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THE MOUNT EREBUS TRAGEDY Air New Zealand DC10-30 ZK-NZP, Flight NZ901 Th 28 November 1979
THE MOUNT EREBUS TRAGEDY Air New Zealand DC10-30 ZK-NZP, Flight NZ901 th 28 November 1979 A REVIEW WAVERLEY PARSONS Graduate Certificate in Antarctic Studies 2003 1 TABLE OF CONTENTS ABSTRACT ................................................................................................................... 2 Introduction ................................................................................................. 3 Prelude: Before the Flight of NZ901 .......................................................... 4 Flight Preparation .......................................................................................................... 4 The Flight Path ............................................................................................................... 5 The Accident ............................................................................................... 7 Sector Whiteout ............................................................................................................. 8 Discovery of Wreckage ............................................................................................... 10 ‘Operation Overdue’ .................................................................................................... 12 The Aftermath ...........................................................................................14 The Offical Aircraft Accident Report – ‘Chippindale’s Report’ ................................. 14 The Royal Commission of Inquiry ............................................................................. -
Antarctic Peninsula
Hucke-Gaete, R, Torres, D. & Vallejos, V. 1997c. Entanglement of Antarctic fur seals, Arctocephalus gazella, by marine debris at Cape Shirreff and San Telmo Islets, Livingston Island, Antarctica: 1998-1997. Serie Científica Instituto Antártico Chileno 47: 123-135. Hucke-Gaete, R., Osman, L.P., Moreno, C.A. & Torres, D. 2004. Examining natural population growth from near extinction: the case of the Antarctic fur seal at the South Shetlands, Antarctica. Polar Biology 27 (5): 304–311 Huckstadt, L., Costa, D. P., McDonald, B. I., Tremblay, Y., Crocker, D. E., Goebel, M. E. & Fedak, M. E. 2006. Habitat Selection and Foraging Behavior of Southern Elephant Seals in the Western Antarctic Peninsula. American Geophysical Union, Fall Meeting 2006, abstract #OS33A-1684. INACH (Instituto Antártico Chileno) 2010. Chilean Antarctic Program of Scientific Research 2009-2010. Chilean Antarctic Institute Research Projects Department. Santiago, Chile. Kawaguchi, S., Nicol, S., Taki, K. & Naganobu, M. 2006. Fishing ground selection in the Antarctic krill fishery: Trends in patterns across years, seasons and nations. CCAMLR Science, 13: 117–141. Krause, D. J., Goebel, M. E., Marshall, G. J., & Abernathy, K. (2015). Novel foraging strategies observed in a growing leopard seal (Hydrurga leptonyx) population at Livingston Island, Antarctic Peninsula. Animal Biotelemetry, 3:24. Krause, D.J., Goebel, M.E., Marshall. G.J. & Abernathy, K. In Press. Summer diving and haul-out behavior of leopard seals (Hydrurga leptonyx) near mesopredator breeding colonies at Livingston Island, Antarctic Peninsula. Marine Mammal Science.Leppe, M., Fernandoy, F., Palma-Heldt, S. & Moisan, P 2004. Flora mesozoica en los depósitos morrénicos de cabo Shirreff, isla Livingston, Shetland del Sur, Península Antártica, in Actas del 10º Congreso Geológico Chileno. -
Level 1 Geography (91010) 2020
91010R 1 Level 1 Geography 2020 91010 Apply concepts and basic geographic skills to demonstrate understanding of a given environment 2.00 p.m. Wednesday 18 November 2020 Credits: Four RESOURCE BOOKLET Refer to this booklet to answer the questions for Geography 91010. Check that this booklet has pages 2–8 in the correct order and that none of these pages is blank. YOU MAY KEEP THIS BOOKLET AT THE END OF THE EXAMINATION. © New Zealand Qualifications Authority, 2020. All rights reserved. No part of this publication may be reproduced by any means without the prior permission of the New Zealand QualificationsAuthority. 2 RESOURCE A: Introducing Ross Island, Antarctica Ross Island is located in Antarctica. The island has been formed by four volcanoes, and the largest of these, Mt Erebus, is the world’s southernmost active volcano. Ross Island is extremely important to New Zealand as it is home to Scott Base, New Zealand’s scientific research station in Antarctica. Scott Base was established at the island’s southern point – Hut Point Peninsula – by Edmund Hillary in 1957. Scott Base is run by Antarctica New Zealand, and its main function is to support scientists as they carry out their vital research on the continent over the summer months. New Zealand has a close relationship with the USA’s McMurdo Station, which is located nearby. During the winter months the island is in Research complete 24-hour darkness and temperatures can drop to –36 °C, which makes outside activities extremely dangerous. Ross Island played a significant part in the incredible exploration era of the early 1900s, when famous explorers such as Robert Scott and Ernest Shackleton used the island as a base as they tried to be the first to reach the South Pole. -
THE PUBLICATION of the NEW ZEALAND ANTARCTIC SOCIETY Vol 34, No
THE PUBLICATION OF THE NEW ZEALAND ANTARCTIC SOCIETY Vol 34, No. 3, 2016 34, No. Vol 03 9 770003 532006 Vol 34, No. 3, 2016 Issue 237 Contents www.antarctic.org.nz is published quarterly by the New Zealand Antarctic Society Inc. ISSN 0003-5327 30 The New Zealand Antarctic Society is a Registered Charity CC27118 EDITOR: Lester Chaplow ASSISTANT EDITOR: Janet Bray New Zealand Antarctic Society PO Box 404, Christchurch 8140, New Zealand Email: [email protected] INDEXER: Mike Wing The deadlines for submissions to future issues are 1 November, 1 February, 1 May and 1 August. News 25 Shackleton’s Bad Lads 26 PATRON OF THE NEW ZEALAND ANTARCTIC SOCIETY: From Gateway City to Volunteer Duty at Scott Base 30 Professor Peter Barrett, 2008 NEW ZEALAND ANTARCTIC SOCIETY How You Can Help Us Save Sir Ed’s Antarctic Legacy 33 LIFE MEMBERS The Society recognises with life membership, First at Arrival Heights 34 those people who excel in furthering the aims and objectives of the Society or who have given outstanding service in Antarctica. They are Conservation Trophy 2016 36 elected by vote at the Annual General Meeting. The number of life members can be no more Auckland Branch Midwinter Celebration 37 than 15 at any one time. Current Life Members by the year elected: Wellington Branch – 2016 Midwinter Event 37 1. Jim Lowery (Wellington), 1982 2. Robin Ormerod (Wellington), 1996 3. Baden Norris (Canterbury), 2003 Travelling with the Huskies Through 4. Bill Cranfield (Canterbury), 2003 the Transantarctic Mountains 38 5. Randal Heke (Wellington), 2003 6. Bill Hopper (Wellington), 2004 Hillary’s TAE/IGY Hut: Calling all stories 40 7. -
The Antarctican Society 905 North Jacksonville Street Arlington, Virginia 22205 Honorary President — Ambassador Paul C
THE ANTARCTICAN SOCIETY 905 NORTH JACKSONVILLE STREET ARLINGTON, VIRGINIA 22205 HONORARY PRESIDENT — AMBASSADOR PAUL C. DANIELS ________________________________________________________________ Presidents: Vol. 85-86 November No. 2 Dr. Carl R. Eklund, 1959-61 Dr. Paul A. Siple, 1961-2 Mr. Gordon D. Cartwright, 1962-3 RADM David M. Tyree (Ret.) 1963-4 Mr. George R. Toney, 1964-5 A PRE-THANKSGIVING TREAT Mr. Morton J. Rubin, 1965-6 Dr. Albert P. Crary, 1966-8 Dr. Henry M. Dater, 1968-70 Mr. George A. Doumani, 1970-1 MODERN ICEBREAKER OPERATIONS Dr. William J. L. Sladen, 1971-3 Mr. Peter F. Bermel, 1973-5 by Dr. Kenneth J. Bertrand, 1975-7 Mrs. Paul A. Siple, 1977-8 Dr. Paul C. Dalrymple, 1978-80 Commander Lawson W. Brigham Dr. Meredith F. Burrill, 1980-82 United States Coast Guard Dr. Mort D. Turner, 1982-84 Dr. Edward P. Todd, 1984-86 Liaison Officer to Chief of Naval Operations Washington, D.C. Honorary Members: Ambassador Paul C. Daniels on Dr. Laurence McKiniey Gould Count Emilio Pucci Tuesday evening, November 26, 1985 Sir Charles S. Wright Mr. Hugh Blackwell Evans 8 PM Dr. Henry M. Dater Mr. August Howard National Science Foundation Memorial Lecturers: 18th and G Streets NW Dr. William J. L. Sladen, 1964 RADM David M. Tyree (Ret.), 1965 Room 543 Dr. Roger Tory Peterson, 1966 Dr. J. Campbell Craddock, 1967 Mr. James Pranke, 1968 - Light Refreshments - Dr. Henry M. Dater, 1970 Sir Peter M. Scott, 1971 Dr. Frank T. Davies, 1972 Mr. Scott McVay, 1973 Mr. Joseph O. Fletcher, 1974 Mr. Herman R. Friis, 1975 This presentation by one of this country's foremost experts on ice- Dr. -
Chinstrap Penguin at Mcmurdo Sound References
riot suitable for both Stylatractus universus and seudoemi1iania lacunosa. Although the cause of the extinction levels may be in doubt, the extinction clatums are nonetheless strati graphically important and useful. This research was supported by National Science Foundation grant oii 74-20109. References Emiliani, C., and N. J . Shackleton. 1974. The Brunhes Epoch: isotopic paleotemperatures and geochronology. Science, 183: 511-514. Gartner, S. 1972. Late Pleistocene calcareous nanofossils in the Caribbean and their interoceanic correlation. Palaeogeography, Palaeocliinatology, Palaeoecology, 12: 169-191. Gartner, S. 1973. Absolute chronology of the Late Neogene calcareous nanofossil succession in the equatorial Pacific. Bulletin of the Geological Society ojAmerica, 84: 2021-2034. Chinstrap penguin, Pygoscelis antarctica, at the edge of the Hays, J . D. 1965. Radiolaria and late Tertiary and Quaternary ice channel leading to McMurdo Station. This photograph history of antarctic seas. Antarctic Research Series, 5: 125-134. was taken on 26 January 1975 from the bridge of USCGC Hays, J. D. 1967. Quaternary sediments of the antarctic ocean. Glacier. In: Progress in Oceanography (Sears, M., editor), 4: 117-131. -1ays, J . D., and W. A. Berggren. 1971. Quaternary bounda- ries and correlations. In: Micropaleontology of Oceans (Funnell, B. M., and W. R. Riedel, editors). 669-691. Kennett, J. P. 1970. Pleistocene paleoclimates and foraminiferal biostratigraphy in subantarctic deep-sea cores. Deep-Sea Re- ice channel leading to McMurdo Station. The pen- search, 17: 125-140. guin was seen approximately 3 kilometers north of Miyajima, M. H. 1974. Absolute chronology of Upper Pleisto- USCGC Staten Island. cene calcareous nanofossil zones of the southeast Indian McMurdo Station from aboard Ocean. -
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). -
Annual Warming Episodes in Seawater Temperatures in Mcmurdo Sound in Relationship to Endogenous Ice in Notothenioid Fish BEN M
Antarctic Science 15 (3): 333–338 (2003) © Antarctic Science Ltd Printed in the UK DOI: 10.1017/S0954102003001342 Annual warming episodes in seawater temperatures in McMurdo Sound in relationship to endogenous ice in notothenioid fish BEN M. HUNT, KEVIN HOEFLING and CHI-HING C. CHENG* Department of Animal Biology, University of Illinois, Urbana, IL 61801, USA *corresponding author: [email protected] Abstract: We obtained two years (1999–2001) of continuous, high resolution temperature and pressure data at two near-shore shallow water sites in McMurdo Sound, Ross Sea. Contrary to the long-held assumption of constant freezing conditions in the Sound, these records revealed dynamic temperature fluctuations and substantial warming during January to March reaching peak water temperatures of about -0.5°C. They also revealed that excursions above -1.1°C, the equilibrium melting point of ice in Antarctic notothenioid fish, totalled 8–21 days during the summer. Microscopic ice crystals are known to enter these fish but ice growth is arrested by antifreeze proteins. Prior to this study there were no known mechanisms of eliminating accumulated endogenous ice. The warm temperature excursions provide for the first time a possible physical mechanism, passive melting, for ice removal. The continuous records also showed a correlation between tidal pressures and cold temperature episodes, which suggests the influx of cold currents from under the Ross Ice Shelf may provide a mechanism for ice crystal nucleation as the source of the ice in McMurdo Sound fish. The accumulation of anchor ice on one logger caused it to float up which was recorded as a decrease in pressure. -
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. -
Federal Register/Vol. 84, No. 78/Tuesday, April 23, 2019/Rules
Federal Register / Vol. 84, No. 78 / Tuesday, April 23, 2019 / Rules and Regulations 16791 U.S.C. 3501 et seq., nor does it require Agricultural commodities, Pesticides SUPPLEMENTARY INFORMATION: The any special considerations under and pests, Reporting and recordkeeping Antarctic Conservation Act of 1978, as Executive Order 12898, entitled requirements. amended (‘‘ACA’’) (16 U.S.C. 2401, et ‘‘Federal Actions to Address Dated: April 12, 2019. seq.) implements the Protocol on Environmental Justice in Minority Environmental Protection to the Richard P. Keigwin, Jr., Populations and Low-Income Antarctic Treaty (‘‘the Protocol’’). Populations’’ (59 FR 7629, February 16, Director, Office of Pesticide Programs. Annex V contains provisions for the 1994). Therefore, 40 CFR chapter I is protection of specially designated areas Since tolerances and exemptions that amended as follows: specially managed areas and historic are established on the basis of a petition sites and monuments. Section 2405 of under FFDCA section 408(d), such as PART 180—[AMENDED] title 16 of the ACA directs the Director the tolerance exemption in this action, of the National Science Foundation to ■ do not require the issuance of a 1. The authority citation for part 180 issue such regulations as are necessary proposed rule, the requirements of the continues to read as follows: and appropriate to implement Annex V Regulatory Flexibility Act (5 U.S.C. 601 Authority: 21 U.S.C. 321(q), 346a and 371. to the Protocol. et seq.) do not apply. ■ 2. Add § 180.1365 to subpart D to read The Antarctic Treaty Parties, which This action directly regulates growers, as follows: includes the United States, periodically food processors, food handlers, and food adopt measures to establish, consolidate retailers, not States or tribes. -
Ice Production in Ross Ice Shelf Polynyas During 2017–2018 from Sentinel–1 SAR Images
remote sensing Article Ice Production in Ross Ice Shelf Polynyas during 2017–2018 from Sentinel–1 SAR Images Liyun Dai 1,2, Hongjie Xie 2,3,* , Stephen F. Ackley 2,3 and Alberto M. Mestas-Nuñez 2,3 1 Key Laboratory of Remote Sensing of Gansu Province, Heihe Remote Sensing Experimental Research Station, Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences, Lanzhou 730000, China; [email protected] 2 Laboratory for Remote Sensing and Geoinformatics, Department of Geological Sciences, University of Texas at San Antonio, San Antonio, TX 78249, USA; [email protected] (S.F.A.); [email protected] (A.M.M.-N.) 3 Center for Advanced Measurements in Extreme Environments, University of Texas at San Antonio, San Antonio, TX 78249, USA * Correspondence: [email protected]; Tel.: +1-210-4585445 Received: 21 April 2020; Accepted: 5 May 2020; Published: 7 May 2020 Abstract: High sea ice production (SIP) generates high-salinity water, thus, influencing the global thermohaline circulation. Estimation from passive microwave data and heat flux models have indicated that the Ross Ice Shelf polynya (RISP) may be the highest SIP region in the Southern Oceans. However, the coarse spatial resolution of passive microwave data limited the accuracy of these estimates. The Sentinel-1 Synthetic Aperture Radar dataset with high spatial and temporal resolution provides an unprecedented opportunity to more accurately distinguish both polynya area/extent and occurrence. In this study, the SIPs of RISP and McMurdo Sound polynya (MSP) from 1 March–30 November 2017 and 2018 are calculated based on Sentinel-1 SAR data (for area/extent) and AMSR2 data (for ice thickness). -
Geology of Hut Point Peninsula, Ross Island
significantly below their Curie temperatures (approxi- Wilson, R. L., and N. D. Watkins. 1967. Correlation of mately 550°C.). petrology and natural magnetic polarity in Columbia Plateau basalts. Geophysical Journal of the Royal Astro- Previous work (Pucher, 1969; Stacey and Banerjee, nomical Society, 12(4): 405-424. 1974) indicates that the CRM intensity acquired in a low field is significantly less than the TRM intensity. It thus would appear that if a CRM induced at temperatures considerably below the Curie tempera- Geology of Hut Point Peninsula, ture, contributes a significant proportion to the ob- Ross Island served NRM intensity, too low an intensity value will be assigned to the ancient field. Although it is too early to report a firm value for PHILIP R. KYLE the intensity of the ancient field during the imprint- Department of Geology ing of unit 13 and related flows, we think that the Victoria University strength of the ambient field was more likely to Wellington, New Zealand have been about 0.5 oe (based on samples at about 141 meters) than about 0.1 oe (based on samples SAMUEL B. TREVES 122.18 and 126.06 meters). The virtual dipole Department of Geology moment (Smith, 1967b) calculated for an estimated University of Nebraska field intensity of 0.5 oe at the site is 7 X 10 25 gauss Lincoln, Nebraska 68508 cubic centimeters. This is larger than the value of 5.5 X 1025 gauss cubic centimeters (Smith, 1967b) Hut Point Peninsula is about 20 kilometers long calculated on the basis of paleointensity experiments and 2 to 4 kilometers wide.