Inc
    ANTARCTIC 1 Compiled by Mike Wing US bulldozer, 1: 202, 340, 12: 54, New Zealand Antarctic Society (Inc) ACECRC, see Antarctic Climate & Ecosystems Cooperation Research Centre Volume 1-26: June 2009 Acevedo, Capitan. A.O. 4: 36, Ackerman, Piers, 21: 16, Vessel names are shown viz: “Aconcagua” Ackroyd, Lieut. F: 1: 307, All book reviews are shown under ‘Book Reviews’ Ackroyd-Kelly, J. W., 10: 279, All Universities are shown under ‘Universities’ “Aconcagua”, 1: 261 Aircraft types appear under Aircraft. Acta Palaeontolegica Polonica, 25: 64, Obituaries & Tributes are shown under 'Obituaries', ACZP, see Antarctic Convergence Zone Project see also individual names. Adam, Dieter, 13: 6, 287, Adam, Dr James, 1: 227, 241, 280, Vol 20 page numbers 27-36 are shared by both Adams, Chris, 11: 198, 274, 12: 331, 396, double issues 1&2 and 3&4. Those in double issue Adams, Dieter, 12: 294, 3&4 are marked accordingly. Adams, Ian, 1: 71, 99, 167, 229, 263, 330, 2: 23, Adams, J.B., 26: 22, Adams, Lt. R.D., 2: 127, 159, 208, Adams, Sir Jameson Obituary, 3: 76, A Adams Cape, 1: 248, Adams Glacier, 2: 425, Adams Island, 4: 201, 302, “101 In Sung”, f/v, 21: 36, Adamson, R.G. 3: 474-45, 4: 6, 62, 116, 166, 224, ‘A’ Hut restorations, 12: 175, 220, 25: 16, 277, Aaron, Edwin, 11: 55, Adare, Cape - see Hallett Station Abbiss, Jane, 20: 8, Addison, Vicki, 24: 33, Aboa Station, (Finland) 12: 227, 13: 114, Adelaide Island (Base T), see Bases F.I.D.S. Abbott, Dr N.D.
    [Show full text]
  • Recent Extension Driven by Mantle Upwelling Beneath the Admiralty Mountains (East Antarctica)
    TECTONICS, VOL. 27, XXXXXX, doi:10.1029/2007TC002197, 2008 Click Here for Full Article 2 Recent extension driven by mantle upwelling beneath the 3 Admiralty Mountains (East Antarctica) 1 1 2 3 4 Claudio Faccenna, Federico Rossetti, Thorsten W. Becker, Stefania Danesi, 3 5 and Andrea Morelli 6 Received 10 August 2007; revised 4 April 2008; accepted 17 June 2008; published XX Month 2008. 8 [1] Northern Victoria Land is located at the boundary structed by subsidence and uplift history, is commonly 47 9 between an extended, presumably hot, region (West considered polyphased, involving an early Cretaceous phase 48 10 Antarctic Rift System) and the thick, possibly cold, linked to the Gondwana breakup followed by a major 49 11 East Antarctic craton. The style and timing of Tertiary Cenozoic one [e.g., Cooper et al., 1997; Behrendt et al., 50 12 deformation along with relationships with the 1991; Tessensohn and Wo¨rner, 1991; Lawver and Gahagan, 51 1994; Davey and Brancolini, 1995; Salvini et al., 1997; 52 13 magmatic activity are still unclear, and contrasting Behrendt, 1999; Cande et al., 2000; Mukasa and Dalziel, 53 14 models have been proposed. We performed structural 2000; Cande and Stock, 2004]. 54 15 and morphotectonic analyses at the NE termination of [3] There are two outstanding questions concerning the 55 16 northern Victoria Land in the Admiralty Mountains kinematic and tectonic evolution of the Cenozoic tectonic 56 17 area, where the relationship between topography, episode in the WARS. First, the pattern of deformation 57 18 tectonics, and magmatism is expected to be well changes abruptly moving from Victoria Land to the western 58 19 pronounced.
    [Show full text]