The Antarctic Sun, January 7, 2007
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'Landscapes of Exploration' Education Pack
Landscapes of Exploration February 11 – 31 March 2012 Peninsula Arts Gallery Education Pack Cover image courtesy of British Antarctic Survey Cover image: Launch of a radiosonde meteorological balloon by a scientist/meteorologist at Halley Research Station. Atmospheric scientists at Rothera and Halley Research Stations collect data about the atmosphere above Antarctica this is done by launching radiosonde meteorological balloons which have small sensors and a transmitter attached to them. The balloons are filled with helium and so rise high into the Antarctic atmosphere sampling the air and transmitting the data back to the station far below. A radiosonde meteorological balloon holds an impressive 2,000 litres of helium, giving it enough lift to climb for up to two hours. Helium is lighter than air and so causes the balloon to rise rapidly through the atmosphere, while the instruments beneath it sample all the required data and transmit the information back to the surface. - Permissions for information on radiosonde meteorological balloons kindly provided by British Antarctic Survey. For a full activity sheet on how scientists collect data from the air in Antarctica please visit the Discovering Antarctica website www.discoveringantarctica.org.uk and select resources www.discoveringantarctica.org.uk has been developed jointly by the Royal Geographical Society, with IBG0 and the British Antarctic Survey, with funding from the Foreign and Commonwealth Office. The Royal Geographical Society (with IBG) supports geography in universities and schools, through expeditions and fieldwork and with the public and policy makers. Full details about the Society’s work, and how you can become a member, is available on www.rgs.org All activities in this handbook that are from www.discoveringantarctica.org.uk will be clearly identified. -
Rapid Transport of Ash and Sulfate from the 2011 Puyehue-Cordón
PUBLICATIONS Journal of Geophysical Research: Atmospheres RESEARCH ARTICLE Rapid transport of ash and sulfate from the 2011 10.1002/2017JD026893 Puyehue-Cordón Caulle (Chile) eruption Key Points: to West Antarctica • Ash and sulfate from the June 2011 Puyehue-Cordón Caulle eruption were Bess G. Koffman1,2 , Eleanor G. Dowd1 , Erich C. Osterberg1 , David G. Ferris1, deposited in West Antarctica 3 3 3,4 1 • Depositional phasing and duration Laura H. Hartman , Sarah D. Wheatley , Andrei V. Kurbatov , Gifford J. Wong , 5 6 3,4 4 suggest rapid transport through the Bradley R. Markle , Nelia W. Dunbar , Karl J. Kreutz , and Martin Yates troposphere • Ash/sulfate phasing, ash size 1Department of Earth Sciences, Dartmouth College, Hanover, New Hampshire, USA, 2Now at Department of Geology, Colby distributions, and geochemistry College, Waterville, Maine, USA, 3Climate Change Institute, University of Maine, Orono, Maine, USA, 4School of Earth and distinguish this midlatitude eruption Climate Sciences, University of Maine, Orono, Maine, USA, 5Department of Earth and Space Sciences, University of from low- and high-latitude eruptions Washington, Seattle, Washington, USA, 6New Mexico Bureau of Geology and Mineral Resources, Socorro, New Mexico, USA Supporting Information: • Supporting Information S1 Abstract The Volcanic Explosivity Index 5 eruption of the Puyehue-Cordón Caulle volcanic complex (PCC) in central Chile, which began 4 June 2011, provides a rare opportunity to assess the rapid transport and Correspondence to: deposition of sulfate and ash from a midlatitude volcano to the Antarctic ice sheet. We present sulfate, B. G. Koffman, [email protected] microparticle concentrations of fine-grained (~5 μm diameter) tephra, and major oxide geochemistry, which document the depositional sequence of volcanic products from the PCC eruption in West Antarctic snow and shallow firn. -
Integrated Tephrochonology Copyedited
U.S. Geological Survey and The National Academies; USGS OFR-2007-xxxx, Extended Abstract.yyy, 1- Integrated tephrochronology of the West Antarctic region- Implications for a potential tephra record in the West Antarctic Ice Sheet (WAIS) Divide Ice Core N.W. Dunbar,1 W.C. McIntosh,1 A.V. Kurbatov,2 and T.I Wilch 3 1NMGB/EES Department, New Mexico Tech, Socorro NM, 87801, USA ( [email protected] , [email protected] ) 2Climate Change Institute 303 Bryand Global Sciences Center, Orono, ME, 04469, USA ([email protected]) 3Department of Geological Sciences, Albion College, Albion MI, 49224, USA ( [email protected] ) Summary Mount Berlin and Mt. Takahe, two West Antarctica volcanic centers have produced a number of explosive, ashfall generating eruptions over the past 500,000 yrs. These eruptions dispersed volcanic ash over large areas of the West Antarctic ice sheet. Evidence of these eruptions is observed at two blue ice sites (Mt. Waesche and Mt. Moulton) as well as in the Siple Dome and Byrd (Palais et al., 1988) ice cores. Geochemical correlations between tephra sampled at the source volcanoes, at blue ice sites, and in the Siple Dome ice core suggest that at least some of the eruptions covered large areas of the ice sheet with a volcanic ash, and 40 Ar/ 39 Ar dating of volcanic material provides precise timing when these events occurred. Volcanic ash from some of these events expected to be found in the WAIS Divide ice core, providing chronology and inter-site correlation. Citation: Dunbar, N.W., McIntosh, W.C., Kurbatov, A., and T.I Wilch (2007), Integrated tephrochronology of the West Antarctic region- Implications for a potential tephra record in the West Antarctic Ice Sheet (WAIS) Divide Ice Core, in Antarctica: A Keystone in a Changing World – Online Proceedings of the 10 th ISAES X, edited by A. -
Halley Research Station
British Antarctic Survey Halley Research Station Halley V The Station alley V took six years from being conceived at the The Laws Building comprises three sections, a Hdrawing board to its commissioning in February services/technical support area, living area and sleeping 1992. It is novel in that the three main buildings sit 4 m quarters. Diesel engines provide electrical power and above the snow on independent jackable steel platforms. their waste heat warms the buildings and melts snow to The largest is the Laws Building (accommodation) which provide water.The living area includes a darkroom, is 59 m long, 14.6 m wide and 3 m high.The smaller lounge, library, dining room, kitchen, computer room, base Simpson Building (meteorology and ozone studies) and commander’s office, communications room, recreation Piggott Building (upper atmospheric sciences) house room, storage areas, washrooms, a hospital and a surgery. specialist laboratories.The height of the platforms above There are 20 two-person bedrooms.The winter station the ice shelf affects the local wind turbulence and the complement ranges from 14 to 18 and includes scientists, build-up of drifting snow. Each summer the platforms are support staff and a doctor. Summer visitors are raised an average of 1m to compensate for the accommodated in the Drewry Building,a self-contained accumulated snowfall. In addition, the supporting legs can building on skis that is towed to a fresh site each year to be realigned to correct for distortion caused by avoid burial, and also serves as an emergency refuge.The differential movement in the flow of the ice shelf beneath. -
The Centenary of the Scott Expedition to Antarctica and of the United Kingdom’S Enduring Scientific Legacy and Ongoing Presence There”
Debate on 18 October: Scott Expedition to Antarctica and Scientific Legacy This Library Note provides background reading for the debate to be held on Thursday, 18 October: “the centenary of the Scott Expedition to Antarctica and of the United Kingdom’s enduring scientific legacy and ongoing presence there” The Note provides information on Antarctica’s geography and environment; provides a history of its exploration; outlines the international agreements that govern the territory; and summarises international scientific cooperation and the UK’s continuing role and presence. Ian Cruse 15 October 2012 LLN 2012/034 House of Lords Library Notes are compiled for the benefit of Members of the House of Lords and their personal staff, to provide impartial, politically balanced briefing on subjects likely to be of interest to Members of the Lords. Authors are available to discuss the contents of the Notes with the Members and their staff but cannot advise members of the general public. Any comments on Library Notes should be sent to the Head of Research Services, House of Lords Library, London SW1A 0PW or emailed to [email protected]. Table of Contents 1.1 Geophysics of Antarctica ....................................................................................... 1 1.2 Environmental Concerns about the Antarctic ......................................................... 2 2.1 Britain’s Early Interest in the Antarctic .................................................................... 4 2.2 Heroic Age of Antarctic Exploration ....................................................................... -
The Human Footprint of the IPY 2007-2008 in Antarctica
IP 86 Agenda Item: ATCM 10 CEP 5 Presented by: ASOC Original: English The Human Footprint of the IPY 2007-2008 in Antarctica Attachments: 1 IP 86 The Human Footprint of the IPY 2007-2008 in Antarctica Information Paper Submitted by ASOC to ATCM XXX (CEP Agenda Item 5; ATCM Agenda Item 10) Abstract The International Polar Year (IPY) 2007-2008 is ambitious in scope and scale. At least 350 research activities with Antarctic or bipolar focus will take place during the IPY period of March 2007-March 2009. 82% (or 286) of them are planning to conduct fieldwork in Antarctica (Fig. 1a). 105 activities are planning to leave behind physical infrastructure, ranging from extensive arrays of instrumentation to new facilities. The Antarctic Treaty Secretariat’s database of environmental impact assessments lists only 7 completed assessments that are directly linked to science or logistics that are planned for the IPY. During the IPY, research and its corresponding logistical support activity will intensify around existing centers of research, such as the Antarctic Peninsula, Dronning Maud Land, Prydz Bay and the Weddell and Ross Seas. A number of large-scale research activities has also been planned in areas which have been hitherto seldom accessed, including the Gamburtsev Mountains in East Antarctica, the Amundsen Sea embayment and the West Antarctic ice sheet and subglacial lakes (Fig. 2). Many of them have been planned as the precursor of long-term research programs. In view of the ensemble of the research projects that have been endorsed, the IPY is likely to lead to: ! a direct increase in human activity in Antarctica; ! an increase in infrastructure in Antarctica; ! an increased pressure on Antarctica’s wilderness values; ! an increased level of interest in Antarctica, which can indirectly generate more activities other than scientific research, adding to the current trend of rapid growth and diversification of Antarctic tourism. -
U.S. Advance Exchange of Operational Information, 2005-2006
Advance Exchange of Operational Information on Antarctic Activities for the 2005–2006 season United States Antarctic Program Office of Polar Programs National Science Foundation Advance Exchange of Operational Information on Antarctic Activities for 2005/2006 Season Country: UNITED STATES Date Submitted: October 2005 SECTION 1 SHIP OPERATIONS Commercial charter KRASIN Nov. 21, 2005 Depart Vladivostok, Russia Dec. 12-14, 2005 Port Call Lyttleton N.Z. Dec. 17 Arrive 60S Break channel and escort TERN and Tanker Feb. 5, 2006 Depart 60S in route to Vladivostok U.S. Coast Guard Breaker POLAR STAR The POLAR STAR will be in back-up support for icebreaking services if needed. M/V AMERICAN TERN Jan. 15-17, 2006 Port Call Lyttleton, NZ Jan. 24, 2006 Arrive Ice edge, McMurdo Sound Jan 25-Feb 1, 2006 At ice pier, McMurdo Sound Feb 2, 2006 Depart McMurdo Feb 13-15, 2006 Port Call Lyttleton, NZ T-5 Tanker, (One of five possible vessels. Specific name of vessel to be determined) Jan. 14, 2006 Arrive Ice Edge, McMurdo Sound Jan. 15-19, 2006 At Ice Pier, McMurdo. Re-fuel Station Jan. 19, 2006 Depart McMurdo R/V LAURENCE M. GOULD For detailed and updated schedule, log on to: http://www.polar.org/science/marine/sched_history/lmg/lmgsched.pdf R/V NATHANIEL B. PALMER For detailed and updated schedule, log on to: http://www.polar.org/science/marine/sched_history/nbp/nbpsched.pdf SECTION 2 AIR OPERATIONS Information on planned air operations (see attached sheets) SECTION 3 STATIONS a) New stations or refuges not previously notified: NONE b) Stations closed or refuges abandoned and not previously notified: NONE SECTION 4 LOGISTICS ACTIVITIES AFFECTING OTHER NATIONS a) McMurdo airstrip will be used by Italian and New Zealand C-130s and Italian Twin Otters b) McMurdo Heliport will be used by New Zealand and Italian helicopters c) Extensive air, sea and land logistic cooperative support with New Zealand d) Twin Otters to pass through Rothera (UK) upon arrival and departure from Antarctica e) Italian Twin Otter will likely pass through South Pole and McMurdo. -
The WAIS Divide Deep Ice Core WD2014 Chronology – Part 2: Annual-Layer Counting (0–31 Ka BP)
Clim. Past, 12, 769–786, 2016 www.clim-past.net/12/769/2016/ doi:10.5194/cp-12-769-2016 © Author(s) 2016. CC Attribution 3.0 License. The WAIS Divide deep ice core WD2014 chronology – Part 2: Annual-layer counting (0–31 ka BP) Michael Sigl1,2, Tyler J. Fudge3, Mai Winstrup3,a, Jihong Cole-Dai4, David Ferris5, Joseph R. McConnell1, Ken C. Taylor1, Kees C. Welten6, Thomas E. Woodruff7, Florian Adolphi8, Marion Bisiaux1, Edward J. Brook9, Christo Buizert9, Marc W. Caffee7,10, Nelia W. Dunbar11, Ross Edwards1,b, Lei Geng4,5,12,d, Nels Iverson11, Bess Koffman13, Lawrence Layman1, Olivia J. Maselli1, Kenneth McGwire1, Raimund Muscheler8, Kunihiko Nishiizumi6, Daniel R. Pasteris1, Rachael H. Rhodes9,c, and Todd A. Sowers14 1Desert Research Institute, Nevada System of Higher Education, Reno, NV 89512, USA 2Laboratory for Radiochemistry and Environmental Chemistry, Paul Scherrer Institute, 5232 Villigen, Switzerland 3Department of Earth and Space Sciences, University of Washington, Seattle, WA 98195, USA 4Department of Chemistry and Biochemistry, South Dakota State University, Brookings, SD 57007, USA 5Dartmouth College Department of Earth Sciences, Hanover, NH 03755, USA 6Space Science Laboratory, University of California, Berkeley, Berkeley, CA 94720, USA 7Department of Physics and Astronomy, PRIME Laboratory, Purdue University, West Lafayette, IN 47907, USA 8Department of Geology, Lund University, 223 62 Lund, Sweden 9College of Earth, Ocean, and Atmospheric Sciences, Oregon State University, Corvallis, OR 97331, USA 10Department of Earth, Atmospheric, -
Inhomogeneity of the Surface Air Temperature Record from Halley, Antarctica
15 JUNE 2021 K I N G E T A L . 4771 Inhomogeneity of the Surface Air Temperature Record from Halley, Antarctica a a a a a a JOHN C. KING, JOHN TURNER, STEVE COLWELL, HUA LU, ANDREW ORR, TONY PHILLIPS, a a J. SCOTT HOSKING, AND GARETH J. MARSHALL a British Antarctic Survey, Cambridge, United Kingdom (Manuscript received 25 September 2020, in final form 10 March 2021) ABSTRACT: Commencing in 1956, observations made at Halley Research Station in Antarctica provide one of the longest continuous series of near-surface temperature observations from the Antarctic continent. Since few other records of comparable length are available, the Halley record has been used extensively in studies of long-term Antarctic climate variability and change. The record does not, however, come from a single location but is a composite of observations from a sequence of seven stations, all situated on the Brunt Ice Shelf, that range from around 10 to 50 km in distance from the coast. Until now, it has generally been assumed that temperature data from all of these stations could be combined into a single composite record with no adjustment. Here, we examine this assumption of homogeneity. Application of a statistical changepoint algorithm to the composite record detects a sudden cooling associated with the move from Halley IV to Halley V station in 1992. We show that this temperature step is consistent with local temperature gradients measured by a network of automatic weather stations and with those simulated by a high-resolution atmospheric model. These temperature gradients are strongest in the coastal region and result from the onshore advection of maritime air. -
Antarctic Treaty
ANTARCTIC TREATY REPORT OF THE NORWEGIAN ANTARCTIC INSPECTION UNDER ARTICLE VII OF THE ANTARCTIC TREATY FEBRUARY 2009 Table of Contents Table of Contents ............................................................................................................................................... 1 1. Introduction ................................................................................................................................................... 2 1.1 Article VII of the Antarctic Treaty .................................................................................................................... 2 1.2 Past inspections under the Antarctic Treaty ................................................................................................... 2 1.3 The 2009 Norwegian Inspection...................................................................................................................... 3 2. Summary of findings ...................................................................................................................................... 6 2.1 General ............................................................................................................................................................ 6 2.2 Operations....................................................................................................................................................... 7 2.3 Scientific research .......................................................................................................................................... -
West Antarctic Ice Sheet Divide Ice Core Climate, Ice Sheet History, Cryobiology
WAIS DIVIDE SCIENCE COORDINATION OFFICE West Antarctic Ice Sheet Divide Ice Core Climate, Ice Sheet History, Cryobiology A GUIDE FOR THE MEDIA AND PUBLIC Field Season 2011-2012 WAIS (West Antarctic Ice Sheet) Divide is a United States deep ice coring project in West Antarctica funded by the National Science Foundation (NSF). WAIS Divide’s goal is to examine the last ~100,000 years of Earth’s climate history by drilling and recovering a deep ice core from the ice divide in central West Antarctica. Ice core science has dramatically advanced our understanding of how the Earth’s climate has changed in the past. Ice cores collected from Greenland have revolutionized our notion of climate variability during the past 100,000 years. The WAIS Divide ice core will provide the first Southern Hemisphere climate and greenhouse gas records of comparable time resolution and duration to the Greenland ice cores enabling detailed comparison of environmental conditions between the northern and southern hemispheres, and the study of greenhouse gas concentrations in the paleo-atmosphere, with a greater level of detail than previously possible. The WAIS Divide ice core will also be used to test models of WAIS history and stability, and to investigate the biological signals contained in deep Antarctic ice cores. 1 Additional copies of this document are available from the project website at http://www.waisdivide.unh.edu Produced by the WAIS Divide Science Coordination Office with support from the National Science Foundation, Office of Polar Programs. 2 Contents -
BAS Science Summaries 2018-2019 Antarctic Field Season
BAS Science Summaries 2018-2019 Antarctic field season BAS Science Summaries 2018-2019 Antarctic field season Introduction This booklet contains the project summaries of field, station and ship-based science that the British Antarctic Survey (BAS) is supporting during the forthcoming 2018/19 Antarctic field season. I think it demonstrates once again the breadth and scale of the science that BAS undertakes and supports. For more detailed information about individual projects please contact the Principal Investigators. There is no doubt that 2018/19 is another challenging field season, and it’s one in which the key focus is on the West Antarctic Ice Sheet (WAIS) and how this has changed in the past, and may change in the future. Three projects, all logistically big in their scale, are BEAMISH, Thwaites and WACSWAIN. They will advance our understanding of the fragility and complexity of the WAIS and how the ice sheets are responding to environmental change, and contributing to global sea-level rise. Please note that only the PIs and field personnel have been listed in this document. PIs appear in capitals and in brackets if they are not present on site, and Field Guides are indicated with an asterisk. Non-BAS personnel are shown in blue. A full list of non-BAS personnel and their affiliated organisations is shown in the Appendix. My thanks to the authors for their contributions, to MAGIC for the field sites map, and to Elaine Fitzcharles and Ali Massey for collating all the material together. Thanks also to members of the Communications Team for the editing and production of this handy summary.