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Geophysical Research Letters
Geophysical Research Letters RESEARCH LETTER Variation in the Distribution and Properties of Circumpolar 10.1029/2018GL077430 Deep Water in the Eastern Amundsen Sea, on Seasonal Key Points: Timescales, Using Seal-Borne Tags • In the eastern Amundsen Sea, the CDW layer is thicker in winter than in summer and contains more heat Helen K. W. Mallett1 , Lars Boehme2 , Mike Fedak2 , Karen J. Heywood1 , and salt 1 3,4 • On isopycnals, CDW is cooler and David P. Stevens , and Fabien Roquet fresher in winter, likely the result of a rising core of offshelf CDW changing 1Centre for Ocean and Atmospheric Sciences, University of East Anglia, Norwich, UK, 2Sea Mammal Research Unit, CDW properties onshelf University of St Andrews, St Andrews, UK, 3Department of Meteorology, Stockholm University, Stockholm, Sweden, • Farther south, in PIB, this seasonality 4Department of Marine Sciences, University of Gothenburg, Gothenburg, Sweden is less pronounced, likely the result of mixing as the PIB gyre recirculates CDW of different ages Abstract In the Amundsen Sea, warm saline Circumpolar Deep Water (CDW) crosses the continental shelf toward the vulnerable West Antarctic ice shelves, contributing to their basal melting. Supporting Information: Due to lack of observations, little is known about the spatial and temporal variability of CDW, • Supporting Information S1 particularly seasonally. A new data set of 6,704 seal tag temperature and salinity profiles in the easternmost trough between February and December 2014 reveals a CDW layer on average 49 dbar thicker in late Correspondence to: winter (August to October) than in late summer (February to April), the reverse seasonality of that seen K. -
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. -
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HNiTflRCiTilC A NEWS BULLETIN published quarterly by the NEW ZEALAND ANTARCTIC SOCIETY (INC) ,m — i * Halley, the British Antarctic Survey's station on the Brunt Ice Shelf, Coats Land,, was rebuilt last season for the third time since 1956-57. This picture taken in March shows one of the four wooden tubes, each of which houses a two-storey building, under construction in a pre-shaped and compacted snow hollow. BAS Copyngh! Registered at Post Office Headquarters, Vol. 10, No. 2 Wellington, New Zealand, as a magazine. SOUTH GEORGIA -.. SOUTH SANDWICH Is «C*2K SOUTH ORKNEY Is x \ 6SignyluK //o Orcadas arg SOUTH AMERICA / /\ ^ Borga T"^00Molodezhnaya \^' 4 south , * /weooEii \ ft SA ' r-\ *r\USSR --A if SHETLAND ,J£ / / ^^Jf ORONMIIDROWNING MAUD LAND' E N D E R B Y \ ] > * \ /' _ "iV**VlX" JN- S VDruzhnaya/General /SfA/ S f Auk/COATS ' " y C O A TBelirano SLd L d l arg L A N D p r \ ' — V&^y D««hjiaya/cenera.1 Beld ANTARCTIC •^W^fCN, uSS- fi?^^ /K\ Mawson \ MAC ROBERTSON LAN0\ \ *usi \ /PENINSULA' ^V^/^CRp^e J ^Vf (set mjp Mow) C^j V^^W^gSobralARG - Davis aust L Siple USA Amundsen-Scon OUEEN MARY LAND flMimy ELLSWORTH , U S A / ^ U S S R ') LAND °Vos1okussR/ r». / f c i i \ \ MARIE BYRO fee Shelf V\ . IAND WILKES LAND Scon ROSS|N2i? SEA jp>r/VICTORIAIj^V .TERRE ,; ' v / I ALAND n n \ \^S/ »ADEUL. n f i i f / / GEORGE V Ld .m^t Dumom d'Urville iranu Leningradskayra V' USSR,.'' \ -------"'•BAlLENYIs^ ANTARCTIC PENINSULA 1 Teniente Matienzo arc 2 Esperanza arg 3 Almirante Brown arg 4 Petrel arg 5 Decepcion arg 6 Vicecomodoro Marambio arg ' ANTARCTICA 7 Ariuro Prat chile 500 1000 Miles 8 Bernardo O'Higgms chile 9 Presidente Frei chile - • 1000 Kilomnre 10 Stonington I. -
Article Is Available On- J.: the International Bathymetric Chart of the Southern Ocean Line At
The Cryosphere, 14, 1399–1408, 2020 https://doi.org/10.5194/tc-14-1399-2020 © Author(s) 2020. This work is distributed under the Creative Commons Attribution 4.0 License. Getz Ice Shelf melt enhanced by freshwater discharge from beneath the West Antarctic Ice Sheet Wei Wei1, Donald D. Blankenship1, Jamin S. Greenbaum1, Noel Gourmelen2, Christine F. Dow3, Thomas G. Richter1, Chad A. Greene4, Duncan A. Young1, SangHoon Lee5, Tae-Wan Kim5, Won Sang Lee5, and Karen M. Assmann6,a 1Institute for Geophysics and Department of Geological Sciences, Jackson School of Geosciences, University of Texas at Austin, Austin, Texas, USA 2School of GeoSciences, University of Edinburgh, Edinburgh, UK 3Department of Geography and Environmental Management, University of Waterloo, Waterloo, Ontario, Canada 4Jet Propulsion Laboratory, California Institute of Technology, Pasadena, California, USA 5Korea Polar Research Institute, Incheon, South Korea 6Department of Earth Sciences, University of Gothenburg, Gothenburg, Sweden apresent address: Institute of Marine Research, Tromsø, Norway Correspondence: Wei Wei ([email protected]) Received: 18 July 2019 – Discussion started: 26 July 2019 Revised: 8 March 2020 – Accepted: 10 March 2020 – Published: 27 April 2020 Abstract. Antarctica’s Getz Ice Shelf has been rapidly thin- 1 Introduction ning in recent years, producing more meltwater than any other ice shelf in the world. The influx of fresh water is The Getz Ice Shelf (Getz herein) in West Antarctica is over known to substantially influence ocean circulation and bi- 500 km long and 30 to 100 km wide; it produces more fresh ological productivity, but relatively little is known about water than any other source in Antarctica (Rignot et al., 2013; the factors controlling basal melt rate or how basal melt is Jacobs et al., 2013), and in recent years its melt rate has spatially distributed beneath the ice shelf. -
NJDARM: Collection Guide
NJDARM: Collection Guide - NEW JERSEY STATE ARCHIVES COLLECTION GUIDE Record Group: Governor Franklin Murphy (1846-1920; served 1902-1905) Series: Correspondence, 1902-1905 Accession #: 1989.009, Unknown Series #: S3400001 Guide Date: 1987 (JK) Volume: 6 c.f. [12 boxes] Box 1 | Box 2 | Box 3 | Box 4 | Box 5 | Box 6 | Box 7 | Box 8 | Box 9 | Box 10 | Box 11 | Box 12 Contents Explanatory Note: All correspondence is either to or from the Governor's office unless otherwise stated. Box 1 1. Elections, 1901-1903. 2. Primary election reform, 1902-1903. 3. Requests for interviews, 1902-1904 (2 files). 4. Taxation, 1902-1904. 5. Miscellaneous bills before State Legislature and U.S. Congress, 1902 (2 files). 6. Letters of congratulation, 1902. 7. Acknowledgements to letters recommending government appointees, 1902. 8. Fish and game, 1902-1904 (3 files). 9. Tuberculosis Sanatorium Commission, 1902-1904. 10. Invitations to various functions, April - July 1904. 11. Requests for Governor's autograph and photograph, 1902-1904. 12. Princeton Battle Monument, 1902-1904. 13. Forestry, 1901-1905. 14. Estate of Imlay Clark(e), 1902. 15. Correspondence re: railroad passes & telegraph stamps, 1902-1903. 16. Delinquent Corporations, 1901-1905 (2 files). 17. Robert H. McCarter, Attorney General, 1903-1904. 18. New Jersey Reformatories, 1902-1904 (6 files). Box 2 19. Reappointment of Minister Powell to Haiti, 1901-1902. 20. Corporations and charters, 1902-1904. 21. Miscellaneous complaint letters, December 1901-1902. file:///M|/highpoint/webdocs/state/darm/darm2011/guides/guides%20for%20pdf/s3400001.html[5/16/2011 9:33:48 AM] NJDARM: Collection Guide - 22. Joshua E. -
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. -
ROLF E. PETERS and MARY ANN CHANCE INTRODUCTION D.D
"The Lost Years"—1902-1904 ROLF E. PETERS and MARY ANN CHANCE ABSTRACT: Cyrus Lerner, an investigative lawyer, produced a report on chiropractic that identified the period of 1902-1904 as "The Lost Years" of chiropractic. This paper is an attempt to fill in that period based on later published research and our own investigations. INDEXTERMSiMeSH: CHIROPRACTIC; HISTORICAL ARTICLE. Chiropr J Aust 2003; 33: 2-10. INTRODUCTION Clarence N. Flick, DC, of St Albans, NY established the Thus the D.D. Palmer era—with D.D. as the sole authority Foundation for Health Research Inc., which was chartered in teaching chiropractic at his school—ended when he decided New York on 20 January 1950. The Foundation believed that to leave for Califomia in 1902, apparently not giving any 36 years of failed efforts to achieve licensure for the profession reason. in the state of New York were due to the difficult-to-challenge perception that the chiropractic claim was without scientific B.J. PALMER: HOLDING THE BAG basis and that it represented a potential danger to public health. With the disappearance of D.D. Palmer from Davenport, The Foundation hired Cyrus M. Lerner, a prominent B.J. Palmer was left in sole charge. Prior to his graduation, investigative attorney, to explore every fact bearing on the B.J. had already practised in Manistique, Michigan, from 20 historical basis and development of chiropractic. He had full June 1901 to 31 September 1901 He lodged at the home of access to the archives at the Palmer School, as well as G. Keils, on River Street.^ His first patient, seen on 20 June newspaper and court records, and had several interviews with 1901, was Dr. -
Glacier Change Along West Antarctica's Marie Byrd Land Sector
Glacier change along West Antarctica’s Marie Byrd Land Sector and links to inter-decadal atmosphere-ocean variability Frazer D.W. Christie1, Robert G. Bingham1, Noel Gourmelen1, Eric J. Steig2, Rosie R. Bisset1, Hamish D. Pritchard3, Kate Snow1 and Simon F.B. Tett1 5 1School of GeoSciences, University of Edinburgh, Edinburgh, UK 2Department of Earth & Space Sciences, University of Washington, Seattle, USA 3British Antarctic Survey, Cambridge, UK Correspondence to: Frazer D.W. Christie ([email protected]) Abstract. Over the past 20 years satellite remote sensing has captured significant downwasting of glaciers that drain the West 10 Antarctic Ice Sheet into the ocean, particularly across the Amundsen Sea Sector. Along the neighbouring Marie Byrd Land Sector, situated west of Thwaites Glacier to Ross Ice Shelf, glaciological change has been only sparsely monitored. Here, we use optical satellite imagery to track grounding-line migration along the Marie Byrd Land Sector between 2003 and 2015, and compare observed changes with ICESat and CryoSat-2-derived surface elevation and thickness change records. During the observational period, 33% of the grounding line underwent retreat, with no significant advance recorded over the remainder 15 of the ~2200 km long coastline. The greatest retreat rates were observed along the 650-km-long Getz Ice Shelf, further west of which only minor retreat occurred. The relative glaciological stability west of Getz Ice Shelf can be attributed to a divergence of the Antarctic Circumpolar Current from the continental-shelf break at 135° W, coincident with a transition in the morphology of the continental shelf. Along Getz Ice Shelf, grounding-line retreat reduced by 68% during the CryoSat-2 era relative to earlier observations. -
Late Quaternary Volcanic Activity in Marie Byrd Land: Potential 40Ar/39Ar-Dated Time Horizons in West Antarctic Ice and Marine Cores
Late Quaternary volcanic activity in Marie Byrd Land: Potential 40Ar/39Ar-dated time horizons in West Antarctic ice and marine cores T. I. Wilch* Department of Geological Sciences, Albion College, Albion, Michigan 49224 W. C. McIntosh Department of Earth and Environmental Science, New Mexico Institute of Mining and Technology, and New Mexico Bureau of Mines and Mineral Resources, Socorro, New Mexico 87801 N. W. Dunbar New Mexico Bureau of Mines and Mineral Resources, Socorro, New Mexico 87801 ABSTRACT More than 12 40Ar/39Ar-dated tephra lay- ies is to determine the basal age of the ice sheet. ers, exposed in bare ice on the summit ice cap The 1968 Byrd Station ice core in the West Late Quaternary volcanic activity at three of Mount Moulton, 30 km from their inferred Antarctic Ice Sheet has an inferred basal age of major alkaline composite volcanoes in Marie source at Mount Berlin, range in age from 492 only 74 ka (Hammer et al., 1994). The exten- Byrd Land, West Antarctica, is dominated by to 15 ka. These englacial tephra layers provide sive lateral flow of ice from the ice divide area explosive eruptions, many capable of deposit- a minimum age of 492 ka for the oldest iso- to Byrd Station may have removed or disturbed ing ash layers as regional time-stratigraphic topically dated ice in West Antarctica. This much of the basal ice record. Consequently, the horizons in the West Antarctic Ice Sheet and well-dated section of locally derived glacial ice 74 ka date of the Byrd core provides only a in Southern Ocean marine sediments. -
A Possible Adélie Penguin Sub-Colony on Fast Ice by Cape Crozier, Antarctica
Antarctic Science page 1 of 6 (2019) © Antarctic Science Ltd 2019 doi:10.1017/S095410201900018X A possible Adélie penguin sub-colony on fast ice by Cape Crozier, Antarctica MICHELLE LARUE1,2, DAVID ILES3, SARA LABROUSSE3, LEO SALAS4, GRANT BALLARD4, DAVID AINLEY5 and BENJAMIN SAENZ6 1Department of Earth Sciences, 116 Church St SE, University of Minnesota, Minneapolis, MN 55455, USA 2Department of Geography, 724 Julius von Haast Building, University of Canterbury, Christchurch 8041, New Zealand 3Woods Hole Oceanographic Institution, Mailstop 50, Woods Hole, MA 02543, USA 4Point Blue Conservation Science, 3820 Cypress Drive #11, Petaluma, CA 94954, USA 5H.T. Harvey and Associates Ecological Consultants, 983 University Avenue Building D, Los Gatos, CA 95032, USA 6Acoustics Consulting, Berkeley, CA, USA [email protected] Abstract: Adélie penguins are renowned for their natal philopatry on land-based colonies, requiring small pebbles to be used for nests. We report on an opportunistic observation via aerial survey, where hundreds of Adélie penguins were documented displaying nesting behaviours on fast ice ∼3 km off the coast of Cape Crozier, which is one of the largest colonies in the world. We counted 426 Adélie penguins engaging in behaviours of pair formation, spacing similarly to normal nest distributions and lying in divots in the ice that looked like nests. On our first visit, it was noticed that the guano stain was bright pink, consistent with krill consumption, but had shifted to green over the course of ∼2 weeks, indicating that the birds were fasting (a behaviour consistent with egg incubation). However, eggs were not observed. We posit four hypotheses that may explain the proximate causes of this behaviour and caution against future high-resolution satellite imagery interpretation due to the potential for confusing ice-nesting Adélie penguins with the presence of emperor penguin colonies.