Science Planning Summary 2019-20
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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. -
Antarctic Peninsula
Hucke-Gaete, R, Torres, D. & Vallejos, V. 1997c. Entanglement of Antarctic fur seals, Arctocephalus gazella, by marine debris at Cape Shirreff and San Telmo Islets, Livingston Island, Antarctica: 1998-1997. Serie Científica Instituto Antártico Chileno 47: 123-135. Hucke-Gaete, R., Osman, L.P., Moreno, C.A. & Torres, D. 2004. Examining natural population growth from near extinction: the case of the Antarctic fur seal at the South Shetlands, Antarctica. Polar Biology 27 (5): 304–311 Huckstadt, L., Costa, D. P., McDonald, B. I., Tremblay, Y., Crocker, D. E., Goebel, M. E. & Fedak, M. E. 2006. Habitat Selection and Foraging Behavior of Southern Elephant Seals in the Western Antarctic Peninsula. American Geophysical Union, Fall Meeting 2006, abstract #OS33A-1684. INACH (Instituto Antártico Chileno) 2010. Chilean Antarctic Program of Scientific Research 2009-2010. Chilean Antarctic Institute Research Projects Department. Santiago, Chile. Kawaguchi, S., Nicol, S., Taki, K. & Naganobu, M. 2006. Fishing ground selection in the Antarctic krill fishery: Trends in patterns across years, seasons and nations. CCAMLR Science, 13: 117–141. Krause, D. J., Goebel, M. E., Marshall, G. J., & Abernathy, K. (2015). Novel foraging strategies observed in a growing leopard seal (Hydrurga leptonyx) population at Livingston Island, Antarctic Peninsula. Animal Biotelemetry, 3:24. Krause, D.J., Goebel, M.E., Marshall. G.J. & Abernathy, K. In Press. Summer diving and haul-out behavior of leopard seals (Hydrurga leptonyx) near mesopredator breeding colonies at Livingston Island, Antarctic Peninsula. Marine Mammal Science.Leppe, M., Fernandoy, F., Palma-Heldt, S. & Moisan, P 2004. Flora mesozoica en los depósitos morrénicos de cabo Shirreff, isla Livingston, Shetland del Sur, Península Antártica, in Actas del 10º Congreso Geológico Chileno. -
Jörg M. Schäfer
JÖRG M. SCHÄFER LAMONT-DOHERTY EARTH OBSERVATORY • THE EARTH INSTITUTE AT COLUMBIA UNIVERSITY ROUTE 9W • PALISADES, NY 10964 • USA PHONE: 1 845 365 8756 • FAX: 1 845 365 8155 • EMAIL: [email protected] Personal Born 1968 in Stuttgart, Germany Citizenship: German Language: german, english, french 90 Morningside Drive • Apt. 2G New York • NY-10027 Education Lamont Research Professor Lamont-Doherty Earth Observatory of Columbia University Adjunct Professor Dept. of Earth and Environmental Sciences, Columbia University Doherty Associate Research Scientist (September 2003-November 2008) Lamont-Doherty Earth Observatory of Columbia University Postdoctoral Research Fellow (January 2001-August 2003) Lamont-Doherty Earth Observatory of Columbia University Postdoctoral Researcher (February 2000-October 2000) Dept. of Earth Sciences, Swiss Federal Institute of Technology (ETH) Zürich Ph.D. (March 1996-June 2000) Swiss Federal Institute of Technology (ETH) Zürich. Dissertation: Reconstruction of landscape evolution and continental paleoglaciations using in-situ cosmogenic nuclides. Jointly supervised by Profs. R. Wieler, C. Schlüchter, A.N. Halliday at the Department of Earth Sciences, ETH Zürich Masters Degree (“Diplom”) in Physics (1995) Institute of Environmental Physics, University of Heidelberg, Germany. Reconstruction of bio-geochemical trace substance cycles from an alpine ice- core. Supervisors: Dr. D. Wagenbach, Prof. U. Platt. Exchange student • ERASMUS program (1991-92) Department of Physics, University of Aix- Marseille III, -
Amazing Antarctica – Lesson 6
Year 8 GEOGRAPHY – Ecosystems – Amazing Antarctica – Lesson 6 Title: Ecosystems – Amazing Antarctica TASK 1: write down the following WOW words. As you go through the information, write the definition for each word (you might find some of the definitions as you work through the booklet). • Precipitation = • Albedo = • Ice sheet = • Glaciers = • Food chain = TASK 2: where is Antarctica? Use the following sentence starters and complete them to explain where Antarctica is located around the world. • Antarctica is located at the _________________ pole. • Antarctica is a country/continent/city. • Nearby countries include ______________________. • The oceans that surround Antarctica are __________________________. TASK 3: watch the video and write down facts about Antarctica https://www.youtube.com/watch?v=X3uT89xoKuc Antarctica TASK 4: what is the climate like in Antarctica? Read through the information below and answer the questions in red. Climate of Antarctica Antarctica can be called a desert because of its low levels of precipitation, which is mainly snow. In coastal regions, about 200 mm can fall annually. In mountainous regions and on the East Antarctica plateau, the amount is less than 50 mm annually. Evaporation is not as high as other desert regions because it is so cold, so the snow gradually builds up year after year. There are also strong winds, with recordings of up to 200 mph being made. Antarctica's seasons are opposite to the seasons that we're familiar with in the UK. Antarctic summers happen at the same time as UK winters. This is because Antarctica is in the Southern Hemisphere, which faces the Sun during our winter time. -
Educator's Guide
SOUTH POLE Amundsen’s Route Scott’s Route Roald Amundsen EDUCATOR’S GUIDE amnh.org/education/race Robert Falcon Scott INSIDE: • Suggestions to Help You Come Prepared • Essential Questions for Student Inquiry • Strategies for Teaching in the Exhibition • Map of the Exhibition • Online Resources for the Classroom • Correlation to Standards • Glossary ESSENTIAL QUESTIONS Who would be fi rst to set foot at the South Pole, Norwegian explorer Roald Amundsen or British Naval offi cer Robert Falcon Scott? Tracing their heroic journeys, this exhibition portrays the harsh environment and scientifi c importance of the last continent to be explored. Use the Essential Questions below to connect the exhibition’s themes to your curriculum. What do explorers need to survive during What is Antarctica? Antarctica is Earth’s southernmost continent. About the size of the polar expeditions? United States and Mexico combined, it’s almost entirely covered Exploring Antarc- by a thick ice sheet that gives it the highest average elevation of tica involved great any continent. This ice sheet contains 90% of the world’s land ice, danger and un- which represents 70% of its fresh water. Antarctica is the coldest imaginable physical place on Earth, and an encircling polar ocean current keeps it hardship. Hazards that way. Winds blowing out of the continent’s core can reach included snow over 320 kilometers per hour (200 mph), making it the windiest. blindness, malnu- Since most of Antarctica receives no precipitation at all, it’s also trition, frostbite, the driest place on Earth. Its landforms include high plateaus and crevasses, and active volcanoes. -
Antarctic Primer
Antarctic Primer By Nigel Sitwell, Tom Ritchie & Gary Miller By Nigel Sitwell, Tom Ritchie & Gary Miller Designed by: Olivia Young, Aurora Expeditions October 2018 Cover image © I.Tortosa Morgan Suite 12, Level 2 35 Buckingham Street Surry Hills, Sydney NSW 2010, Australia To anyone who goes to the Antarctic, there is a tremendous appeal, an unparalleled combination of grandeur, beauty, vastness, loneliness, and malevolence —all of which sound terribly melodramatic — but which truly convey the actual feeling of Antarctica. Where else in the world are all of these descriptions really true? —Captain T.L.M. Sunter, ‘The Antarctic Century Newsletter ANTARCTIC PRIMER 2018 | 3 CONTENTS I. CONSERVING ANTARCTICA Guidance for Visitors to the Antarctic Antarctica’s Historic Heritage South Georgia Biosecurity II. THE PHYSICAL ENVIRONMENT Antarctica The Southern Ocean The Continent Climate Atmospheric Phenomena The Ozone Hole Climate Change Sea Ice The Antarctic Ice Cap Icebergs A Short Glossary of Ice Terms III. THE BIOLOGICAL ENVIRONMENT Life in Antarctica Adapting to the Cold The Kingdom of Krill IV. THE WILDLIFE Antarctic Squids Antarctic Fishes Antarctic Birds Antarctic Seals Antarctic Whales 4 AURORA EXPEDITIONS | Pioneering expedition travel to the heart of nature. CONTENTS V. EXPLORERS AND SCIENTISTS The Exploration of Antarctica The Antarctic Treaty VI. PLACES YOU MAY VISIT South Shetland Islands Antarctic Peninsula Weddell Sea South Orkney Islands South Georgia The Falkland Islands South Sandwich Islands The Historic Ross Sea Sector Commonwealth Bay VII. FURTHER READING VIII. WILDLIFE CHECKLISTS ANTARCTIC PRIMER 2018 | 5 Adélie penguins in the Antarctic Peninsula I. CONSERVING ANTARCTICA Antarctica is the largest wilderness area on earth, a place that must be preserved in its present, virtually pristine state. -
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. -
Immediate Scientific Report of the Ross Sea Iceberg Project 1987-88
SCIENCE AND RESEARCH INTERNAL REPORT 9 IMMEDIATE SCIENTIFIC REPORT OF THE ROSS SEA ICEBERG PROJECT 1987-88 by J.R. Keys and A.D.W. Fowler* This is an unpublished report and must not be cited or reproduced in whole or part without permission from the Director, Science and Research. It should be cited as Science and Research Internal Report No.9 (unpublished). Science and Research Directorate, Department of Conservation, P.O. Box 10 420 Wellington, New Zealand April 1988 *Division of Information Technology, DSIR, Lower Hutt. 1 Frontispiece. NOAA 9 infrared satellite image of the 160 km long mega-giant iceberg B-9 on 9 November, four weeks after separating from the eastern front of Ross Ice Shelf. The image was digitized by US Navy scientists at McMurdo Station, paid for by the US National Science Foundation and supplied by the Antarctic Research Center at Scripps Institute. Several other bergs up to 20 km long that calved at the same time can be seen between B-9 and the ice shelf. These bergs have since drifted as far west as Ross Island (approx 600 km) whereas B-9 has moved only 215 km by 13 April, generally in a west-north-west direction. 2 CONTENTS Frontispiece 1 Contents page 2 SUMMARY 3 INTRODUCTION 4 PROPOSED PROGRAMME 5 ITINERARY 6 SCIENTIFIC ACHIEVEMENTS RNZAF C-130 iceberg monitoring flight 6 SPOT satellite image and concurrent aerial Photography 8 Ground-based fieldwork 9 B-9 iceberg 11 CONCLUSION 13 FUTURE RESEARCH 13 PUBLICATIONS 14 Acknowledgenents 14 References 14 FIGURES 15 TABLES 20 3 1. -
Blue Sky Airlines
GPS Support to the National Science Foundation Office of Polar Programs 2001-2002 Season Report GPS Support to the National Science Foundation Office of Polar Programs 2001-2002 Season Report April 15, 2002 Bjorn Johns Chuck Kurnik Shad O’Neel UCAR/UNAVCO Facility University Corporation for Atmospheric Research 3340 Mitchell Lane Boulder, CO 80301 (303) 497-8034 www.unavco.ucar.edu Support funded by the National Science Foundation Office of Polar Programs Scientific Program Order No. 2 (EAR-9903413) to Cooperative Agreement No. 9732665 Cover photo: Erebus Ice Tongue Mapping – B-017 1 UNAVCO 2001-2002 Report Table of Contents: Summary........................................................................................................................................................ 3 Table 1 – 2001-2001 Antarctic Support Provided................................................................................. 4 Table 2 – 2001 Arctic Support Provided................................................................................................ 4 Science Support............................................................................................................................................. 5 Training.................................................................................................................................................... 5 Field Support........................................................................................................................................... 5 Data Processing .................................................................................................................................... -
United States Antarctic Program S Nm 5 Helicopter Landing Facilities 22 2010-11 Ms 180 N Manuela (! USAP Helo Sites (! ANZ Helo Sites This Page: 1
160°E 165°E ALL170°E FACILITIES Terra Nova Bay s United States Antarctic Program nm 5 22 Helicopter Landing Facilities ms 180 n Manuela 2010-11 (! (! This page: USAP Helo Sites ANZ Helo Sites 75°S 1. All facilities 75°S 2. Ross Island Maps by Brad Herried Facilities provided by 3. Koettlitz Glacier Area ANTARCTIC GEOSPATIAL INFORMATION CENTER United States Antarctic Program Next page: 4. Dry Valleys August 2010 Basemap data from ADD / LIMA ROSS ISLAND Peak Brimstone P Cape Bird (ASPA 116) (! (! Mt Bird Franklin Is 76°S Island 76°S 90 nms Lewis Bay (A ! ay (ASPA 156) Mt Erebus (Fang Camp)(! ( (! Tripp Island Fang Glacier ror vasse Lower Erebus Hut Ter rth Cre (!(! Mt No Hoopers Shoulder (!M (! (! (! (! Pony Lake (! Mt Erebus (!(! Cape Cape Royds Cones (AWS Site 114) Crozier (ASPA 124) o y Convoy Range Beaufort Island (AS Battleship Promontory C SPA 105) Granite Harbour Cape Roberts Mt Seuss (! Cotton Glacier Cape Evans rk 77°S T s ad (! Turks Head ! (!(! ( 77°S AWS 101 - Tent Island Big Razorback Island CH Surv ey Site 4 McMurdo Station CH Su (! (! rvey Sit s CH te 3 Survey (! Scott Base m y Site 2 n McMurdo Station CH W Wint - ules Island ! 5 5 t 3 Ju ( er Stora AWS 113 - J l AWS 108 3 ge - Biesia Site (! da Crevasse 1 F AWS Ferrell (! 108 - Bies (! (! siada Cr (! revasse Cape Chocolate (! AWS 113 - Jules Island 78°S AWS 109 Hobbs Glacier 9 - White Is la 78°S nd Salmon Valley L (! Lorne AWS AWS 111 - Cape s (! Spencer Range m Garwood Valley (main camp) Bratina I Warren n (! (!na Island 45 Marshall Vall (! Valley Ross I Miers Valley (main -
Proposal Description: Cenozoic Formation of the Antarctic Glacial Landscape Investigated by Low-Temperature Thermochronometry
PROPOSAL DESCRIPTION: CENOZOIC FORMATION OF THE ANTARCTIC GLACIAL LANDSCAPE INVESTIGATED BY LOW-TEMPERATURE THERMOCHRONOMETRY Summary: This pre-proposal outlines a drilling program aimed at investigating the origin of the present glacial landscape in the fjord system of the western Antarctic Peninsula by applying novel methods of low-temperature thermochronometry. This, in turn, is important in understanding the Cenozoic geologic history of Antarctica and, more broadly, in understanding the role of glaciation in climate-solid Earth interactions. Accomplishing this requires samples of the present bedrock surface in the location of maximum Cenozoic erosion, that is, glacial valley bottoms. Thus, the major challenge is the inherent inaccessibility of the Antarctic landscape: the only significant regions of Antarctica that are not now covered by ice are below present sea level. To overcome this challenge, we propose to employ an IODP mission-specific platform, specifically, a semiautonomous seabed drill suitable for short coring of crystalline bedrock in formerly glaciated and now submarine fjord bottoms. In the following sections: i) we explain why understanding Cenozoic glacial erosion in Antarctica is important; ii) we describe how we propose to develop this understanding; and iii) we outline criteria for a drilling program necessary to implement this strategy. 1. The when and how of Cenozoic glacial erosion: why is it important? Understanding how and when glacial landscapes form is broadly important for two reasons. First, formation of geomorphic features diagnostic of glaciation, e.g., cirques, U-shaped valleys, and landscapes of selective linear erosion (localized glacial troughs incised into an otherwise low-relief landscape; Sugden, 1978) requires the presence of glaciers. -
Mcmurdo Station Master Plan 2.1 December 16, 2015
MCMURDO STATION MASTER PLAN 2.1 DECEMBER 16, 2015 TABLE OF CONTENTS INTRODUCTION 4 GLOSSARY 14 ARCHITECTURAL DESIGN GUIDING PRINCIPLES 18 FACILITY CONSIDERATIONS 22 FACILITIES PROGRAM 38 MCMURDO STATION MASTER PLAN 42 SOCIAL SPACES 70 MASTER PLAN FLOW DIAGRAMS 72 CIVIL SITE & UTILITY PLAN 78 ENERGY 84 INFORMATION TECHNOLOGY & TELECOMMUNICATIONS 98 FIRE PROTECTION STRATEGY 110 CONCLUSION 116 MCMURDO STATION MP 2.1 | DECEMBER 16, 2015 PG. 3 INTRODUCTION The McMurdo Master Plan 1.0 was completed in March of 2013. The purpose of that original plan was to provide an in-depth first look at the current layout of McMurdo, identify both constraints and opportunities for future redevelopment, and create a basic plan to serve as a guide for that development. That initial plan was intended to serve as a Master Plan “starting point” to generate substantive discussion. Not only did it generate that discussion, it also resulted in a great deal of excitement. Since Master Plans are meant to be updated in light of evolving technologies and new requirements, this version was created. The Master Plan 2.0 was published on December 26, 2014. This version, Master Plan 2.1, refelects continued refinement with respect to, among other inputs, modified strategies for Traverse Operations, the IT&C Facility, as well as snow deposition modeling. PG. 4 MCMURDO STATION MP 2.1 | DECEMBER 16, 2015 INTRODUCTION GOALS OF MASTER PLAN 2.1 MISSION STATEMENT The infrastructure modernization will ensure that McMurdo Station remains a viable platform for supporting Antarctic science for the next 35 to 50 years, whereby this modernization will: • Result in comprehensive redevelopment of McMurdo Station, Antarctica, into a more energy and operationally-efficient station, optimized for support of local and deep field science.