Arctic & Antarctic Activity Book
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The Antarctic Treaty System And
The Antarctic Treaty System and Law During the first half of the 20th century a series of territorial claims were made to parts of Antarctica, including New Zealand's claim to the Ross Dependency in 1923. These claims created significant international political tension over Antarctica which was compounded by military activities in the region by several nations during the Second World War. These tensions were eased by the International Geophysical Year (IGY) of 1957-58, the first substantial multi-national programme of scientific research in Antarctica. The IGY was pivotal not only in recognising the scientific value of Antarctica, but also in promoting co- operation among nations active in the region. The outstanding success of the IGY led to a series of negotiations to find a solution to the political disputes surrounding the continent. The outcome to these negotiations was the Antarctic Treaty. The Antarctic Treaty The Antarctic Treaty was signed in Washington on 1 December 1959 by the twelve nations that had been active during the IGY (Argentina, Australia, Belgium, Chile, France, Japan, New Zealand, Norway, South Africa, United Kingdom, United States and USSR). It entered into force on 23 June 1961. The Treaty, which applies to all land and ice-shelves south of 60° South latitude, is remarkably short for an international agreement – just 14 articles long. The twelve nations that adopted the Treaty in 1959 recognised that "it is in the interests of all mankind that Antarctica shall continue forever to be used exclusively for peaceful purposes and shall not become the scene or object of international discord". -
Office of Polar Programs
DEVELOPMENT AND IMPLEMENTATION OF SURFACE TRAVERSE CAPABILITIES IN ANTARCTICA COMPREHENSIVE ENVIRONMENTAL EVALUATION DRAFT (15 January 2004) FINAL (30 August 2004) National Science Foundation 4201 Wilson Boulevard Arlington, Virginia 22230 DEVELOPMENT AND IMPLEMENTATION OF SURFACE TRAVERSE CAPABILITIES IN ANTARCTICA FINAL COMPREHENSIVE ENVIRONMENTAL EVALUATION TABLE OF CONTENTS 1.0 INTRODUCTION....................................................................................................................1-1 1.1 Purpose.......................................................................................................................................1-1 1.2 Comprehensive Environmental Evaluation (CEE) Process .......................................................1-1 1.3 Document Organization .............................................................................................................1-2 2.0 BACKGROUND OF SURFACE TRAVERSES IN ANTARCTICA..................................2-1 2.1 Introduction ................................................................................................................................2-1 2.2 Re-supply Traverses...................................................................................................................2-1 2.3 Scientific Traverses and Surface-Based Surveys .......................................................................2-5 3.0 ALTERNATIVES ....................................................................................................................3-1 -
2. Disc Resources
An early map of the world Resource D1 A map of the world drawn in 1570 shows ‘Terra Australis Nondum Cognita’ (the unknown south land). National Library of Australia Expeditions to Antarctica 1770 –1830 and 1910 –1913 Resource D2 Voyages to Antarctica 1770–1830 1772–75 1819–20 1820–21 Cook (Britain) Bransfield (Britain) Palmer (United States) ▼ ▼ ▼ ▼ ▼ Resolution and Adventure Williams Hero 1819 1819–21 1820–21 Smith (Britain) ▼ Bellingshausen (Russia) Davis (United States) ▼ ▼ ▼ Williams Vostok and Mirnyi Cecilia 1822–24 Weddell (Britain) ▼ Jane and Beaufoy 1830–32 Biscoe (Britain) ★ ▼ Tula and Lively South Pole expeditions 1910–13 1910–12 1910–13 Amundsen (Norway) Scott (Britain) sledge ▼ ▼ ship ▼ Source: Both maps American Geographical Society Source: Major voyages to Antarctica during the 19th century Resource D3 Voyage leader Date Nationality Ships Most southerly Achievements latitude reached Bellingshausen 1819–21 Russian Vostok and Mirnyi 69˚53’S Circumnavigated Antarctica. Discovered Peter Iøy and Alexander Island. Charted the coast round South Georgia, the South Shetland Islands and the South Sandwich Islands. Made the earliest sighting of the Antarctic continent. Dumont d’Urville 1837–40 French Astrolabe and Zeelée 66°S Discovered Terre Adélie in 1840. The expedition made extensive natural history collections. Wilkes 1838–42 United States Vincennes and Followed the edge of the East Antarctic pack ice for 2400 km, 6 other vessels confirming the existence of the Antarctic continent. Ross 1839–43 British Erebus and Terror 78°17’S Discovered the Transantarctic Mountains, Ross Ice Shelf, Ross Island and the volcanoes Erebus and Terror. The expedition made comprehensive magnetic measurements and natural history collections. -
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. -
Asynchronous Antarctic and Greenland Ice-Volume Contributions to the Last Interglacial Sea-Level Highstand
ARTICLE https://doi.org/10.1038/s41467-019-12874-3 OPEN Asynchronous Antarctic and Greenland ice-volume contributions to the last interglacial sea-level highstand Eelco J. Rohling 1,2,7*, Fiona D. Hibbert 1,7*, Katharine M. Grant1, Eirik V. Galaasen 3, Nil Irvalı 3, Helga F. Kleiven 3, Gianluca Marino1,4, Ulysses Ninnemann3, Andrew P. Roberts1, Yair Rosenthal5, Hartmut Schulz6, Felicity H. Williams 1 & Jimin Yu 1 1234567890():,; The last interglacial (LIG; ~130 to ~118 thousand years ago, ka) was the last time global sea level rose well above the present level. Greenland Ice Sheet (GrIS) contributions were insufficient to explain the highstand, so that substantial Antarctic Ice Sheet (AIS) reduction is implied. However, the nature and drivers of GrIS and AIS reductions remain enigmatic, even though they may be critical for understanding future sea-level rise. Here we complement existing records with new data, and reveal that the LIG contained an AIS-derived highstand from ~129.5 to ~125 ka, a lowstand centred on 125–124 ka, and joint AIS + GrIS contributions from ~123.5 to ~118 ka. Moreover, a dual substructure within the first highstand suggests temporal variability in the AIS contributions. Implied rates of sea-level rise are high (up to several meters per century; m c−1), and lend credibility to high rates inferred by ice modelling under certain ice-shelf instability parameterisations. 1 Research School of Earth Sciences, The Australian National University, Canberra, ACT 2601, Australia. 2 Ocean and Earth Science, University of Southampton, National Oceanography Centre, Southampton SO14 3ZH, UK. 3 Department of Earth Science and Bjerknes Centre for Climate Research, University of Bergen, Allegaten 41, 5007 Bergen, Norway. -
Texts G7 Sout Pole Expeditions
READING CLOSELY GRADE 7 UNIT TEXTS AUTHOR DATE PUBLISHER L NOTES Text #1: Robert Falcon Scott and Roald Amundsen (Photo Collages) Scott Polar Research Inst., University of Cambridge - Two collages combine pictures of the British and the Norwegian Various NA NA National Library of Norway expeditions, to support examining and comparing visual details. - Norwegian Polar Institute Text #2: The Last Expedition, Ch. V (Explorers Journal) Robert Falcon Journal entry from 2/2/1911 presents Scott’s almost poetic 1913 Smith Elder 1160L Scott “impressions” early in his trip to the South Pole. Text #3: Roald Amundsen South Pole (Video) Viking River Combines images, maps, text and narration, to present a historical NA Viking River Cruises NA Cruises narrative about Amundsen and the Great Race to the South Pole. Text #4: Scott’s Hut & the Explorer’s Heritage of Antarctica (Website) UNESCO World Google Cultural Website allows students to do a virtual tour of Scott’s Antarctic hut NA NA Wonders Project Institute and its surrounding landscape, and links to other resources. Text #5: To Build a Fire (Short Story) The Century Excerpt from the famous short story describes a man’s desperate Jack London 1908 920L Magazine attempts to build a saving =re after plunging into frigid water. Text #6: The North Pole, Ch. XXI (Historical Narrative) Narrative from the =rst man to reach the North Pole describes the Robert Peary 1910 Frederick A. Stokes 1380L dangers and challenges of Arctic exploration. Text #7: The South Pole, Ch. XII (Historical Narrative) Roald Narrative recounts the days leading up to Amundsen’s triumphant 1912 John Murray 1070L Amundsen arrival at the Pole on 12/14/1911 – and winning the Great Race. -
Polartrec Teacher Joins Hunt for Old Ice in Antarctica
NEWSLETTER OF THE NATIONAL ICE CORE LABORATORY — SCIENCE MANAGEMENT OFFICE Vol. 5 Issue 1 • SPRING 2010 PolarTREC Teacher Joins Hunt for Old Eric Cravens: Ice in Antarctica Farewell & By Jacquelyn (Jackie) Hams, PolarTREC Teacher Thanks! Courtesy: PolarTREC ... page 2 WAIS Divide Ice Core Images Now Available from AGDC ... page 3 WAIS Divide Ice Dave Marchant and Jackie Hams Core Update Photo: PolarTREC ... page 3 WHEN I APPLIED to the PolarTREC I actually left for Antarctica. I was originally program (http://www.polartrec.com/), I was selected by the CReSIS (Center for Remote asked where I would prefer to go given the Sensing of Ice Sheets) project, which has options of the Arctic, Antarctica, or either. I headquarters at the University of Kansas. I checked the Antarctica box only, despite the met and spent a few days visiting the team at Drilling for Old Ice fact that I may have decreased my chances of the University of Kansas and had dinner at the being selected. Antarctica was my preference Principal Investigator’s home with other team ... page 5 for many reasons. As a teacher I felt that members. We were all pleased with the match Antarctica represented the last frontier to study and looked forward to working together. the geologic history of the planet because the continent is uninhabited, not polluted, and In the late summer of 2008, I was informed that NEEM Reaches restricted to pure research. Over the last few the project was cancelled and that I would be Eemian and years I have noticed that my students were assigned to another research team. -
Article Is Available On- 2012
The Cryosphere, 14, 2673–2686, 2020 https://doi.org/10.5194/tc-14-2673-2020 © Author(s) 2020. This work is distributed under the Creative Commons Attribution 4.0 License. Clouds damp the radiative impacts of polar sea ice loss Ramdane Alkama1, Patrick C. Taylor2, Lorea Garcia-San Martin1, Herve Douville3, Gregory Duveiller1, Giovanni Forzieri1, Didier Swingedouw4, and Alessandro Cescatti1 1European Commission – Joint Research Centre, Via Enrico Fermi, 2749, 21027 Ispra (VA), Italy 2NASA Langley Research Center, Hampton, Virginia, USA 3Centre National de Recherches Météorologiques, Météo-France/CNRS, Toulouse, France 4EPOC, Université de Bordeaux, Allée Geoffroy Saint-Hilaire, Pessac 33615, France Correspondence: Ramdane Alkama ([email protected]) and Patrick C. Taylor ([email protected]) Received: 19 November 2019 – Discussion started: 19 December 2019 Revised: 19 June 2020 – Accepted: 6 July 202 – Published: 21 August 2020 Abstract. Clouds play an important role in the climate sys- 1 Introduction tem: (1) cooling Earth by reflecting incoming sunlight to space and (2) warming Earth by reducing thermal energy loss to space. Cloud radiative effects are especially important Solar radiation is the primary energy source for the Earth in polar regions and have the potential to significantly alter system and provides the energy driving motions in the atmo- the impact of sea ice decline on the surface radiation budget. sphere and ocean, the energy behind water phase changes, Using CERES (Clouds and the Earth’s Radiant Energy Sys- and the energy stored in fossil fuels. Only a fraction (Loeb tem) data and 32 CMIP5 (Coupled Model Intercomparison et al., 2018) of the solar energy arriving to the top of the Project) climate models, we quantify the influence of polar Earth atmosphere (short-wave radiation; SW) is absorbed at clouds on the radiative impact of polar sea ice variability. -
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. -
Frederick J. Krabbé, Last Man to See HMS Investigator Afloat, May 1854
The Journal of the Hakluyt Society January 2017 Frederick J. Krabbé, last man to see HMS Investigator afloat, May 1854 William Barr1 and Glenn M. Stein2 Abstract Having ‘served his apprenticeship’ as Second Master on board HMS Assistance during Captain Horatio Austin’s expedition in search of the missing Franklin expedition in 1850–51, whereby he had made two quite impressive sledge trips, in the spring of 1852 Frederick John Krabbé was selected by Captain Leopold McClintock to serve under him as Master (navigation officer) on board the steam tender HMS Intrepid, part of Captain Sir Edward Belcher’s squadron, again searching for the Franklin expedition. After two winterings, the second off Cape Cockburn, southwest Bathurst Island, Krabbé was chosen by Captain Henry Kellett to lead a sledging party west to Mercy Bay, Banks Island, to check on the condition of HMS Investigator, abandoned by Commander Robert M’Clure, his officers and men, in the previous spring. Krabbé executed these orders and was thus the last person to see Investigator afloat. Since, following Belcher’s orders, Kellett had abandoned HMS Resolute and Intrepid, rather than their return journey ending near Cape Cockburn, Krabbé and his men had to continue for a further 140 nautical miles (260 km) to Beechey Island. This made the total length of their sledge trip 863½ nautical miles (1589 km), one of the longest man- hauled sledge trips in the history of the Arctic. Introduction On 22 July 2010 a party from the underwater archaeology division of Parks Canada flew into Mercy Bay in Aulavik National Park, on Banks Island, Northwest Territories – its mission to try to locate HMS Investigator, abandoned here by Commander Robert McClure in 1853.3 Two days later underwater archaeologists Ryan Harris and Jonathan Moore took to the water in a Zodiac to search the bay, towing a side-scan sonar towfish. -
Paper Number: 2897 a History of Early Antarctic Fossil Discoveries in Support of the Supercontinent Gondwana Clary, R.M.1, and Sharpe, T.2
Paper Number: 2897 A History of Early Antarctic Fossil Discoveries in Support of the Supercontinent Gondwana Clary, R.M.1, and Sharpe, T.2 1Mississippi State University, Box 5448, Mississippi State, MS 39762 USA; [email protected] 2Centre for Lifelong Learning, Cardiff University, UK ___________________________________________________________________________ First proposed by Eduard Suess (1831-1914), the supercontinent Gondwana included the present-day continents of South America, Africa, Australia, India, and Antarctica. Alexander Du Toit (1878-1948) expanded Suess’ work in his 1937 book, Our Wandering Continents; An Hypothesis of Continental Drifting. Correlating evidence to support the inclusion of Antarctica in the Gondwana supercontinent would result from the stratigraphic and paleontological data collected within early polar expeditions. Early rock and fossil specimens of Antarctica were recovered by the 1829-1831 Antarctic Expedition sponsored by the United States of America. The expedition included a scientific program, supported by the Lyceum for Natural History of the City of New York. James Eights (1798-1882) produced quality scientific work, including a geological description of the Shetland Islands, and the first fossil of the Antarctic—carbonized wood [1, 2]. The Norwegian expedition of 1893-1894, under Carl Anton Larsen (1860-1924), also found petrified wood fossils on Seymour Island. The wood hinted of a warmer climate in Antarctica’s past, and sparked scientific interest [3]. Within the Heroic Age of Antarctic Exploration (1897-1922), additional fossils were uncovered. Cretaceous ammonites, molluscs, echinoderms and leaves were collected on Seymour Island, and additional plant fossils at Hope Bay, by geologist Nils Otto Gustaf Nordenskjöld (1869-1928) during the Swedish South Polar Expedition of 1901-1904.