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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. -
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. -
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. -
Topographic Control on Post-LGM Groundings of the West Antarctic
Louisiana State University LSU Digital Commons LSU Master's Theses Graduate School 3-25-2018 Topographic Control on Post-LGM Groundings of the West Antarctic Ice Sheet in the Whales Deep Basin, Eastern Ross Sea Matthew aD nielson Louisiana State University and Agricultural and Mechanical College, [email protected] Follow this and additional works at: https://digitalcommons.lsu.edu/gradschool_theses Part of the Geology Commons, Geomorphology Commons, and the Glaciology Commons Recommended Citation Danielson, Matthew, "Topographic Control on Post-LGM Groundings of the West Antarctic Ice Sheet in the Whales Deep Basin, Eastern Ross Sea" (2018). LSU Master's Theses. 4629. https://digitalcommons.lsu.edu/gradschool_theses/4629 This Thesis is brought to you for free and open access by the Graduate School at LSU Digital Commons. It has been accepted for inclusion in LSU Master's Theses by an authorized graduate school editor of LSU Digital Commons. For more information, please contact [email protected]. TOPOGRAPHIC CONTROL ON POST-LGM GROUNDINGS OF THE WEST ANTARCTIC ICE SHEET IN THE WHALES DEEP BASIN, EASTERN ROSS SEA A Thesis Submitted to the Graduate Faculty of Louisiana State University Agricultural and Mechanical College In the partial fulfillment of the requirements for the degree of Master in Science In The Department of Geology and Geophysics by Matthew Danielson B.S., Texas A&M, 2015 May 2018 TABLE OF CONTENTS ABSTRACT………………………………………………………………………………………………………………………………….ii INTRODUCTION…………………………………………………………………………..…………………………………………….1 -
I!Ij 1)11 U.S
u... I C) C) co 1 USGS 0.. science for a changing world co :::2: Prepared in cooperation with the Scott Polar Research Institute, University of Cambridge, United Kingdom Coastal-change and glaciological map of the (I) ::E Bakutis Coast area, Antarctica: 1972-2002 ;::+' ::::r ::J c:r OJ ::J By Charles Swithinbank, RichardS. Williams, Jr. , Jane G. Ferrigno, OJ"" ::J 0.. Kevin M. Foley, and Christine E. Rosanova a :;:,..... CD ~ (I) I ("') a Geologic Investigations Series Map I- 2600- F (2d ed.) OJ ~ OJ '!; :;:, OJ ::J <0 co OJ ::J a_ <0 OJ n c; · a <0 n OJ 3 OJ "'C S, ..... :;:, CD a:r OJ ""a. (I) ("') a OJ .....(I) OJ <n OJ n OJ co .....,...... ~ C) .....,0 ~ b 0 C) b C) C) T....., Landsat Multispectral Scanner (MSS) image of Ma rtin and Bea r Peninsulas and Dotson Ice Shelf, Bakutis Coast, CT> C) An tarctica. Path 6, Row 11 3, acquired 30 December 1972. ? "T1 'N 0.. co 0.. 2003 ISBN 0-607-94827-2 U.S. Department of the Interior 0 Printed on rec ycl ed paper U.S. Geological Survey 9 11~ !1~~~,11~1!1! I!IJ 1)11 U.S. DEPARTMENT OF THE INTERIOR TO ACCOMPANY MAP I-2600-F (2d ed.) U.S. GEOLOGICAL SURVEY COASTAL-CHANGE AND GLACIOLOGICAL MAP OF THE BAKUTIS COAST AREA, ANTARCTICA: 1972-2002 . By Charles Swithinbank, 1 RichardS. Williams, Jr.,2 Jane G. Ferrigno,3 Kevin M. Foley, 3 and Christine E. Rosanova4 INTRODUCTION areas Landsat 7 Enhanced Thematic Mapper Plus (ETM+)), RADARSAT images, and other data where available, to compare Background changes over a 20- to 25- or 30-year time interval (or longer Changes in the area and volume of polar ice sheets are intri where data were available, as in the Antarctic Peninsula). -
Getz Ice Shelf Melt Enhanced by Freshwater Discharge from Beneath the West Antarctic Ice Sheet
Edinburgh Research Explorer Getz Ice Shelf melt enhanced by freshwater discharge from beneath the West Antarctic Ice Sheet Citation for published version: Wei, W, Blankenship, DD, Greenbaum, JS, Gourmelen, N, Dow, CF, Richter, TG, Greene, CA, Young, DA, Lee, S, Kim, T, Lee, WS & Assmann, KM 2020, 'Getz Ice Shelf melt enhanced by freshwater discharge from beneath the West Antarctic Ice Sheet', Cryosphere, vol. 14, no. 4, pp. 1399-1408. https://doi.org/10.5194/tc- 14-1399-2020 Digital Object Identifier (DOI): 10.5194/tc-14-1399-2020 Link: Link to publication record in Edinburgh Research Explorer Document Version: Publisher's PDF, also known as Version of record Published In: Cryosphere Publisher Rights Statement: © Author(s) 2020. This work is distributed under the Creative Commons Attribution 4.0 License. General rights Copyright for the publications made accessible via the Edinburgh Research Explorer is retained by the author(s) and / or other copyright owners and it is a condition of accessing these publications that users recognise and abide by the legal requirements associated with these rights. Take down policy The University of Edinburgh has made every reasonable effort to ensure that Edinburgh Research Explorer content complies with UK legislation. If you believe that the public display of this file breaches copyright please contact [email protected] providing details, and we will remove access to the work immediately and investigate your claim. Download date: 10. Oct. 2021 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. -
November 1960 I Believe That the Major Exports of Antarctica Are Scientific Data
JIET L S. Antarctic Projects OfficerI November 1960 I believe that the major exports of Antarctica are scientific data. Certainly that is true now and I think it will be true for a long time and I think these data may turn out to be of vastly, more value to all mankind than all of the mineral riches of the continent and the life of the seas that surround it. The Polar Regions in Their Relation to Human Affairs, by Laurence M. Gould (Bow- man Memorial Lectures, Series Four), The American Geographiql Society, New York, 1958 page 29.. I ITOJ TJM II IU1viBEt 3 IToveber 1960 CONTENTS 1 The First Month 1 Air Operations 2 Ship Oper&tions 3 Project MAGNET NAF McMurdo Sounds October Weather 4 4 DEEP FREEZE 62 Volunteers Solicited A DAY AT TEE SOUTH POLE STATION, by Paul A Siple 5 in Antarctica 8 International Cooperation 8 Foreign Observer Exchange Program 9 Scientific Exchange Program NavyPrograrn 9 Argentine Navy-U.S. Station Cooperation 9 10 Other Programs 10 Worlds Largest Aircraft in Antarctic Operation 11 ANTARCTICA, by Emil Schulthess The Antarctic Treaty 11 11 USNS PRIVATE FRANIC 3. FETRARCA (TAK-250) 1961 Scientific Leaders 12 NAAF Little Rockford Reopened 13 13 First Flight to Hallett Station 14 Simmer Operations Begin at South Pole First DEEP FREEZE 61 Airdrop 14 15 DEEP FREEZE 61 Cargo Antarctic Real Estate 15 Antarctic Chronology,. 1960-61 16 The 'AuuOiA vises to t):iank Di * ?a]. A, Siple for his artj.ole Wh.4b begins n page 5 Matera1 for other sections of bhis issue was drawn from radio messages and fran information provided bY the DepBr1nozrt of State the Nat0na1 Academy , of Soienoes the NatgnA1 Science Fouxidation the Office 6f NAval Re- search, and the U, 3, Navy Hydziograpbio Offioe, Tiis, issue of tie 3n oovers: i16, aótivitiès o events 11 Novóiber The of the Uxitéd States. -
USGS Open-File Report 2007-1047, Short Research Paper
U.S.Geological Survey and The National Acadamies; USGS OF-2007-1047, Short Research Paper 084; doi:10.3133/of2007-1047.srp084 Differences in ice retreat across Pine Island Bay, West Antarctica, since the Last Glacial Maximum: Indications from multichannel seismic reflection data G. Uenzelmann-Neben,1 K. Gohl,1 R.D. Larter,2 and P. Schlüter1 1Alfred Wegener Institute for Polar and Marine Research, Am Alten Hafen 26, 27568 Bremerhaven, Germany ([email protected], [email protected], [email protected]) 2British Antarctic Survey, Highcross, Madingley Road, Cambridge CB3 0ET, UK ([email protected]) Abstract An understanding of the glacial history of Pine Island Bay (PIB) is essential for refining models of the future stability of the West Antarctic Ice Sheet (WAIS). New multichannel seismic reflection data from inner PIB are interpreted in context of previously published reconstructions for the retreat history in this area since the Last Glacial Maximum. Differences in the behavior of the ice sheet during deglaciation are shown to exist for the western and eastern parts of PIB. While we can identify only a thin veneer of sedimentary deposits in western PIB, eastern PIB shows sedimentary layers ≤ 400 msTWT. This is interpreted as a result of differences in ice retreat: a fast ice retreat in western PIB accompanied by rapid basal melting led to production of large meltwater streams, a slower ice retreat in eastern PIB is most probably the result of smaller drainage basins resulting in less meltwater production. Citation: Uenzelmann-Neben, G., K. Gohl, R.D. Larter, and P. -
Download Itinerary
26 Days The Ross Sea Starting 15 Feb 2022 Get ready to be inspired. FROM $45,950 PER PERSON, TWIN SHARE Travelling with Inspiring Vacations allows you to explore the wonders of the world in a variety of different ways. We have partnered with a worldwide network of local travel experts to bring you culturally unique and delightfully unforgettable travel experiences. Whether it is meandering through narrow canyons by rail, cruising the idyllic waters of the Mediterranean or touring through t... Book Now TOUR ITINERARY The information provided in this document is subject to change and may be affected by unforeseen events outside the control of Inspiring Vacations. Where changes to your itinerary or bookings occur, appropriate advice or instructions will be sent to your email address. Call 1300 88 66 88 Email [email protected] www.inspiringvacations.com Page 1 TOUR ITINERARY DAY 1 Destination Santiago Meals included Dinner Hotel 5 Hotel in Santiago, or similar On arrival at your hotel in Santiago, you will enjoy an afternoon at leisure to explore the city before your early start tomorrow. DAY 2 Destination Santiago Ushuaia - Embarkation Meals included Breakfast, Lunch, Dinner Le Commandant Charcot, Prestige Stateroom Deck 7, or Cruise similar Capital of Argentina's Tierra del Fuego province, Ushuaia is considered the gateway to the White Continent and the South Pole. Nicknamed “El fin del mundo” by the Argentinian people, this city at the end of the world nestles in the shelter of mountains surrounded by fertile plains that the wildlife seem to have chosen as the ultimate sanctuary. -
Glacier Change Along West Antarctica's
The Cryosphere, 12, 2461–2479, 2018 https://doi.org/10.5194/tc-12-2461-2018 © Author(s) 2018. This work is distributed under the Creative Commons Attribution 4.0 License. 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 1School of GeoSciences, University of Edinburgh, Edinburgh, EH8 9XP, UK 2Department of Earth & Space Sciences, University of Washington, Seattle, WA 98195-1310, USA 3NERC British Antarctic Survey, Cambridge, CB3 0ET, UK Correspondence: Robert Bingham ([email protected]) Received: 27 November 2017 – Discussion started: 29 January 2018 Revised: 29 June 2018 – Accepted: 3 July 2018 – Published: 26 July 2018 Abstract. Over the past 20 years satellite remote sensing tively, our findings underscore the importance of spatial and has captured significant downwasting of glaciers that drain inter-decadal variability in atmosphere and ocean interac- the West Antarctic Ice Sheet into the ocean, particularly tions in moderating glaciological change around Antarctica. 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 1 Introduction monitored. Here, we use optical satellite imagery to track grounding-line migration along the Marie Byrd Land Sec- Recent in situ and satellite remote sensing campaigns have tor between 2003 and 2015, and compare observed changes played an important role in constraining the relative roles of with ICESat and CryoSat-2-derived surface elevation and ice, ocean and atmosphere interactions responsible for con- thickness change records. -
Seismic Stratigraphic Record of the Amundsen Sea Embayment Shelf from Pre-Glacial to Recent Times: Evidence for a Dynamic
See discussions, stats, and author profiles for this publication at: https://www.researchgate.net/publication/277390716 Seismic stratigraphic record of the Amundsen Sea Embayment shelf from pre-glacial to recent times: Evidence for a dynamic... Article in Marine Geology · October 2013 DOI: 10.1016/j.margeo.2013.06.011 CITATIONS READS 19 42 10 authors, including: Karsten Gohl Gerhard Kuhn Alfred Wegener Institute Helmholtz Centre fo… Alfred Wegener Institute Helmholtz Centre fo… 175 PUBLICATIONS 2,115 CITATIONS 390 PUBLICATIONS 4,111 CITATIONS SEE PROFILE SEE PROFILE Frank Nitsche Columbia University 92 PUBLICATIONS 1,485 CITATIONS SEE PROFILE Some of the authors of this publication are also working on these related projects: ADMAP-2: the next-generation magnetic anomaly map of the Antarctic View project Changing sediment provenance in the Indian Ocean-Atlantic Ocean gateway during the Pliocene in relation to current dynamics and variations in continental climate View project All content following this page was uploaded by Karsten Gohl on 02 June 2015. The user has requested enhancement of the downloaded file. Marine Geology 344 (2013) 115–131 Contents lists available at ScienceDirect Marine Geology journal homepage: www.elsevier.com/locate/margeo Seismic stratigraphic record of the Amundsen Sea Embayment shelf from pre-glacial to recent times: Evidence for a dynamic West Antarctic ice sheet Karsten Gohl a,⁎, Gabriele Uenzelmann-Neben a, Robert D. Larter b, Claus-Dieter Hillenbrand b, Katharina Hochmuth a, Thomas Kalberg a, Estella Weigelt -
Your Cruise the Ross
The Ross Sea From 16/02/2022 From Ushuaia Ship: LE COMMANDANT CHARCOT to 12/03/2022 to Ushuaia Sailing the Ross Sea means discovering one of the most extreme and conserved universes in the Antarctic. Partially occupied by the Ross Ice Shelf, the largest ice platform in Antarctica , this immense bay located several hundred kilometres from theSouth Pole, is considered as the“ last ocean”, the last intact marine ecosystem and the largest marine sanctuary since 2016. Here, the cold is more intense, the wind more powerful, the ice more impressive, and the scenery more spectacular… In the heart of this polar Garden of Eden, where the ice shelf turns into icebergs, you will encounter prodigious fauna, as well assurrealist landscapes, with infinite shades of blue and stunning reliefs. Antarctic petrels, Minke whales, orcas and seals are at home here, as are very large Overnight in Santiago + flight Santiago/Ushuaia + transfers + flight Ushuaia/Santiago colonies of Adelie and emperor penguins. We are privileged guests in these extreme lands where we are at the mercy of weather and ice conditions. Our navigation will be determined by the type of ice we come across; as the coastal ice must be preserved, we will take this factor into account from day to day in our itineraries. The sailing schedule and any landings, activities and wildlife encounters are subject to weather and ice conditions. These experiences are unique and vary with each departure. The Captain and the Expedition Leader will make every effort to ensure that your experience is as rich as possible, while respecting safety instructions and regulations imposed by the IAATO.