Antarctic Research Station
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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. -
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 ....................................................................... -
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 .......................................................................................................................................... -
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. -
Public Information Leaflet HISTORY.Indd
British Antarctic Survey History The United Kingdom has a long and distinguished record of scientific exploration in Antarctica. Before the creation of the British Antarctic Survey (BAS), there were many surveying and scientific expeditions that laid the foundations for modern polar science. These ranged from Captain Cook’s naval voyages of the 18th century, to the famous expeditions led by Scott and Shackleton, to a secret wartime operation to secure British interests in Antarctica. Today, BAS is a world leader in polar science, maintaining the UK’s long history of Antarctic discovery and scientific endeavour. The early years Britain’s interests in Antarctica started with the first circumnavigation of the Antarctic continent by Captain James Cook during his voyage of 1772-75. Cook sailed his two ships, HMS Resolution and HMS Adventure, into the pack ice reaching as far as 71°10' south and crossing the Antarctic Circle for the first time. He discovered South Georgia and the South Sandwich Islands although he did not set eyes on the Antarctic continent itself. His reports of fur seals led many sealers from Britain and the United States to head to the Antarctic to begin a long and unsustainable exploitation of the Southern Ocean. Image: Unloading cargo for the construction of ‘Base A’ on Goudier Island, Antarctic Peninsula (1944). During the late 18th and early 19th centuries, interest in Antarctica was largely focused on the exploitation of its surrounding waters by sealers and whalers. The discovery of the South Shetland Islands is attributed to Captain William Smith who was blown off course when sailing around Cape Horn in 1819. -
Observations of OH and HO2 Radicals in Coastal Antarctica
Atmos. Chem. Phys., 7, 4171–4185, 2007 www.atmos-chem-phys.net/7/4171/2007/ Atmospheric © Author(s) 2007. This work is licensed Chemistry under a Creative Commons License. and Physics Observations of OH and HO2 radicals in coastal Antarctica W. J. Bloss1,*, J. D. Lee1,**, D. E. Heard1, R. A. Salmon2, S. J.-B. Bauguitte2, H. K. Roscoe2, and A. E. Jones2 1School of Chemistry, University of Leeds, Woodhouse Lane, Leeds, LS2 9JT, UK 2British Antarctic Survey, Madingley Road, Cambridge, CB3 0ET, UK *now at: School of Geography, Earth & Environmental Sciences, University of Birmingham, Edgbaston, Birmingham, B15 2TT, UK **now at: Department of Chemistry, University of York, Heslington, York, YO10 5DD, UK Received: 18 January 2007 – Published in Atmos. Chem. Phys. Discuss.: 23 February 2007 Revised: 27 July 2007 – Accepted: 10 August 2007 – Published: 16 August 2007 Abstract. OH and HO2 radical concentrations have been Field measurement campaigns, in which coordinated mea- measured in the boundary layer of coastal Antarctica for a surements of radical species such as OH, HO2, NO etc. have six-week period during the austral summer of 2005. The been performed, provide a means to test and refine our un- measurements were performed at the British Antarctic Sur- derstanding of fast radical photochemistry. Measurements ◦ 0 ◦ 0 vey’s Halley Research Station (75 35 S, 26 19 W), using of OH and HO2 radicals have been performed in a range the technique of on-resonance laser-induced fluorescence to of marine and continental, polluted and clean environments detect OH, with HO2 measured following chemical conver- (e.g. -
Halley Research Station, Antarctica: Calving Risks and Monitoring Strategies”, by R
Review of “Halley Research Station, Antarctica: calving risks and monitoring strategies”, by R. Anderson, D. H. Jones and G. H. Gudmundsson, submitted to Natural Hazards and Earth System Sciences (NHESS) Reviewer: Ala Khazendar ([email protected]) Summary: This work can be viewed as having two main parts: the first considers the different calving scenarios that can pose a risk to Halley Station. The second part describes the monitoring techniques being applied to provide a measure of advanced warning of a potentially hazardous calving event. I believe that this is a valuable effort. The analysis that the authors present of the historical evidence will be useful not only for the purposes of hazard assessment (the focus of this work) but also for glaciological research and questions of ice-shelf flow and stability. In their analysis of the historical evidence, the authors are careful to identify the limitations of the available observations, and they are to be commended for that. On the other hand, the authors could improve and expand the description of their data analyses and monitoring techniques to better support the results they present, and to make a more persuasive case of the suitability of the monitoring program to the task of hazard detection. The manuscript is generally well structured, and the figures helpful. In particular, Fig. 4 nicely presents the historical evidence. I recommend this paper for publication after the implementation of the suggestions below. Main issues: P. 6232 L. 26-27: “On Brunt Ice Shelf surface temperatures are well below the freezing point throughout the year, and surface melting does not occur.” Given that the main concern of this work is hazard assessment, noting that currently Brunt’s surface temperatures are below freezing is insufficient to conclude that it will not be susceptible to a Larsen-B type disintegration. -
2571 Country Code
2571 Country Code. CountryCode.org is your complete guide to call anywhere in the world. The calling chart above will help you find the dialing codes you need to make long distance phone calls to friends, family, and business partners around the globe. Simply find and click the country you wish to call. You'll find instructions on how to call that country using its country code, as well as other helpful information like area codes, ISO country codes, and the kinds of electrical outlets and phone jacks found in that part of the world. Making a phone call has never been easier with CountryCode.org. The 2-letter codes shown below are supplied by the ISO ( International Organization for Standardization). It bases its list of country names and abbreviations on the list of names published by the United Nations. The UN also uses 3-letter codes, and numerical codes to identify nations, and those are shown below. International Dialing Codes for making overseas phone calls are also listed below. Note: If the columns don't align correctly, please increase the font size in your browser. COUNTRY A2 (ISO) A3 (UN) NUM (UN) DIALING CODE Afghanistan AF AFG 4 93 Albania AL ALB 8 355 Algeria DZ DZA 12 213 American Samoa AS ASM 16 1-684 Andorra AD AND 20 376 Angola AO AGO 24 244 Anguilla AI AIA 660 1-264 Antarctica AQ ATA 10 672 Antigua and Barbuda AG ATG 28 1-268 Argentina AR ARG 32 54 Armenia AM ARM 51 374 Aruba AW ABW 533 297 Australia AU AUS 36 61 Austria AT AUT 40 43 Azerbaijan AZ AZE 31 994 Bahamas BS BHS 44 1-242 Bahrain BH BHR 48 973 Bangladesh BD -
Downloaded 10/01/21 12:24 PM UTC 4772 JOURNAL of CLIMATE VOLUME 34
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. -
The Antarctic Sun, January 7, 2007
January 7, 2007 Enhancing the snapshot Two young scientists look to augment ice core project By Steven Profaizer Sun staff For most of the year, the weather at WAIS Divide field camp blows … and blows and blows. Wind and snow are a regular part of life and science on the often-overcast West Antarctic Ice Sheet. But very suddenly in mid- December, the wind stopped and the clouds cleared, the sun came out and the tem- peratures climbed to nega- tive 10 degrees Celsius. Ben Smith lowers a video See ENHANCING camera into a borehole on on page 7 the West Antarctic Ice Sheet. Steven Profaizer / The Antarctic Sun Drillers create pilot hole for WAIS Divide ice core – Page 9 Drill enhancements provide excellent results – Page 11 Workers piece together arch to house deep drill – Page 12 More stories about LIFE and SCIENCE at WAIS Nine-member camp staff brings life to barren ice sheet – Page 13 Antarctic nuclear monitoring stations INSIDE contribute to worldwide CTBT network Keeper of the cores By Steve Martaindale tries at 321 sites. Several monitoring sta- Page 3 Sun staff tions are in Antarctica, including a recently In the 60-plus years since the dawn of certified radionuclide sampler at Palmer the Atomic Age, the specter of unreliable Station. information has cast a thicker pall over the “As you might guess, nobody is suspi- Spin doctor turns into medic naturally gloomy subject of nuclear prolif- cious of Antarctica producing a nuclear Page 16 eration. Nations have not felt they could weapon,” said Erik Swanberg, whose busi- take the word of others to not build and test ness it is to build some of the monitoring weapons.