Ice Flow Velocity Mapping of East Antarctica from 1963 to 1989
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PROGETTO ANTARTIDE Rapporto Sulla Campagna Antartica Estate Australe 1996
PROGRAMMA NAZIONALE DI RICERCHE IN ANTARTIDE Rapporto sulla Campagna Antartica Estate Australe 1996 - 97 Dodicesima Spedizione PROGETTO ANTARTIDE ANT 97/02 PROGRAMMA NAZIONALE DI RICERCHE IN ANTARTIDE Rapporto sulla Campagna Antartica Estate Australe 1996 - 97 Dodicesima Spedizione A cura di J. Mϋller, T. Pugliatti, M.C. Ramorino, C.A. Ricci PROGETTO ANTARTIDE ENEA - Progetto Antartide Via Anguillarese,301 c.p.2400,00100 Roma A.D. Tel.: 06-30484816,Fax:06-30484893,E-mail:[email protected] I N D I C E Premessa SETTORE 1 - EVOLUZIONE GEOLOGICA DEL CONTINENTE ANTARTICO E DELL'OCEANO MERIDIONALE Area Tematica 1a Evoluzione Geologica del Continente Antartico Progetto 1a.1 Evoluzione del cratone est-antartico e del margine paleo-pacifico del Gondwana.3 Progetto 1a.2 Evoluzione mesozoica e cenozoica del Mare di Ross ed aree adiacenti..............11 Progetto 1a.3 Magmatismo Cenozoico del margine occidentale antartico..................................17 Progetto 1a.4 Cartografia geologica, geomorfologica e geofisica ...............................................18 Area Tematica 1b-c Margini della Placca Antartica e Bacini Periantartici Progetto 1b-c.1 Strutture crostali ed evoluzione cenozoica della Penisola Antartica e del margine coniugato cileno ......................................................................................25 Progetto 1b-c.2 Indagini geofisiche sul sistema deposizionale glaciale al margine pacifico della Penisola Antartica.........................................................................................42 -
Late Pleistocene Interactions of East and West Antarctic Ice-Flow Regim.Es: Evidence From
J oumal oJ Glaciology, r·ol. 42, S o. 142, 1996 Late Pleistocene interactions of East and West Antarctic ice-flow regim.es: evidence from. the McMurdo Ice Shelf THO}'IAS B . KELLOGG, TERRY H UG HES AND D .\VJD!\ E. KELLOGG Depa rtmen t oJ Geo logical Sciences alld Institute for QJlatemm) Studies, UI/ iversilj' oJ ,\Jail/ e, Orono , "faine 04469. [j.S. A. ABSTRACT. \Ve prese nt new interpreta ti ons of d eglacia tion in M cMurdo Sound and the wes tern R oss Sea, with o bservati onall y based reconstructi ons of interacti ons between Eas t a nd \Ves t Antarcti c ice a t the las t glacial maximum (LG YI ), 16 000, 12 000, 8000 a nd 4000 BP. At the LG M , East Anta rctic ice fr om Muloek Glacier spli t; one bra nch turned wes tward south of R oss Tsland b ut the other bra nch rounded R oss Island before fl owing south"'est in to lVf cMurdo Sound. This fl ow regime, constrained b y a n ice sa ddle north of R n. s Isla nd, is consisten t wi th the reconstruc ti on of Stuiyer a nd others (198I a ) . After the LG lVI. , grounding-line retreat was m ost ra pid in areas \~ ' i th greates t wa ter d epth, es pecially a long th e Vic toria Land coast. By 12 000 BP , the ice-flow regime in :'.1cMurdo Sound c ha nged to through-flowing l\1ulock G lacier ice, with lesse r contributions from K oettlitz, Blue a nd F crra r Glaciers, because the formcr ice saddle north of R oss Isla nd was repl aced by a d om e. -
S41467-018-05625-3.Pdf
ARTICLE DOI: 10.1038/s41467-018-05625-3 OPEN Holocene reconfiguration and readvance of the East Antarctic Ice Sheet Sarah L. Greenwood 1, Lauren M. Simkins2,3, Anna Ruth W. Halberstadt 2,4, Lindsay O. Prothro2 & John B. Anderson2 How ice sheets respond to changes in their grounding line is important in understanding ice sheet vulnerability to climate and ocean changes. The interplay between regional grounding 1234567890():,; line change and potentially diverse ice flow behaviour of contributing catchments is relevant to an ice sheet’s stability and resilience to change. At the last glacial maximum, marine-based ice streams in the western Ross Sea were fed by numerous catchments draining the East Antarctic Ice Sheet. Here we present geomorphological and acoustic stratigraphic evidence of ice sheet reorganisation in the South Victoria Land (SVL) sector of the western Ross Sea. The opening of a grounding line embayment unzipped ice sheet sub-sectors, enabled an ice flow direction change and triggered enhanced flow from SVL outlet glaciers. These relatively small catchments behaved independently of regional grounding line retreat, instead driving an ice sheet readvance that delivered a significant volume of ice to the ocean and was sustained for centuries. 1 Department of Geological Sciences, Stockholm University, Stockholm 10691, Sweden. 2 Department of Earth, Environmental and Planetary Sciences, Rice University, Houston, TX 77005, USA. 3 Department of Environmental Sciences, University of Virginia, Charlottesville, VA 22904, USA. 4 Department -
Washington Geology, V, 21, No. 2, July 1993
WASHINGTON GEOLOGY Washington Department of Natural Resources, Division of Geology and Earth Resources Vol. 21, No. 2, July 1993 , Mount Baker volcano from the northeast. Bagley Lakes, in the foreground, are on a Pleistocene recessional moraine that is now the parking lot for Mount Baker Ski Area. Just below Sherman Peak, an erosional remnant on the left skyline, is Boulder Glacier. Park and Rainbow Glaciers share the area below the main summit (Grant Peak, 10,778 ft) . Boulder, Park, and Rainbow Glaciers drain into Baker Lake, which is out of the photo on the left. Mazama Glacier forms under the ridge that extends to Hadley Peak on the right. (See related article, p. 3 and Fig. 2, p. 5.) Table Mountain, the flat area just above and to the right of center, is a truncated lava flow. Lincoln Peak is just visible over the right shoulder of Mount Baker. Photo taken in 1964. In This Issue: Current behavior of glaciers in the North Cascades and its effect on regional water supplies, p. 3; Radon potential of Washington, p. 11; Washington areas selected for water quality assessment, p. 14; The changing role of cartogra phy in OGER-Plugging into the Geographic Information System, p. 15; Additions to the library, p. 16. Revised State Surface Minin!Jf Act-1993 by Raymond Lasmanls WASHINGTON The 1993 regular session of the 53rd Le:gislature passed a major revision of the surface mine reclamation act as En GEOLOGY grossed Second Substitute Senate Bill No. 5502. The new law takes effect on July 1, 1993. Both environmental groups and surface miners testified in favor of the act. -
ICE FLOW VELOCITY MAPPING in EAST ANTARCTICA USING HISTORICAL IMAGES from 1960S to 1980S: RECENT PROGRESS
The International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences, Volume XLIII-B3-2021 XXIV ISPRS Congress (2021 edition) ICE FLOW VELOCITY MAPPING IN EAST ANTARCTICA USING HISTORICAL IMAGES FROM 1960s TO 1980s: RECENT PROGRESS S. Luo 1,2, Y. Cheng 1,2, Z. Li 1,2, Y. Wang 1,2, K. Wang 1,2, X. Wang 1,2, G. Qiao 1,2, W. Ye 1,2, Y. Li 1,2, M. Xia 1,2, X. Yuan 1,2, Y. Tian 1,2, X. Tong 1,2, R. Li 1,2* 1Center for Spatial Information Science and Sustainable Development Applications, Tongji University, 1239 Siping Road, Shanghai, China - (shulei, chengyuan_1994, tjwkl, wxfjj620, qiaogang, menglianxia, 1996yuanxiaohan, tianyixiang, xhtong, rli) @tongji.edu.cn, (zhenli_0324, yanjunli_1995) @outlook.com, [email protected], [email protected] 2 College of Surveying and Geo-Informatics, Tongji University, 1239 Siping Road, Shanghai, China Commission TCIII, WG III/9 KEY WORDS: East Antarctica, Ice Flow, Historical Image, Velocity Validation, Ice Flux, Mass Balance ABSTRACT: Recent research indicates that the estimated elevation changes and associated mass balance in East Antarctica are of some degree of uncertainty; a light accumulation has occurred in its vast inland regions, while mass loss in Wilkes Land appears significant. It is necessary to study the mass change trend in the context of a long period of the East Antarctic Ice Sheet (EAIS). The input-output method based on surface ice flow velocity and ice thickness is one of the most important ways to estimate the mass balance, which can provide longer-term knowledge of mass balance because of the availability of the early satellites in 1960s. -
Report November 1996
International Council of Scientific Unions No13 report November 1996 Contents SCAR Group of Specialists on Global Change and theAntarctic (GLOCHANT) Report of bipolar meeting of GLOCHANT / IGBP-PAGES Task Group 2 on Palaeoenvironments from Ice Cores (PICE), 1995 1 Report of GLOCHANTTask Group 3 on Ice Sheet Mass Balance and Sea-Level (ISMASS), 1995 6 Report of GLOCHANT IV meeting, 1996 16 GLOCHANT IV Appendices 27 Published by the SCIENTIFIC COMMITTEE ON ANTARCTIC RESEARCH at the Scott Polar Research Institute, Cambridge, United Kingdom INTERNATIONAL COUNCIL OF SCIENTIFIC UNIONS SCIENTIFIC COMMITfEE ON ANTARCTIC RESEARCH SCAR Report No 13, November 1996 Contents SCAR Group of Specialists on Global Change and theAntarctic (GLOCHANT) Report of bipolar meeting of GLOCHANT / IGBP-PAGES Task Group 2 on Palaeoenvironments from Ice Cores (PICE), 1995 1 Report of GLOCHANT Task Group 3 on Ice Sheet Mass Balance and Sea-Level (ISMASS), 1995 6 Report of GLOCHANT IV meeting, 1996 16 GLOCHANT IV Appendices 27 Published by the SCIENTIFIC COMMITfEE ON ANT ARCTIC RESEARCH at the Scott Polar Research Institute, Cambridge, United Kingdom SCAR Group of Specialists on Global Change and the Antarctic (GLOCHANT) Report of the 1995 bipolar meeting of the GLOCHANT I IGBP-PAGES Task Group 2 on Palaeoenvironments from Ice Cores. (PICE) Boston, Massachusetts, USA, 15-16 September; 1995 Members ofthe PICE Group present Dr. D. Raynaud (Chainnan, France), Dr. D. Peel (Secretary, U.K.}, Dr. J. White (U.S.A.}, Mr. V. Morgan (Australia), Dr. V. Lipenkov (Russia), Dr. J. Jouzel (France), Dr. H. Shoji (Japan, proxy for Prof. 0. Watanabe). Apologies: Prof. 0. -
1 Compiled by Mike Wing New Zealand Antarctic Society (Inc
ANTARCTIC 1 Compiled by Mike Wing US bulldozer, 1: 202, 340, 12: 54, New Zealand Antarctic Society (Inc) ACECRC, see Antarctic Climate & Ecosystems Cooperation Research Centre Volume 1-26: June 2009 Acevedo, Capitan. A.O. 4: 36, Ackerman, Piers, 21: 16, Vessel names are shown viz: “Aconcagua” Ackroyd, Lieut. F: 1: 307, All book reviews are shown under ‘Book Reviews’ Ackroyd-Kelly, J. W., 10: 279, All Universities are shown under ‘Universities’ “Aconcagua”, 1: 261 Aircraft types appear under Aircraft. Acta Palaeontolegica Polonica, 25: 64, Obituaries & Tributes are shown under 'Obituaries', ACZP, see Antarctic Convergence Zone Project see also individual names. Adam, Dieter, 13: 6, 287, Adam, Dr James, 1: 227, 241, 280, Vol 20 page numbers 27-36 are shared by both Adams, Chris, 11: 198, 274, 12: 331, 396, double issues 1&2 and 3&4. Those in double issue Adams, Dieter, 12: 294, 3&4 are marked accordingly. Adams, Ian, 1: 71, 99, 167, 229, 263, 330, 2: 23, Adams, J.B., 26: 22, Adams, Lt. R.D., 2: 127, 159, 208, Adams, Sir Jameson Obituary, 3: 76, A Adams Cape, 1: 248, Adams Glacier, 2: 425, Adams Island, 4: 201, 302, “101 In Sung”, f/v, 21: 36, Adamson, R.G. 3: 474-45, 4: 6, 62, 116, 166, 224, ‘A’ Hut restorations, 12: 175, 220, 25: 16, 277, Aaron, Edwin, 11: 55, Adare, Cape - see Hallett Station Abbiss, Jane, 20: 8, Addison, Vicki, 24: 33, Aboa Station, (Finland) 12: 227, 13: 114, Adelaide Island (Base T), see Bases F.I.D.S. Abbott, Dr N.D. -
Nunataks As Barriers to Ice Flow: Implications for Palaeo Ice-Sheet
https://doi.org/10.5194/tc-2021-173 Preprint. Discussion started: 11 June 2021 c Author(s) 2021. CC BY 4.0 License. Nunataks as barriers to ice flow: implications for palaeo ice-sheet reconstructions Martim Mas e Braga1,2, Richard Selwyn Jones3,4, Jennifer C. H. Newall1,2, Irina Rogozhina5, Jane L. Andersen6, Nathaniel A. Lifton7,8, and Arjen P. Stroeven1,2 1Geomorphology & Glaciology, Department of Physical Geography, Stockholm University, Stockholm, Sweden 2Bolin Centre for Climate Research, Stockholm University, Stockholm, Sweden 3Department of Geography, Durham University, Durham, UK 4School of Earth, Atmosphere and Environment, Monash University, Melbourne, Australia 5Department of Geography, Norwegian University of Science and Technology, Trondheim, Norway 6Department of Geoscience, Aarhus University, Aarhus, Denmark 7Department of Earth, Atmospheric, and Planetary Sciences, Purdue University, West Lafayette, USA 8Department of Physics and Astronomy, Purdue University, West Lafayette, USA Correspondence: Martim Mas e Braga ([email protected]) Abstract. Numerical models predict that discharge from the polar ice sheets will become the largest contributor to sea level rise over the coming centuries. However, the predicted amount of ice discharge and associated thinning depends on how well ice sheet models reproduce glaciological processes, such as ice flow in regions of large topographic relief, where ice flows around bedrock summits (i.e. nunataks) and through outlet glaciers. The ability of ice sheet models to capture long-term ice loss is 5 best tested by comparing model simulations against geological data. A benchmark for such models is ice surface elevation change, which has been constrained empirically at nunataks and along margins of outlet glaciers using cosmogenic exposure dating. -
Mm^Umamm a N E W S B U L L E T I N
mm^umamm 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 ■ H.M.N.Z.S. ENDEAVOUR about to tie up in Winter Quarters Bay. On right, Vince's Cross and Scott's hut. J. Calvert photo. MARCH, 1965 AUSTRALIA Winter and Summer bases Scott- S u m m e r b a s e o n l y t H a l l e f t "cton NEW ZEALAND Transferred base Wilkes UStcAust Temporarily non -operational. .KSyowa TASMANIA , Campbell I. (N-l) , ^ V - r . ^ ^ N . AT // \$ 5«|* Pasar'C ^rd(i/.sA . *"Vp»tuk , N |(I/.«.AJ i - S c o t t ( U . 5 J i t - A N T A R. M^ciJ ^>cwj a fi/V wX " < S M a u d **$P -Marion I. ttM DRAWN BY DEPARTMENT OF LANDS 1 SURVEY WELLINGTON, NEW ZEALAND, MAR.I9l»4- 1 " . " E D I T I O N m ilHl^IBS^IKB^k (Successor to "Antarctic News Bulletin") MARCH, 1965 Editor: L. B. Quartermain, M.A., 1 Ariki Road, Wellington, E.2, New Zealand. Business Communications, Subscriptions, etc., to: Secretary, New Zealand Antarctic Society, P.O. Box 2110, Wellington, N.Z. CONTENTS EXPEDITIONS New Zealand The Central Nimrod Glacier Geological Expedition: M. G. Laird Victoria University Research in Ice-free Areas: W. M. Prebble The D-region Project: J. B. Gregory France United States First Leg of Traverse Australia Belgium-Holland U.S.S.R South Africa Argentina United Kingdom Chile Japan Sub-Antarctic Islands British South Georgia Expedition Big Ben Conquered Special Articles: Hallett Closed Antarctic Stations—I. -
Mmymtmmx* a N E W S B U L L E T I N
mmymtmmx* A N E W S B U L L E T I N published b y t h e NEW ZEALAND ANTARCTIC SOCIETY 7i^ ■ I l , U.S.N.S. MAUMEE DOCKED AT McMURDO. Official U.S. Navy photo. Vol. 5, No. 9 MARCH, 1970 AUSTRALIA y»L/ E 'T w / ) WELLINGTONI -SCHRISTCHURCH I NEW ZEALAND TASMANIA VOSS DEPENDED ^ <k \^«**V t\ / Byrd(US)* ANTARCTICA, \ / l\ Ah Pliteiu <US)0<' Alferej Sobnl (Arj) < J,Gtncnl Belfrano \ / W N G M A L ) 0 \ j H . l l t y B a y ( U K ) / ^ < / (USSR)X%*r)\»»A-^ %^D "VVAY) I * aXA Tsplent."xsfi&** ^J#/&**?&- (USSM ^V^X^^ ^'^ 0r< DRAWN BY DEPARTMENT OF LANDS * SURVEY WELLINGTON. NEW ZEALAND. AUG IM9 3rd EDITION MLiHTOA IB ©INKD" (Successor to "Antarctic News Bulletin") Vol. 5. No. 9 57th ISSUE MARCH, 1970 Contributions, enquiries, etc., to the Acting Editor, C/- P.O. Box 2110, Wellington. Business Communications, Subscriptions, etc., to: Secretary, New Zealand Antarctic Society, P.O. Box 2110, Wellington, N.Z. CONTENTS ■ EXPEDITIONS New Zealand The First Year at Vanda Station: S. K. Cutfield U.S.A. France Belgium Australia U.S.S.R. South Africa Japan 389, 406 United Kingdom Argentina Sub-Antarctic Islands Flights to the Pole Antarctic Bookshelf Co-operation in Antarctic Research Antarctic Tourism 403 March, 1970 BAD WEATHER HAMPERS ACTIVITIES AT NEW ZEALAND STATIONS At Scott Base. Vanda Station and in the field, a very extensive summer programme was carried through despite much stormy weather and in the face of unexpected transport and other difficulties. Leader Bruce Willis reported late in AT TERRA NOVA BAY December: Unfortunately not as much ground as "With such a splendid start to the expected was covered by the four-man month as the celebration of the tenth DS1R geological party at Terro Nova anniversary of the signing of the Ant Bay owing to a combination of deep arctic Treaty, it seemed that we were soft snow and warm weather, but never set for a period of concerted activity. -
Te Puna Patiotio Antarctic Research Centre
Te Puna Patiotio Antarctic Research Centre Annual Review 2020 IMPROVING UNDERSTANDING OF ANTARCTIC CLIMATE AND ICE SHEET PROCESSES, AND THEIR IMPACT ON NEW ZEALAND AND THE EARTH SYSTEM CONTENTS Skelton Glacier, Antarctica - Photo: Shaun Eaves Impacts by Numbers 2 Director’s Summary 4 Research Outcomes 6 Science Drilling Office 19 Teaching & Supervision 20 Significant Events 22 Financial Summary 30 Antarctic Research Centre Annual Review 2020 Designed and edited by: Michelle Dow Our Engagement 34 Contributions from: Nancy Bertler, Ruzica Dadic, Warren Dickinson, Michelle Dow, Gavin Dunbar, Nick Golledge, Huw Horgan, Publications & Conferences 38 Liz Keller, Richard Levy, Darcy Mandeno, Rob McKay, Tim Naish, Jamey Stutz, Lauren Vargo, Oliver Wigmore, and Holly Winton. Our People 44 Cover Image: Peter Barrett, Skelton Neve, Antarctica, 1970/71 - Photo: John McPherson 2019 65 year 1 Prime Minister’s legacy New Zealander Science Prize of Emeritus Professor Peter Barrett Ruzica Dadic, joins the world’s celebrated during a awarded to the “Melting Ice largest international polar two day symposium. and Rising Seas” team led by research expedition, MOSAiC. the ARC. 10 8 200 $6.3 $800 $18 times modellers people million thousand thousand USD more likely to get extreme from three institutes working attended the 17th S.T. Lee in revenue obtained by ARC added to the ARC Endowed awarded to Rob McKay for the glacier melt with human- together to provide future Lecture in person and online. in 2020, 75% from externally Development Fund from the Asahiko Taira Scientific Ocean induced climate change. projections on Earth’s climate funded grants. PM Science Prize award and Drilling Research Prize. -
Holocene Thinning of Darwin and Hatherton Glaciers, Antarctica, and Implications for Grounding-Line Retreat in the Ross Sea
The Cryosphere, 15, 3329–3354, 2021 https://doi.org/10.5194/tc-15-3329-2021 © Author(s) 2021. This work is distributed under the Creative Commons Attribution 4.0 License. Holocene thinning of Darwin and Hatherton glaciers, Antarctica, and implications for grounding-line retreat in the Ross Sea Trevor R. Hillebrand1,a, John O. Stone1, Michelle Koutnik1, Courtney King2, Howard Conway1, Brenda Hall2, Keir Nichols3, Brent Goehring3, and Mette K. Gillespie4 1Department of Earth and Space Sciences, University of Washington, Seattle, WA 98195, USA 2School of Earth and Climate Science and Climate Change Institute, University of Maine, Orono, ME 04469, USA 3Department of Earth and Environmental Sciences, Tulane University, New Orleans, LA 70118, USA 4Faculty of Engineering and Science, Western Norway University of Applied Sciences, Sogndal, 6856, Norway anow at: Fluid Dynamics and Solid Mechanics Group, Los Alamos National Laboratory, Los Alamos, NM 87545, USA Correspondence: Trevor R. Hillebrand ([email protected]) Received: 8 December 2020 – Discussion started: 15 December 2020 Revised: 4 May 2021 – Accepted: 27 May 2021 – Published: 20 July 2021 Abstract. Chronologies of glacier deposits in the available records from the mouths of other outlet glaciers Transantarctic Mountains provide important constraints in the Transantarctic Mountains, many of which thinned by on grounding-line retreat during the last deglaciation in hundreds of meters over roughly a 1000-year period in the the Ross Sea. However, between Beardmore Glacier and Early Holocene. The deglaciation histories of Darwin and Ross Island – a distance of some 600 km – the existing Hatherton glaciers are best matched by a steady decrease in chronologies are generally sparse and far from the modern catchment area through the Holocene, suggesting that Byrd grounding line, leaving the past dynamics of this vast region and/or Mulock glaciers may have captured roughly half of largely unconstrained.