Ross Island Trail System Mcmurdo Station & Scott Base, Antarctica
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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. -
Mcmurdo STATION MODERNIZATION STUDY Building Shell & Fenestration Study
McMURDO STATION MODERNIZATION STUDY Building Shell & Fenestration Study April 29, 2016 Final Submittal MCMURDO STATION MODERNIZATION STUDY | APRIL 29, 2016 MCMURDO STATION MODERNIZATION STUDY | APRIL 29, 2016 2 TABLE OF CONTENTS Section 1: Overview PG. 7-51 Team Directory PG. 8 Project Description PG. 9 Methodology PG. 10-11 Design Criteria/Environmental Conditions PG. 12-20 (a) General Description (b) Environmental Conditions a. Wind b. Temp c. RH d. UV e. Duration of sunlight f. Air Contaminants (c) Graphic (d) Design Criteria a. Thermal b. Air Infiltration c. Moisture d. Structural e. Fire Safety f. Environmental Impact g. Corrosion/Degradation h. Durability i. Constructability j. Maintainability k. Aesthetics l. Mechanical System, Ventilation Performance and Indoor Air Quality implications m. Structural implications PG. 21-51 Benchmarking 3 Section 2: Technical Investigation and Research PG. 53-111 Envelope Components and Assemblies PG. 54-102 (a) Components a. Cladding b. Air Barrier c. Insulation d. Vapor Barrier e. Structural f. Interior Assembly (b) Assemblies a. Roofs b. Walls c. Floors Fenestration PG. 103-111 (a) Methodology (b) Window Components Research a. Window Frame b. Glazing c. Integration to skin (c) Door Components Research a. Door i. Types b. Glazing Section 3: Overall Recommendation PG. 113-141 Total Configured Assemblies PG. 114-141 (a) Roofs a. Good i. Description of priorities ii. Graphic b. Better i. Description of priorities ii. Graphic c. Best i. Description of priorities ii. Graphic 4 (b) Walls a. Good i. Description of priorities ii. Graphic b. Better i. Description of priorities ii. Graphic c. Best i. Description of priorities ii. -
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. -
NITROGEN on MARS: INSIGHTS from CURIOSITY. J. C. Stern1 , B. Sutter2, W. A. Jackson3, Rafael Na- Varro-González4, Christopher P
Lunar and Planetary Science XLVIII (2017) 2726.pdf 1 2 3 NITROGEN ON MARS: INSIGHTS FROM CURIOSITY. J. C. Stern , B. Sutter , W. A. Jackson , Rafael Na- varro-González4, Christopher P. McKay5, Douglas W. Ming6, P. Douglas Archer2, D. P. Glavin1, A. G. Fairen7,8 and Paul R. Mahaffy1. 1NASA GSFC, Code 699, Greenbelt, MD 20771, [email protected], 2Jacobs, NASA Johnson Space Center, Houston, TX 77058, 3Texas Tech University, Lubbock, TX 79409, 4Universidad Nacional Autónoma de México, México, D.F. 04510, Mexico, 5NASA Ames Research Center, Moffett Field, CA 94035, 6NASA Johnson Space Center, Houston TX 77058, 7Centro de Astrobiologia, Madrid, Spain, 8Cornell University, Ithaca, NY 14853 Introduction: Recent detection of nitrate on Mars [1] indicates that nitrogen fixation processes occurred in early martian history. Data collected by the Sample Analysis at Mars (SAM) instrument on the Curiosity Rover can be integrated with Mars analog work in order to better understand the fixation and mobility of nitrogen on Mars, and thus its availability to putative biology. In particular, the relationship between nitrate and other soluble salts may help reveal the timing of nitrogen fixation and post-depositional behavior of nitrate on Mars. In addition, in situ measurements of nitrogen abundance and isotopic composition may be used to model atmospheric conditions on early Mars. Methods: The data presented are from analyses of solid Martian drilled and scooped samples by the Sam- ple Analysis at Mars (SAM) instrument suite on the Mars Science Laboratory (MSL) Curiosity Rover. SAM performs evolved gas analysis (EGA), in which a 3 Figure 1. -
Polar Ice Coring and IGY 1957-58 in This Issue
NEWSLETTER OF T H E N A T I O N A L I C E C O R E L ABORATORY — S CIE N C E M A N AGE M E N T O FFICE Vol. 3 Issue 1 • SPRING 2008 Polar Ice Coring and IGY 1957-58 In this issue . An Interview with Dr. Anthony J. “Tony” Gow Polar Ice Coring and IGY 1957-58 From the early 1950’s through the mid-1960’s, U.S. polar ice coring research was led by two U.S. Army An Interview with Dr. Tony Gow .... 1 Corps of Engineers research labs: the Snow, Ice, and Permafrost Research Establishment (SIPRE), and Upcoming Meetings ...................... 2 later, the Cold Regions Research and Engineering Laboratory (CRREL). One of the high-priority research Greenland Science projects recommended by the U.S. National Academy of Sciences/National Committee for IGY 1957-58 and Education Week ..................... 3 was to deep core drill into polar ice sheets for scientific purposes. To this end, SIPRE was tasked with Ice Core Working Group developing and running the entire U.S. ice core drilling and research program. Following the successful Members ....................................... 3 pre-IGY pilot drilling trials at Site-2 NW Greenland in 1956 (305 m) and 1957 (411 m), the SIPRE WAIS Divide turned their attention to deep ice core drilling in Antarctica for IGY 1957-58. Dr. Anthony J. (Tony) Ice Core Update ............................ 5 Gow (CRREL, retired) was one of the scientists on the project. In March 2008, the NICL-SMO had Ice Cores and POLAR-PALOOZA the opportunity to sit down with Dr. -
Non-Collider Searches for Stable Massive Particles
Non-collider searches for stable massive particles S. Burdina, M. Fairbairnb, P. Mermodc,, D. Milsteadd, J. Pinfolde, T. Sloanf, W. Taylorg aDepartment of Physics, University of Liverpool, Liverpool L69 7ZE, UK bDepartment of Physics, King's College London, London WC2R 2LS, UK cParticle Physics department, University of Geneva, 1211 Geneva 4, Switzerland dDepartment of Physics, Stockholm University, 106 91 Stockholm, Sweden ePhysics Department, University of Alberta, Edmonton, Alberta, Canada T6G 0V1 fDepartment of Physics, Lancaster University, Lancaster LA1 4YB, UK gDepartment of Physics and Astronomy, York University, Toronto, ON, Canada M3J 1P3 Abstract The theoretical motivation for exotic stable massive particles (SMPs) and the results of SMP searches at non-collider facilities are reviewed. SMPs are defined such that they would be suffi- ciently long-lived so as to still exist in the cosmos either as Big Bang relics or secondary collision products, and sufficiently massive such that they are typically beyond the reach of any conceiv- able accelerator-based experiment. The discovery of SMPs would address a number of important questions in modern physics, such as the origin and composition of dark matter and the unifi- cation of the fundamental forces. This review outlines the scenarios predicting SMPs and the techniques used at non-collider experiments to look for SMPs in cosmic rays and bound in mat- ter. The limits so far obtained on the fluxes and matter densities of SMPs which possess various detection-relevant properties such as electric and magnetic charge are given. Contents 1 Introduction 4 2 Theory and cosmology of various kinds of SMPs 4 2.1 New particle states (elementary or composite) . -
Perchlorate and Chlorate Biogeochemistry in Ice-Covered Lakes of the Mcmurdo Dry Valleys, Antarctica
Available online at www.sciencedirect.com Geochimica et Cosmochimica Acta 98 (2012) 19–30 www.elsevier.com/locate/gca Perchlorate and chlorate biogeochemistry in ice-covered lakes of the McMurdo Dry Valleys, Antarctica W. Andrew Jackson a,⇑, Alfonso F. Davila b,c, Nubia Estrada a, W. Berry Lyons d, John D. Coates e, John C. Priscu f a Department of Civil and Environmental Engineering, Texas Tech University, Lubbock, TX 79409, USA b NASA Ames Research Center, Moffett Field, CA 95136, USA c SETI Institute, 189 Bernardo Ave., Suite 100, Mountain View, CA 94043-5203, USA d Byrd Polar Research Center, The Ohio State University, Columbus, OH 43210, USA e Department of Plant and Microbial Biology, University of California, Berkeley, CA 94720, USA f Department of Land Resources & Environmental Sciences, Montana State University, Bozeman, MT 59717, USA Received 15 February 2012; accepted in revised form 5 September 2012; available online 19 September 2012 Abstract À À We measured chlorate (ClO3 ) and perchlorate (ClO4 ) concentrations in ice covered lakes of the McMurdo Dry Valleys À À (MDVs) of Antarctica, to evaluate their role in the ecology and geochemical evolution of the lakes. ClO3 and ClO4 are À À present throughout the MDV Lakes, streams, and other surface water bodies. ClO3 and ClO4 originate in the atmosphere and are transported to the lakes by surface inflow of glacier melt that has been differentially impacted by interaction with soils À À and aeolian matter. Concentrations of ClO3 and ClO4 in the lakes and between lakes vary based on both total evaporative concentration, as well as biological activity within each lake. -
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. -
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). -
NO ONE KNOWS ABOUT US by Bridget Canning. a Creative Writing
NO ONE KNOWS ABOUT US By Bridget Canning. A Creative Writing Thesis submitted to the School of Graduate Studies in partial fulfillment of the requirements for the degree of Masters of Arts in English (Creative Writing) Department of English, Memorial University of Newfoundland Abstract: No One Knows about Us is a collection of twelve contemporary short stories. As the title suggests, the characters in each story deal with secrets: relationships, longings, grudges, addictions, and trickery. For them, these secrets are simultaneously overwhelming and futile; their importance within their small worlds reflect a deeper feeling of insignificance in the greater scheme of life in a small city in a northern province hemmed on to the side of a continent. Here are a range of characters and situations set in St. John’s, Newfoundland and Labrador. The stories are mapped out in different areas of the city and move chronologically over a year, starting in fall and ending in late summer. They work together to create a small sample of life in modern-day St. John’s – one that is informed by the influences of history, economy, and weather. i Acknowledgements: This thesis would not have been accomplished without the help of the English department faculty at Memorial such as Robert Finley, Robert Chafe, and especially my thesis advisor, Lisa Moore. Thanks to the Graduate Society for their financial support. Thanks to Jonathan Weir, Deirdre Snook, and the members of the Naked Parade Writing Collective for their guidance and encouragement. ii Contents: 1. Seen, p. 1 2. With Glowing Hearts, p. 19 3. -
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.