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[Lil 72111 Chi "Liili-S -Duvl R^Uiihj]I^ Im^'Isdtirss • Business^Ofiles • Advertising •Magazine A
The Journal of the New Zealand Antarctic Society Vol 17, No. 4, 2000 [lil 72111 chi "Liili-S -duVl r^uiiHj]i^ iM^'isDTirss • Business^ofiles • Advertising •Magazine a . " ^ newsletter publishing • Corporate communications 'V- ■• • Marketingi.. cormtownications • Media relations • Event management x • Financial PR, annual reports P 0 Box 2369 Tel ++64-3-3650344 Christchurch Fax ++64-3-3654255 New Zealand [email protected] ANTARCTIC CONTENTS Shackleton's Voyage Re-enacted Successful season at Cape Roberts Traverses by Women Surfing Antarctica Lone Rower's Attempt Our cover illustration of Shackleton's Hut is courtesy of © Colin Monteath of Hedgehog House and is sourced from his magnificent book Hunting Meteorites 'Antarctica: Beyond the Southern Ocean', published 1996 David Bateman Ltd, reprinted 1997,160pp. Titanic Icebergs Price NZ $50. Volume 17, No. 4, 2000 Looking for 'White Gold' Issue No. 171 ANTARCTIC is published quarterly by the New Tourism Zealand Antarctic Society Inc., ISSN 0003-5327. Editor Vicki Hyde. Please address all editorial enquiries to Warren Winfly 2000 Head, Publisher, 'Antarctic', PO Box 2369, Christchurch, or Tel 03 365 0344, facsimile 03 365 4255, email: [email protected] Riding the Hagglund Printed by Herald Communications, 52 Bank Street, Timaru, New Zealand. The 'Vanda Lake' Boys The Riddle of the Antarctic Peninsula Shackleton's Endurance Exhibition REVIEWS Book review - 'The Endurance' by Caroline Alexander TRIBUTE Harding Dunnett tribute Volume 17, No. 4, 2000 Antarctic NEWS SHACKLETON'S EPIC BOAT VOYAGE RE ENACTED Four men have successfully re-en Television network ROUTE OF THE JOURNEY acted Shackleton's epic 1916 open film crew aboard mak Siidgeorgien boat journey from Elephant Island to ing a documentary of South Georgia, including his climb the re-enactment. -
The Recent Nature of the Siberian Pole of Cold*
T H E RECENT NATU R E OF T H E S IB E RI AN PO LE O F CO L D* By 1. P. GERASIMOV (I nstitute of Geography, Academy of Sciences of the U.S.S.R., Moscow) ABSTRACT. The Siberian pole of cold is situated in the extreme north-east of Eurasia (in the region of the Cherskiy mountain system, in the upper parts of the basins of the Yana, Indigirka and K o lyma Rivers). Particularl y low air and soil temperatures have been observed in the intermontane areas. Among these localities is the famous O ymyakon, where the lowest minimum temperature in the Northern Hemisphere has been recorded. In the climate of this area extreme aridity, connected with the intracontinental position of thc territory, is combined with intense cold. In the two highest massifs (Ulakhan-Chistayand Suntar-Khayata) small centres of recent glacierization (chiefly kars) are developed ; there are also distinct traces of a more extensive older mountain g laciation. In the intermontane areas and on the principal level of the dissected hilly peneplain positive indications of a former glaciation are absent. However, the recent cryogenic phenomena r epresented by fossil ice, permafrost, taryns, as well as thermokarstic, solifluction and congelation features, are very abundant and diverse. The widespread development of all th ese features gives this territory a periglacial aspect, and also provides the possibility of using the study of many recent phenomena for palaeogeographical purposes. From this point of view, the processes leading to the formation of loess deposits (cryogenic facies) and the formation of structural and thixotropic soils are of particular interest. -
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 .................................................................................................................................. -
USCGC Glacier (WAGB-4)
NATIONAL REGISTER ELIGIBILITY ASSESSMENT VESSEL: USS Glacier (AGB-4) USCGC Glacier (WAGB-4) USCGC Glacier underway circa 1966-1972. Photo courtesy of U.S. Coast Guard. The icebreaker Glacier. Vessel History The former U.S. Coast Guard Cutter Glacier is an oceangoing icebreaker that was originally designed and constructed for the U.S. Navy in the mid-1950s. In 1966, Glacier was transferred to the Coast Guard. Ingalls Shipbuilding in Pascagoula, Mississippi began constructing the icebreaker in August 1953 and delivered the ship to the U.S. Navy in May 1955. It was named for Glacier Bay, Alaska, and was the fourth ship to carry this name. After its initial shakedown cruise, Glacier sailed from its homeport of Boston, Massachusetts as Admiral Richard E. Byrd’s flagship bound for the Antarctic as part of Operation Deep Freeze I1 in late 1955. It reached the 1 Operation Deep Freeze I was the codename for a series of scientific expeditions to Antarctica in 1955-56. The impetus behind the expeditions was the International Geophysical Year 1957-58. IGY was a collaborative effort of 40 nations to study the North and South Poles and points in between. Their goal was to advance knowledge of Antarctic hydrography and weather systems, glacial movements, and marine life. The U.S. Navy was charged with supporting the U.S. scientists for their portion of the IGY studies. 2 Ross Ice Pack in December where it smashed through thick ice “carving” out a harbor in Kainan Bay for ships delivering materials, supplies, and labor for the construction of Little America V.2 After clearing a channel and leading a group of ships to Kainan Bay, Glacier headed toward the Ross Ice Shelf to assist in the construction of a naval air station at McMurdo Sound. -
Kinematic First-Order Calving Law Implies Potential for Abrupt Ice-Shelf Retreat
Manuscript prepared for The Cryosphere with version 3.2 of the LATEX class copernicus.cls. Date: 30 January 2012 Kinematic First-Order Calving Law implies Potential for Abrupt Ice-Shelf Retreat Anders Levermann1,2, Torsten Albrecht1,2, Ricarda Winkelmann1,2, Maria A. Martin1,2, Marianne Haseloff1,3, and Ian Joughin4 1Earth System Analysis, Potsdam Institute for Climate Impact Research, Potsdam, Germany 2Institute of Physics, Potsdam University, Potsdam, Germany 3University of British Columbia, Vancouver, Canada 4Polar Science Center, APL, University of Washington, Seattle, Washington, USA Correspondence to: Anders Levermann ([email protected]) Abstract. Recently observed large-scale disintegration of Antarctic ice shelves has moved their fronts closer towards grounded ice. In response, ice-sheet discharge into the ocean has accelerated, contributing to global sea-level rise and emphasizing the importance of calving-front dynamics. The position of the ice front strongly influences the stress field within the entire sheet-shelf-system 5 and thereby the mass flow across the grounding line. While theories for an advance of the ice- front are readily available, no general rule exists for its retreat, making it difficult to incorporate the retreat in predictive models. Here we extract the first-order large-scale kinematic contribution to calving which is consistent with large-scale observation. We emphasize that the proposed equation does not constitute a comprehensive calving law but represents the first order kinematic contribution 10 which can and should be complemented by higher order contributions as well as the influence of potentially heterogeneous material properties of the ice. When applied as a calving law, the equation naturally incorporates the stabilizing effect of pinning points and inhibits ice shelf growth outside of embayments. -
Management Plan for Antarctic Specially Protected Area No. 116 NEW COLLEGE VALLEY, CAUGHLEY BEACH, CAPE BIRD, ROSS ISLAND
Management Plan For Antarctic Specially Protected Area No. 116 NEW COLLEGE VALLEY, CAUGHLEY BEACH, CAPE BIRD, ROSS ISLAND 1. Description of values to be protected In 1985, two areas at Cape Bird, Ross Island were designated as SSSI No. 10, Caughley Beach (Recommendation XIII-8 (1985)) and SPA No. 20, New College Valley (Recommendation XIII-12 (1985)), following proposals by New Zealand that these areas should be protected because they contained some of the richest stands of moss and associated microflora and fauna in the Ross Sea region of Antarctica. This is the only area on Ross Island where protection is specifically given to plant assemblages and associated ecosystems. At that time, SPA No. 20 was enclosed within SSSI No. 10, in order to provide more stringent access conditions to that part of the Area. In 2000, SSSI No. 10 was incorporated with SPA No. 20 by Measure 1 (2000), with the former area covered by SPA No. 20 becoming a Restricted Zone within the revised SPA No. 20. The boundaries of the Area were revised from the boundaries in the original recommendations, in view of improved mapping and to follow more closely the ridges enclosing the catchment of New College Valley. Caughley Beach itself was adjacent to, but never a part of, the original Area, and for this reason the entire Area was renamed as New College Valley, which was within both of the original sites. The Area was redesignated by Decision 1 (2002) as Antarctic Specially Protected Area (ASPA) No. 116 and a revised Management Plan was adopted through Measure 1 (2006). -
The Antarctic Treaty
The Antarctic Treaty Measures adopted at the Thirty-ninth Consultative Meeting held at Santiago, Chile 23 May – 1 June 2016 Presented to Parliament by the Secretary of State for Foreign and Commonwealth Affairs by Command of Her Majesty November 2017 Cm 9542 © Crown copyright 2017 This publication is licensed under the terms of the Open Government Licence v3.0 except where otherwise stated. To view this licence, visit nationalarchives.gov.uk/doc/open-government-licence/version/3 Where we have identified any third party copyright information you will need to obtain permission from the copyright holders concerned. This publication is available at www.gov.uk/government/publications Any enquiries regarding this publication should be sent to us at Treaty Section, Foreign and Commonwealth Office, King Charles Street, London, SW1A 2AH ISBN 978-1-5286-0126-9 CCS1117441642 11/17 Printed on paper containing 75% recycled fibre content minimum Printed in the UK by the APS Group on behalf of the Controller of Her Majestyʼs Stationery Office MEASURES ADOPTED AT THE THIRTY-NINTH ANTARCTIC TREATY CONSULTATIVE MEETING Santiago, Chile 23 May – 1 June 2016 The Measures1 adopted at the Thirty-ninth Antarctic Treaty Consultative Meeting are reproduced below from the Final Report of the Meeting. In accordance with Article IX, paragraph 4, of the Antarctic Treaty, the Measures adopted at Consultative Meetings become effective upon approval by all Contracting Parties whose representatives were entitled to participate in the meeting at which they were adopted (i.e. all the Consultative Parties). The full text of the Final Report of the Meeting, including the Decisions and Resolutions adopted at that Meeting and colour copies of the maps found in this command paper, is available on the website of the Antarctic Treaty Secretariat at www.ats.aq/documents. -
Immediate Scientific Report of the Ross Sea Iceberg Project 1987-88
SCIENCE AND RESEARCH INTERNAL REPORT 9 IMMEDIATE SCIENTIFIC REPORT OF THE ROSS SEA ICEBERG PROJECT 1987-88 by J.R. Keys and A.D.W. Fowler* This is an unpublished report and must not be cited or reproduced in whole or part without permission from the Director, Science and Research. It should be cited as Science and Research Internal Report No.9 (unpublished). Science and Research Directorate, Department of Conservation, P.O. Box 10 420 Wellington, New Zealand April 1988 *Division of Information Technology, DSIR, Lower Hutt. 1 Frontispiece. NOAA 9 infrared satellite image of the 160 km long mega-giant iceberg B-9 on 9 November, four weeks after separating from the eastern front of Ross Ice Shelf. The image was digitized by US Navy scientists at McMurdo Station, paid for by the US National Science Foundation and supplied by the Antarctic Research Center at Scripps Institute. Several other bergs up to 20 km long that calved at the same time can be seen between B-9 and the ice shelf. These bergs have since drifted as far west as Ross Island (approx 600 km) whereas B-9 has moved only 215 km by 13 April, generally in a west-north-west direction. 2 CONTENTS Frontispiece 1 Contents page 2 SUMMARY 3 INTRODUCTION 4 PROPOSED PROGRAMME 5 ITINERARY 6 SCIENTIFIC ACHIEVEMENTS RNZAF C-130 iceberg monitoring flight 6 SPOT satellite image and concurrent aerial Photography 8 Ground-based fieldwork 9 B-9 iceberg 11 CONCLUSION 13 FUTURE RESEARCH 13 PUBLICATIONS 14 Acknowledgenents 14 References 14 FIGURES 15 TABLES 20 3 1. -
The Antarctic Treaty
! ! ! ! ! ! The Antarctic Treaty ! ! ! ! Measures adopted at the Thirty-ninth Consultative Meeting held at Santiago, Chile 23 May – 1 June 2016 ! ! ! ! ! ! ! ! ! ! Presented to Parliament by the Secretary of State for Foreign and Commonwealth Affairs by Command of Her Majesty November 2017! Cm 9542 © Crown copyright 2017 This publication is licensed under the terms of the Open Government Licence v3.0 except where otherwise stated. To view this licence, visit nationalarchives.gov.uk/doc/open-government-licence/version/3 Where we have identified any third party copyright information you will need to obtain permission from the copyright holders concerned. This publication is available at www.gov.uk/government/publications Any enquiries regarding this publication should be sent to us at Treaty Section, Foreign and Commonwealth Office, King Charles Street, London, SW1A 2AH ISBN 978-1-5286-0126-9 CCS1117441642 11/17 Printed on paper containing 75% recycled fibre content minimum Printed in the UK by the APS Group on behalf of the Controller of Her Majesty!s Stationery Office MEASURES ADOPTED AT THE THIRTY-NINTH ANTARCTIC TREATY CONSULTATIVE MEETING Santiago, Chile 23 May – 1 June 2016 The Measures1 adopted at the Thirty-ninth Antarctic Treaty Consultative Meeting are reproduced below from the Final Report of the Meeting. In accordance with Article IX, paragraph 4, of the Antarctic Treaty, the Measures adopted at Consultative Meetings become effective upon approval by all Contracting Parties whose representatives were entitled to participate in the meeting at which they were adopted (i.e. all the Consultative Parties). The full text of the Final Report of the Meeting, including the Decisions and Resolutions adopted at that Meeting and colour copies of the maps found in this command paper, is available on the website of the Antarctic Treaty Secretariat at www.ats.aq/documents. -
Network Sites
CHAPTER 3: NETWORK SITES 3. Network Sites NSF UV monitoring network sites currently include three locations in Antarctica (McMurdo Station, Palmer Station, and Amundsen-Scott South Pole Station), one station in Ushuaia Argentina, and one site in Barrow, Alaska. In addition, one instrument system is installed in San Diego, California, which also serves as a training facility for site operators. Information on the longitude, latitude of the stations and the year they were established are given in Table 3.1. The sites are described in detail in the following, including prevailing meteorological conditions and typical column ozone values. Table 3.1. NSF spectroradiometer installation sites. ID # Site Longitude Latitude Established Normal Season 1 McMurdo, Antarctica 166º40’E 77º51’S March 1988 August – April 2 Palmer, Antarctica 64º03’W 64º46’S May 1988 Year-round 3 South Pole, Antarctica 0 90º00’S February 1988 September - March 4 Ushuaia, Argentina* 68º19’W 54º49’S November 1988 Year-round 5 San Diego, California** 117º11’W 32º45’N November 1992 Year-round 6 Barrow, Alaska*** 156º47’W 71º18’N December 1990 January – November *CADIC: Centro Austral de Investigaciones Cientificas, Argentina **Biospherical Instruments Inc. ***UIC/NARL: Ukpeagvik Inupiat Corporation (formerly) Naval Arctic Research Laboratory 3.1. McMurdo Station, Antarctica McMurdo Station is located on the southern tip of Ross Island (77°51’S, 166°40’E), and has had a long history in Antarctic exploration. It is the largest field station in Antarctica, accommodating up to 1200 people in summer and 250 in winter. There is a large laboratory facility, the “Crary Lab”, supporting a wide range of scientific projects. -
References the Larsen Shelf
ICE OF CROWN PRINCE GUSTAV CHANNEL, GRAHAM LAND, ANTARCTICA 409 Thus the Larsen Shelf Ice now extends north from Robertson Island into the southern end of the Channel. The position of its eastern edge, north of Robertson Island, is doubtful, but Taylor's party must have crossed it on their journey from Cape Longing to Snow Hill Island. They crossed some rifts when near Cape Foster which Russell says "might possibly open up and act as tide cracks," and it is most likely that the border between shelf and sea ice was somewhere in this area. In mid-September 1948 the edge of the shelf ice was observed to have broken back west wards to within about 24 km. of Cape Sobral. In conclusion, Larsen Shelf Ice, at the present time, extends as one continuous homogeneous sheet of varying thickness, north-eastwards from its previously mapped northern limit near Robertson Island to the Sji:igren Glacier tongue in the southern part of the Channel. Its seaward edge, whose position obviously varies from year to year, may be taken to run from Robertson Island generally north-east towards James Ross Island. North-east of the Sji:igren Glacier tongue landfast sea ice covers the northern part of the Channel and often persists for several seasons. I am indebted to Mr. J . M. Wordie, St. John's College, Cambridge, for much helpful criticism of this paper and also for the interpretation of the sea ice section. I also acknowledge with thanks the permission of the Colonial Office to publish this report. MS. -
Bruce Hopper
april 1936 The Soviet Conquest of the Far North Bruce Hopper Volume 14 • Number 3 The contents of Foreign Affairs are copyrighted.©1936 Council on Foreign Relations, Inc. All rights reserved. Reproduction and distribution of this material is permitted only with the express written consent of Foreign Affairs. Visit www.foreignaffairs.com/permissions for more information. THE SOVIET CONQUEST OF THE FAR NORTH By Bruce Hopper THE search for the Northeast Passage to Cathay, which for four centuries stirred the imagination of European mari seem at ners, has at last ended in triumph. We the beginning a new of phase of man's relations with the North. are to In this great polar saga three historic dates. The first seek the short-cut route from the Atlantic to the Pacific was Sir on Hugh Willoughby, who in 1553 perished with all hands the coast. In centuries of of Murman the ensuing navigators many the seafaring nations resumed the search. Some turned back be were to fore being caught; others lured eastward their doom in the ice. In 1878-79, A. E. Nordenski?ld made the first through passage by "freezing in" for the winter. The only other expedi to ? of on tions subsequently pass those Vil'kitsky, Amundsen on ? the Maud, Toll, and Nansen the celebrated Fram pursued the same method. It remained for the Soviet ice-breaker, Sibiry akov, from to Vladivostok in 1932, to sailing Arkhangelsk ? complete a season first the through-passage in single navigating the time in history. was not an was This feat accident of Soviet exploration.