The Emperor Penguin - Vulnerable to Projected Rates of Warming and Sea Ice Loss ⁎ Philip N
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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. -
Management Plan for Specially Protected Area No. 8 Dion Islands, Marguerite Bay, Antarctic Peninsula
ANNEX TO RECOMMENDATION XVI-6 Management Plan for Specially Protected Area No. 8 Dion Islands, Marguerite Bay, Antarctic Peninsula 1. Geographical location The Dion Islands (67°52'S, 68°43'W) are a small group of low-lying rocky islands lying about 13 km south of the southern end of Adelaide Island, in the north- western part of Marguerite Bay. 2. Management Plan (i) Description of Area The Area comprises all of the Dion Islands archipelago, which lie within an area of about 12 km2, together with the intervening sea. The islands and islets are small, rocky and often precipitous, notably Emperor Island which is also the highest (46 m altitude). The main islands are the largest of the Courtier Islands group (c. 8 ha), Emperor Island (c. 5 ha) and the largest of the Consort Islands group (c. 3 ha). Low lying areas occur on the two largest islands. There are a few small permanent ice patches, but there are no streams or permanent pools. (ii) Reason for designation The Area possesses the only known breeding population of Emperor penguins (Aptenodytes forsteri) on the west side of the Antarctic Peninsula. It is situated on a low-lying raised beach and rocky headland in the south-eastern part of Emperor Island. It is also the most northerly and probably the smallest colony (annual numbers fluctuate between about 50 and 500 pairs), and is one of only two in which breeding occurs on land (see also SPA No. 1). It is also the most isolated Emperor colony, being about 2,500 km (by sea) from the nearest other known rookery. -
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. -
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 .................................................................................................................................. -
A NEWS BULLETIN Published Quarterly by the NEW ZEALAND
A N E W S B U L L E T I N p u b l i s h e d q u a r t e r l y b y t h e NEW ZEALAND ANTARCTIC SOCIETY THESE VISITORS TO LAKE FRYXELL IN THE TAYLOR VALLEY ARE LIKE DWARFS AGAINST THE TOWERING CANADA GLACIER WHICH FLOWS DOWN FROM THE ASGAARD RANGE. —Photo by R. K. McBride. Antarctic Division, D.S.I.R. September 1972 «i (Successor to "Antarctic News Bulletin") Vol. 6, No. 7 67th ISSUE Editor: H. F. GRIFFITHS, 14 Woodchester Avenue, Christchurch 1. Assistant Editor: J. M. CAFFIN, 35 Chepstow Avenue, Christchurch 5. Address all contributions, enquiries, etc., to the Editor. All Business Communications, Subscriptions, etc., to: The Secretary, New Zealand Antarctic Society, P.O. Box 1223, Christchurch, N.Z CONTENTS ARTICLES SECOND-IN-COMMAND POLAR ACTIVITIES NEW ZEALAND 222, 225, 231, 240, 243, 251, 253 U.S.A 226, 232, 252 AUSTRALIA 236 UNITED KINGDOM 234 U.S.S.R 238, 239, 241 SOUTH AFRICA 242, 250 CZECHOSLOVAKIA 235 SUB-ANTARCTIC CAMPBELL ISLAND GENERAL LONE TRIP TO POLE DISCOVERY EXPEDITION LETTERS WHALING QUOTAS FIXED ANTARCTIC BOOKSHELF Fifteen years have passed since the International Geophysical Year of 1957-58 and it might be thought that the Antarctic Continent, through the continuing research carried out by the participating nations, would by now have yielded up all its secrets. But this is a false premise; new discoveries in the various branches of science have either highlighted gaps in our knowledge or have pointed the way to investigation in new fields. -
Species Status Assessment Emperor Penguin (Aptenodytes Fosteri)
SPECIES STATUS ASSESSMENT EMPEROR PENGUIN (APTENODYTES FOSTERI) Emperor penguin chicks being socialized by male parents at Auster Rookery, 2008. Photo Credit: Gary Miller, Australian Antarctic Program. Version 1.0 December 2020 U.S. Fish and Wildlife Service, Ecological Services Program Branch of Delisting and Foreign Species Falls Church, Virginia Acknowledgements: EXECUTIVE SUMMARY Penguins are flightless birds that are highly adapted for the marine environment. The emperor penguin (Aptenodytes forsteri) is the tallest and heaviest of all living penguin species. Emperors are near the top of the Southern Ocean’s food chain and primarily consume Antarctic silverfish, Antarctic krill, and squid. They are excellent swimmers and can dive to great depths. The average life span of emperor penguin in the wild is 15 to 20 years. Emperor penguins currently breed at 61 colonies located around Antarctica, with the largest colonies in the Ross Sea and Weddell Sea. The total population size is estimated at approximately 270,000–280,000 breeding pairs or 625,000–650,000 total birds. Emperor penguin depends upon stable fast ice throughout their 8–9 month breeding season to complete the rearing of its single chick. They are the only warm-blooded Antarctic species that breeds during the austral winter and therefore uniquely adapted to its environment. Breeding colonies mainly occur on fast ice, close to the coast or closely offshore, and amongst closely packed grounded icebergs that prevent ice breaking out during the breeding season and provide shelter from the wind. Sea ice extent in the Southern Ocean has undergone considerable inter-annual variability over the last 40 years, although with much greater inter-annual variability in the five sectors than for the Southern Ocean as a whole. -
Velocity Increases at Cook Glacier, East Antarctica Linked to Ice Shelf Loss and a Subglacial Flood Event
The Cryosphere Discuss., https://doi.org/10.5194/tc-2018-107 Manuscript under review for journal The Cryosphere Discussion started: 1 June 2018 c Author(s) 2018. CC BY 4.0 License. Velocity increases at Cook Glacier, East Antarctica linked to ice shelf loss and a subglacial flood event Bertie W.J. Miles1*, Chris R. Stokes1, Stewart S.R. Jamieson1 1Department of Geography, Durham University, Science Site, South Road, Durham, DH1 3LE 5 Correspondence to: [email protected] Abstract: Cook Glacier drains a large proportion of the Wilkes Subglacial Basin in East Antarctica, a region thought to be vulnerable to marine ice sheet instability and with potential to make a significant contribution to sea-level. Despite its importance, there have been very 10 few observations of its longer-term behaviour (e.g. of velocity or changes at its ice front). Here we use a variety of satellite imagery to produce a time-series of ice-front position change from 1947-2017 and ice velocity from 1973-2017. Cook Glacier has two distinct outlets (termed East and West) and we observe the near-complete loss of the Cook West Ice Shelf at some time between 1973 and 1989. This was associated with a doubling of the velocity of Cook West 15 glacier, which may also be linked to previously published reports of inland thinning. The loss of the Cook West Ice Shelf is surprising given that the present-day ocean-climate conditions in the region are not typically associated with catastrophic ice shelf loss. However, we speculate that a more intense ocean-climate forcing in the mid-20th century may have been important in forcing its collapse. -
Haswell Island (Haswell Island and Adjacent Emperor Penguin Rookery on Fast Ice)
Measure 5 (2016) Management Plan for Antarctic Specially Protected Area No. 127 Haswell Island (Haswell Island and Adjacent Emperor Penguin Rookery on Fast Ice) 1. Description of values to be protected The area includes Haswell Island with its littoral zone and adjacent fast ice when present. Haswell Island was discovered in 1912 by the Australian Antarctic Expedition led by D. Mawson. It was named after William Haswell, professor of biology who rendered assistance to the expedition. Haswell is the biggest island of the same-name archipelago, with a height of 93 meters and 0,82 sq.meters in area. The island is at 2,5 km distance from the Russian Mirny Station operational from 1956. At East and South-East of the island, there is a large colony of Emperor penguins (Aptenodytes forsteri) on fast ice. The Haswell Island is a unique breeding site for almost all breeding bird species in East Antarctica including the: Antarctic petrel (Talassoica antarctica), Antarctic fulmar (Fulmarus glacioloides), Cape petrel (Daption capense), Snow petrel (Pagodroma nivea), Wilson’s storm petrel (Oceanites oceanicus), South polar skua (Catharacta maccormicki), Lonnberg skua Catharacta antarctica lonnbergi and Adelie penguin (Pygoscelis adeliae). The Area supports five species of pinnipeds, including the Ross seal (Ommatophoca rossii) which falls in the protected species category. ATCM VIII (Oslo, 1975) approved its designation as SSSI 7 on the aforementioned grounds after a proposal by the USSR. Map 1 shows the location of the Haswell Islands (except Vkhodnoy Island), Mirny Station, and logistic activity sites. It was renamed and renumbered as ASPA No. 127 by Decision 1 (2002). -
Energetics of the Antarctic Silverfish, Pleuragramma Antarctica, from the Western Antarctic Peninsula
Chapter 8 Energetics of the Antarctic Silverfish, Pleuragramma antarctica, from the Western Antarctic Peninsula Eloy Martinez and Joseph J. Torres Abstract The nototheniid Pleuragramma antarctica, commonly known as the Antarctic silverfish, dominates the pelagic fish biomass in most regions of coastal Antarctica. In this chapter, we provide shipboard oxygen consumption and nitrogen excretion rates obtained from P. antarctica collected along the Western Antarctic Peninsula and, combining those data with results from previous studies, develop an age-dependent energy budget for the species. Routine oxygen consumption of P. antarctica fell in the midrange of values for notothenioids, with a mean of 0.057 ± −1 −1 0.012 ml O2 g h (χ ± 95% CI). P. antarctica showed a mean ammonia-nitrogen excretion rate of 0.194 ± 0.042 μmol NH4-N g−1 h−1 (χ ± 95% CI). Based on current data, ingestion rates estimated in previous studies were sufficient to cover the meta- bolic requirements over the year classes 0–10. Metabolism stood out as the highest energy cost to the fish over the age intervals considered, initially commanding 89%, gradually declining to 67% of the annual energy costs as the fish aged from 0 to 10 years. Overall, the budget presented in the chapter shows good agreement between ingested and combusted energy, and supports the contention of a low-energy life- style for P. antarctica, but it also resembles that of other pelagic species in the high percentage of assimilated energy devoted to metabolism. It differs from more tem- perate coastal pelagic fishes in its large investment in reproduction and its pattern of slow steady growth throughout a relatively long lifespan. -
2019 Weddell Sea Expedition
Initial Environmental Evaluation SA Agulhas II in sea ice. Image: Johan Viljoen 1 Submitted to the Polar Regions Department, Foreign and Commonwealth Office, as part of an application for a permit / approval under the UK Antarctic Act 1994. Submitted by: Mr. Oliver Plunket Director Maritime Archaeology Consultants Switzerland AG c/o: Maritime Archaeology Consultants Switzerland AG Baarerstrasse 8, Zug, 6300, Switzerland Final version submitted: September 2018 IEE Prepared by: Dr. Neil Gilbert Director Constantia Consulting Ltd. Christchurch New Zealand 2 Table of contents Table of contents ________________________________________________________________ 3 List of Figures ___________________________________________________________________ 6 List of Tables ___________________________________________________________________ 8 Non-Technical Summary __________________________________________________________ 9 1. Introduction _________________________________________________________________ 18 2. Environmental Impact Assessment Process ________________________________________ 20 2.1 International Requirements ________________________________________________________ 20 2.2 National Requirements ____________________________________________________________ 21 2.3 Applicable ATCM Measures and Resolutions __________________________________________ 22 2.3.1 Non-governmental activities and general operations in Antarctica _______________________________ 22 2.3.2 Scientific research in Antarctica __________________________________________________________ -
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. -
Moult of the Emperor Penguin: Travel, Location, and Habitat Selection
MARINE ECOLOGY PROGRESS SERIES Vol. 204: 269–277, 2000 Published October 5 Mar Ecol Prog Ser Moult of the emperor penguin: travel, location, and habitat selection G. L. Kooyman1,*, E. C. Hunke2, S. F. Ackley3, R. P. van Dam1, G. Robertson4 1Scholander Hall, 0204, Scripps Institution of Oceanography, La Jolla, California 92093, USA 2MS-B216, Los Alamos National Laboratory, Los Alamos, New Mexico 87545, USA 3Cold Regions Research and Engineering Laboratory 72 Lyme Rd., Hanover, New Hampshire 03755, USA 4Australian Antarctic Division, Channel Highway, Kingston 7050, Tasmania, Australia ABSTRACT: All penguins except emperors Aptenodytes forsteri and Adelies Pygoscelis adeliae moult on land, usually near the breeding colonies. These 2 Antarctic species typically moult some- where in the pack-ice. Emperor penguins begin their moult in early summer when the pack-ice cover of the Antarctic Ocean is receding. The origin of the few moulting birds seen by observers on pass- ing ships is unknown, and the locations are often far from any known colonies. We attached satellite transmitters to 12 breeding adult A. forsteri from western Ross Sea colonies before they departed the colony for the last time before moulting. In addition, we surveyed some remote areas of the Weddell Sea north and east of some large colonies that are located along the southern and western borders of this sea. The tracked birds moved at a rate of nearly 50 km d–1 for more than 1000 km over 30 d to reach areas of perennially consistent pack-ice. Almost all birds traveled to the eastern Ross Sea and western Amundsen Sea.