Management Plan for Antarctic Specially Protected Area No. 162
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Introduction Itinerary
ANTARCTICA - AKADEMIK SHOKALSKY TRIP CODE ACHEIWM DEPARTURE 10/02/2022 DURATION 25 Days LOCATIONS East Antarctica INTRODUCTION This is a 25 day expedition voyage to East Antarctica starting and ending in Invercargill, New Zealand. The journey will explore the rugged landscape and wildlife-rich Subantarctic Islands and cross the Antarctic circle into Mawsonâs Antarctica. Conditions depending, it will hope to visit Cape Denison, the location of Mawsonâs Hut. East Antarctica is one of the most remote and least frequented stretches of coast in the world and was the fascination of Australian Antarctic explorer, Sir Douglas Mawson. A true Australian hero, Douglas Mawson's initial interest in Antarctica was scientific. Whilst others were racing for polar records, Mawson was studying Antarctica and leading the charge on claiming a large chunk of the continent for Australia. On his quest Mawson, along with Xavier Mertz and Belgrave Ninnis, set out to explore and study east of the Mawson's Hut. On what began as a journey of discovery and science ended in Mertz and Ninnis perishing and Mawson surviving extreme conditions against all odds, with next to no food or supplies in the bitter cold of Antarctica. This expedition allows you to embrace your inner explorer to the backdrop of incredible scenery such as glaciers, icebergs and rare fauna while looking out for myriad whale, seal and penguin species. A truly unique journey not to be missed. ITINERARY DAY 1: Invercargill Arrive at Invercargill, New Zealand’s southernmost city. Established by Scottish settlers, the area’s wealth of rich farmland is well suited to the sheep and dairy farms that dot the landscape. -
Office of Polar Programs
DEVELOPMENT AND IMPLEMENTATION OF SURFACE TRAVERSE CAPABILITIES IN ANTARCTICA COMPREHENSIVE ENVIRONMENTAL EVALUATION DRAFT (15 January 2004) FINAL (30 August 2004) National Science Foundation 4201 Wilson Boulevard Arlington, Virginia 22230 DEVELOPMENT AND IMPLEMENTATION OF SURFACE TRAVERSE CAPABILITIES IN ANTARCTICA FINAL COMPREHENSIVE ENVIRONMENTAL EVALUATION TABLE OF CONTENTS 1.0 INTRODUCTION....................................................................................................................1-1 1.1 Purpose.......................................................................................................................................1-1 1.2 Comprehensive Environmental Evaluation (CEE) Process .......................................................1-1 1.3 Document Organization .............................................................................................................1-2 2.0 BACKGROUND OF SURFACE TRAVERSES IN ANTARCTICA..................................2-1 2.1 Introduction ................................................................................................................................2-1 2.2 Re-supply Traverses...................................................................................................................2-1 2.3 Scientific Traverses and Surface-Based Surveys .......................................................................2-5 3.0 ALTERNATIVES ....................................................................................................................3-1 -
Potential Regime Shift in Decreased Sea Ice Production After the Mertz Glacier Calving
ARTICLE Received 27 Jan 2012 | Accepted 3 Apr 2012 | Published 8 May 2012 DOI: 10.1038/ncomms1820 Potential regime shift in decreased sea ice production after the Mertz Glacier calving T. Tamura1,2,*, G.D. Williams2,*, A.D. Fraser2 & K.I. Ohshima3 Variability in dense shelf water formation can potentially impact Antarctic Bottom Water (AABW) production, a vital component of the global climate system. In East Antarctica, the George V Land polynya system (142–150°E) is structured by the local ‘icescape’, promoting sea ice formation that is driven by the offshore wind regime. Here we present the first observations of this region after the repositioning of a large iceberg (B9B) precipitated the calving of the Mertz Glacier Tongue in 2010. Using satellite data, we find that the total sea ice production for the region in 2010 and 2011 was 144 and 134 km3, respectively, representing a 14–20% decrease from a value of 168 km3 averaged from 2000–2009. This abrupt change to the regional icescape could result in decreased polynya activity, sea ice production, and ultimately the dense shelf water export and AABW production from this region for the coming decades. 1 National Institute of Polar Research, Tachikawa, Japan. 2 Antarctic Climate & Ecosystem Cooperative Research Centre, University of Tasmania, Hobart, Australia. 3 Institute of Low Temperature of Science, Sapporo, Japan. *These authors contributed equally to this work. Correspondence and requests for materials should be addressed to T.T. (email: [email protected]) or to G.D.W. (email: [email protected]). NATURE COMMUNICATIONS | 3:826 | DOI: 10.1038/ncomms1820 | www.nature.com/naturecommunications © 2012 Macmillan Publishers Limited. -
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. -
Crustal Architecture of the Oblique-Slip Conjugate Margins of George V Land and Southeast Australia H
U. S. Geological Survey and The National Academies; USGS OF-2007-1047, Short Research Paper 109; doi: 10.3133/of2007-1047.srp109 Crustal architecture of the oblique-slip conjugate margins of George V Land and southeast Australia H. M. J. Stagg1 and A. M. Reading2 1Geoscience Australia, GPO Box 378, Canberra ACT 2601, Australia ([email protected]) 2School of Earth Sciences, University of Tasmania, Private Bag 79, Hobart TAS 7001, Australia ([email protected]) Abstract A conceptual, lithospheric-scale cross-section of the conjugate, oblique-slip margins of George V Land, East Antarctica, and southeast Australia (Otway Basin) has been constructed based on the integration of seismic and sample data. This cross-section is characterised by asymmetry in width and thickness, and depth-dependent crustal extension at breakup in the latest Maastrichtian. The broad Antarctic margin (~360 km apparent rift width) developed on thick crust (~42 km) of the Antarctic craton, whereas the narrow Otway margin (~220 km) developed on the thinner crust (~31 km) of the Ross–Delamerian Orogen. The shallow basement (velocities ~5.5 km.s-1) and the deep continental crust (velocities >6.4 km.s-1) appear to be largely absent across the central rift, while the mid-crustal, probably granitic layer (velocities ~6 km.s-1) is preserved. Comparison with published numerical models suggests that the shallow basement and deep crust may have been removed by simple shear, whereas the mid-crust has been ductilely deformed. Citation: H.M.J. Stagg and A.M. Reading (2007), Crustal architecture of the oblique-slip conjugate margins of George V Land and southeast Australia, in Antarctica: A Keystone in a Changing World – Online Proceedings of the 10th ISAES, edited by A.K. -
Antarctic Primer
Antarctic Primer By Nigel Sitwell, Tom Ritchie & Gary Miller By Nigel Sitwell, Tom Ritchie & Gary Miller Designed by: Olivia Young, Aurora Expeditions October 2018 Cover image © I.Tortosa Morgan Suite 12, Level 2 35 Buckingham Street Surry Hills, Sydney NSW 2010, Australia To anyone who goes to the Antarctic, there is a tremendous appeal, an unparalleled combination of grandeur, beauty, vastness, loneliness, and malevolence —all of which sound terribly melodramatic — but which truly convey the actual feeling of Antarctica. Where else in the world are all of these descriptions really true? —Captain T.L.M. Sunter, ‘The Antarctic Century Newsletter ANTARCTIC PRIMER 2018 | 3 CONTENTS I. CONSERVING ANTARCTICA Guidance for Visitors to the Antarctic Antarctica’s Historic Heritage South Georgia Biosecurity II. THE PHYSICAL ENVIRONMENT Antarctica The Southern Ocean The Continent Climate Atmospheric Phenomena The Ozone Hole Climate Change Sea Ice The Antarctic Ice Cap Icebergs A Short Glossary of Ice Terms III. THE BIOLOGICAL ENVIRONMENT Life in Antarctica Adapting to the Cold The Kingdom of Krill IV. THE WILDLIFE Antarctic Squids Antarctic Fishes Antarctic Birds Antarctic Seals Antarctic Whales 4 AURORA EXPEDITIONS | Pioneering expedition travel to the heart of nature. CONTENTS V. EXPLORERS AND SCIENTISTS The Exploration of Antarctica The Antarctic Treaty VI. PLACES YOU MAY VISIT South Shetland Islands Antarctic Peninsula Weddell Sea South Orkney Islands South Georgia The Falkland Islands South Sandwich Islands The Historic Ross Sea Sector Commonwealth Bay VII. FURTHER READING VIII. WILDLIFE CHECKLISTS ANTARCTIC PRIMER 2018 | 5 Adélie penguins in the Antarctic Peninsula I. CONSERVING ANTARCTICA Antarctica is the largest wilderness area on earth, a place that must be preserved in its present, virtually pristine state. -
Antarctica: Music, Sounds and Cultural Connections
Antarctica Music, sounds and cultural connections Antarctica Music, sounds and cultural connections Edited by Bernadette Hince, Rupert Summerson and Arnan Wiesel Published by ANU Press The Australian National University Acton ACT 2601, Australia Email: [email protected] This title is also available online at http://press.anu.edu.au National Library of Australia Cataloguing-in-Publication entry Title: Antarctica - music, sounds and cultural connections / edited by Bernadette Hince, Rupert Summerson, Arnan Wiesel. ISBN: 9781925022285 (paperback) 9781925022292 (ebook) Subjects: Australasian Antarctic Expedition (1911-1914)--Centennial celebrations, etc. Music festivals--Australian Capital Territory--Canberra. Antarctica--Discovery and exploration--Australian--Congresses. Antarctica--Songs and music--Congresses. Other Creators/Contributors: Hince, B. (Bernadette), editor. Summerson, Rupert, editor. Wiesel, Arnan, editor. Australian National University School of Music. Antarctica - music, sounds and cultural connections (2011 : Australian National University). Dewey Number: 780.789471 All rights reserved. No part of this publication may be reproduced, stored in a retrieval system or transmitted in any form or by any means, electronic, mechanical, photocopying or otherwise, without the prior permission of the publisher. Cover design and layout by ANU Press Cover photo: Moonrise over Fram Bank, Antarctica. Photographer: Steve Nicol © Printed by Griffin Press This edition © 2015 ANU Press Contents Preface: Music and Antarctica . ix Arnan Wiesel Introduction: Listening to Antarctica . 1 Tom Griffiths Mawson’s musings and Morse code: Antarctic silence at the end of the ‘Heroic Era’, and how it was lost . 15 Mark Pharaoh Thulia: a Tale of the Antarctic (1843): The earliest Antarctic poem and its musical setting . 23 Elizabeth Truswell Nankyoku no kyoku: The cultural life of the Shirase Antarctic Expedition 1910–12 . -
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. -
32. Mawson's Huts and Cape Denison
32. Mawson’s Huts and Cape Denison Updated: 2014 67°00’31”S, 142°40’43”E – Mawson’s Huts and Cape Denison, Commonwealth Bay, East Antarctica, Antarctic Specially Protected Area No. 162, and Historic Site and Monument No. 77. Key features ‐ Historic huts and original contents from the Australasian Antarctic Expedition of 1911‐ 1914 led by Dr (later Sir) Douglas Mawson. ‐ A largely unmodified cultural landscape with expedition huts, objects and artefacts in their original context, demonstrating the living conditions, scientific research, isolation, and environmental extremes of the expedition. Description Topography: Cape Denison is a largely ice‐free peninsula adjacent to the polar plateau. The cape consists of rocky ridges and valleys. The Antarctic Specially Protected Area (ASPA) extends from Land’s End to John O’Groats, and south to the moraine line. Fauna: Confirmed breeders: Adélie penguins (Pygoscelis adeliae) in multiple colonies, and small numbers of Wilson’s storm petrels (Oceanites oceanicus), snow petrels (Pagodroma nivea), and south polar skuas (Catharacta maccormicki). Other: Weddell, leopard, and elephant seals haul out (Leptonychotes weddellii, Hydrurga leptonyx, Mirounga leonina), and emperor penguins (Aptenodytes forsteri), southern giant petrels (Macronectes giganteus), cape petrels (Daption capense), and Antarctic petrels (Thalassoica Antarctica) have been observed. Flora: 13 lichen species, and non‐marine algae have been recorded in the area. Historic Huts and Artefacts: Four huts from the Australasian Antarctic Expedition of 1911‐1914 stand at Cape Denison: the Main Hut and the Magnetograph House which are intact; and the Absolute Magnetic Hut and Transit Hut which are standing ruins. Also present are remains of scientific instruments and installations, wireless masts, a memorial cross, and scatters of artefacts. -
Australian ANTARCTIC Magazine ISSUE 18 2010 Australian
AusTRALIAN ANTARCTIC MAGAZINE ISSUE 18 2010 AusTRALIAN ANTARCTIC ISSUE 2010 MAGAZINE 18 The Australian Antarctic Division, a Division of the Department of the Environment, Water, Heritage and the Arts, leads Australia’s Antarctic program and seeks CONTENTS to advance Australia’s Antarctic interests in pursuit of its vision of having ‘Antarctica valued, protected EXPLORING THE SOUTHERN OCEAN and understood’. It does this by managing Australian government activity in Antarctica, providing transport Southern Ocean marine life in focus 1 and logistic support to Australia’s Antarctic research Snails and ‘snot’ tell acid story 4 program, maintaining four permanent Australian research stations, and conducting scientific research Science thrown overboard 6 programs both on land and in the Southern Ocean. Antarctica – a catalyst for science communication 8 Australia’s four Antarctic goals are: First non-lethal whale study answers big questions 9 • To maintain the Antarctic Treaty System Journal focuses on Antarctic research 11 and enhance Australia’s influence in it; • To protect the Antarctic environment; BROKE–West breaks ground in marine research 11 • To understand the role of Antarctica in EAST ANTARCTIC CENSUS the global climate system; and Shedding light on the sea floor 13 • To undertake scientific work of practical, economic and national significance. Plankton in the spotlight 15 Australian Antarctic Magazine seeks to inform the Sorting the catch 16 Australian and international Antarctic community Using fish to identify ecological regions 17 about the activities of the Australian Antarctic program. Opinions expressed in Australian Antarctic Magazine International flavour enhances Japanese research cruise 18 do not necessarily represent the position of the Australian Government. -
Cape Denison MAWSON CENTENNIAL 1911–2011, Commonwealth Bay
Cape Denison MAWSON CENTENNIAL 1911–2011, Commonwealth Bay Mawson and the Australasian Geology of Cape Denison Landforms of Cape Denison Position of Cape Denison in Gondwana Antarctic Expedition The two dominant rock-types found at Cape Denison Cape Denison is a small ice-free rocky outcrop covering Around 270 Million years ago the continents that we are orthogneiss and amphibolite. There are also minor less than one square kilometre, which emerges from The Australasian Antarctic Expedition (AAE) took place know today were part of a single ancient supercontinent occurrences of coarse grained felsic pegmatites. beneath the continental ice sheet. Stillwell (1918) reported between 1911 and 1914, and was organised and led by called Pangea. Later, Pangea split into two smaller that the continental ice sheet rises steeply behind Cape the geologist, Dr Douglas Mawson. The expedition was The Cape Denison Orthogneiss was described by Stillwell (1918) as supercontinents, Laurasia and Gondwana, and Denison reaching an altitude of ‘1000 ft in three miles and jointly funded by the Australian and British Governments coarse-grained grey quartz-feldspar layered granitic gneiss. These rock Antarctica formed part of Gondwana. with contributions received from various individuals and types are normally formed by metamorphism (changed by extreme heat 1500 ft in five and a half miles’ (approximately 300 metres and pressure) of granites. The Cape Denison Orthogneiss is found around In current reconstructions of the supercontinent Gondwana, the Cape scientific societies, including the Australasian Association to 450 metres over 8.9 kilometres). Photography by Chris Carson Cape Denison, the nearby offshore Mackellar Islands, and nearby outcrops Denison–Commonwealth Bay region was located adjacent to the coast for the Advancement of Science. -
Southward an Analysis of the Literary Productions of the Discovery and Nimrod Expeditions to Antarctica
Corso di Laurea magistrale (ordinamento ex D.M. 270/2004) In LLEAP – Lingue e Letterature Europee, Americane e Postcoloniali Tesi di Laurea Southward An analysis of the literary productions of the Discovery and Nimrod Expeditions to Antarctica. Relatore Ch. Prof. Emma Sdegno Laureando Monica Stragliotto Matricola 820667 Anno Accademico 2012 / 2013 CONTENTS INTRODUCTION 3 Chapter I The History of Explorations in Antarctica 8 Chapter II Outstanding Men, Outstanding Deeds 31 Chapter III Antarctic Journals: the Models 46 Chapter IV Antarctic Journals: Scott’s Odyssey and Shackleton’s Personal Attempt 70 Chapter V The South Polar Times and Aurora Australis: Antarctic Literary Productions 107 CONCLUSION 129 BIBLIOGRAPHY 134 2 INTRODUCTION When we think about Antarctica, we cannot help thinking of names such as Roald Admunsen, Robert Falcon Scott and Ernest Shackleton. These names represented the greatest demonstration of human endurance and courage in exploration and they still preserve these features today. The South Pole represented an unspoilt, unknown, unexplored area for a long time, and all the Nations competed fiercely to be the first to reach the geographical South Pole. England, which displays a great history of exploration, contributed massively to the rush to the Antarctic especially in the first decade of the 20th century. The long years spent in the Antarctic by the British explorers left a priceless inheritance. First of all, the scientific fields such as meteorology, geology and zoology were tellingly improved. The study of the ice sheet allowed the scientists of the time to partly explain the phenomenon of glaciations. In addition, magnetism was still a new field to be explored and the study of phenomena such as the aurora australis and the magnetic pole as a moving spot1 were great discoveries that still influence our present knowledge.