Deep-Frozen Science There Are Other Points on Which Con- Sciousness Lacks Clarity
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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. -
Fram Strait Ice Export During the Nineteenth and Twentieth Centuries Reconstructed from a Multiyear Sea Ice Index from Southwestern Greenland
2782 JOURNAL OF CLIMATE VOLUME 16 Fram Strait Ice Export during the Nineteenth and Twentieth Centuries Reconstructed from a Multiyear Sea Ice Index from Southwestern Greenland TORBEN SCHMITH AND CARSTEN HANSEN* Danish Climate Centre, Danish Meteorological Institute, Copenhagen, Denmark (Manuscript received 8 May 2002, in ®nal form 30 January 2003) ABSTRACT Historical observations of multiyear ice, called ``storis,'' in the southwest Greenland waters exist from the period 1820±2000, obtained from ship logbooks and ice charts. It is argued that this ice originates in the Arctic Ocean and has traveled via the Fram Strait, southward along the Greenland coast in the East Greenland Current, and around the southern tip of Greenland. Therefore, it is hypothesized that these observations can be used as ``proxies'' for reconstructing the Fram Strait ice export on an annual basis. An index describing the storis extent is extracted from the observations and a linear statistical model formulated relating this index to the Fram Strait ice export. The model is calibrated using ice export values from a hindcast study with a coupled ocean±ice model over the period 1949±98. Subsequently, the model is used to reconstruct the Fram Strait annual ice export in the period 1820±2000. The model has signi®cant skill, calculated on independent data. Based on this reconstruction, it is discussed how time periods with large and small ice export on multidecadal timescales coincide with time periods of cold and warm North Atlantic sea surface temperatures reported by others. This implies that trend studies based on satellite observations should be regarded with some care, since the time period of satellite observations, the last decades, where a particularly strong negative trend is observed in the ice export, is preceded by a time period with a positive trend. -
Melges Promo
# THE WORLD LEADER IN PERFORMANCE ONE DESIGN RACING # # MELGES.COM # # MELGES.COM MELGES BOAT WORKS, INC. was founded by Harry C. Melges, Sr. in 1945. Melges became an instant leader in scow boat design, production and delivery in the U.S., particularly in the Midwest. Harry, Sr. initially built boats out of wood. The first boats produced were flat-bottomed row boats, which provided a core business to keep his vision and the company alive. It wasn't long before he branched into race boat production delivering the best hulls, sails, spars, covers and accessories ensuring his customers stayed on the competitive cutting-edge. Melges (pronounced mel•gis), is one of the most reputable, recognized and respected family names in the sailing industry. The devotion, generosity, perseverance and passion that surrounds the name is undeniable. It will forever be a legendary symbol of quality, excellence and experience that is second-to-none. Early on Harry Sr.’s son, Harry “Buddy” Melges, Jr. was involved in operating the family boat building business. Over time, Buddy established an impressive collection of championship titles and Olympic medals. During the 1964 Olympics, Buddy was awarded a bronze medal in the Flying Dutchman and in 1968 won a gold medal at the Pan Am Games. In 1972, he won a gold medal in the Soling in Kiel, Germany — the Soling’s official debut in Olympic competition. In the years that followed, Buddy won over 60 major national and international sailing championship titles. They include the Star in 1978 and 1979; 5.5 Metre in 1967, 1973 and 1983; International 50 Foot World Cup in 1989; Maxi in 1991 and the National E Scows in 1965, 1969, 1978, 1979 and 1983. -
Toxicological Profile for Barium and Barium Compounds
TOXICOLOGICAL PROFILE FOR BARIUM AND BARIUM COMPOUNDS U.S. DEPARTMENT OF HEALTH AND HUMAN SERVICES Public Health Service Agency for Toxic Substances and Disease Registry August 2007 BARIUM AND BARIUM COMPOUNDS ii DISCLAIMER The use of company or product name(s) is for identification only and does not imply endorsement by the Agency for Toxic Substances and Disease Registry. BARIUM AND BARIUM COMPOUNDS iii UPDATE STATEMENT A Toxicological Profile for Barium and Barium Compounds, Draft for Public Comment was released in September 2005. This edition supersedes any previously released draft or final profile. Toxicological profiles are revised and republished as necessary. For information regarding the update status of previously released profiles, contact ATSDR at: Agency for Toxic Substances and Disease Registry Division of Toxicology and Environmental Medicine/Applied Toxicology Branch 1600 Clifton Road NE Mailstop F-32 Atlanta, Georgia 30333 BARIUM AND BARIUM COMPOUNDS iv This page is intentionally blank. v FOREWORD This toxicological profile is prepared in accordance with guidelines developed by the Agency for Toxic Substances and Disease Registry (ATSDR) and the Environmental Protection Agency (EPA). The original guidelines were published in the Federal Register on April 17, 1987. Each profile will be revised and republished as necessary. The ATSDR toxicological profile succinctly characterizes the toxicologic and adverse health effects information for the hazardous substance described therein. Each peer-reviewed profile identifies and reviews the key literature that describes a hazardous substance's toxicologic properties. Other pertinent literature is also presented, but is described in less detail than the key studies. The profile is not intended to be an exhaustive document; however, more comprehensive sources of specialty information are referenced. -
From Gondwana to Antarctica the Discovery Of, and Early Expeditions To, Antarctica Indigenous Plants and Animals Arc C 4 0 0
TTHEHE LLASTAST GGREATREAT Department of Science and Technology WWILDERNESSILDERNESS www.dst.gov.za Sou y from th Af From Gondwana to wa rica The discovery of, and a . I Antarctica km t t early expeditions to, 0 ak 0 e 1195-13695-136 mmyaya 0 s Antarctica 4 4 JURASSIC ERA – A single s i 0 335050 BBCC mass of land (a super- a d continent) called Early Greeks hypothesise ic a Gondwana begins t y that a large mass of land to break up to c s must exist to counter the r form modern day t weight of the Arctic. They a o Africa, Antarctica, t call this land Antarctica n t New Zealand, Australia and India. Dinosaurs r – meaning ‘opposite the Arctic’. evolve and oceans teem with fi sh. Bird-like A a . creatures evolve and the climate is warm and wet. v y e 11773773 a l Captain James Cook circumnavigates the 1136-6536-65 mmyaya t Antarctic and is the fi rst to cross the Antarctic M h CRETACEOUS ERA – Antarctica has a sub- / Circle. e l i tropical climate and is covered with ferns and r r conifers. Australia and New Zealand breaks e p 11819819 away from Antarctica as it drifts towards the b A Fabian von Bellingshausen becomes fi rst person South Pole. y d to see the Antarctic continent, after crossing the s n h Antarctic Circle. a 6600 myamya i p PALAEOCENE ERA – As the continents drift r . e Weddell Sea 11820820 further apart from each other, oceans begin to I t b Captain John Davis, on a sealing expedition, surround them. -
The Quest for the Northwest Passage, by James P. Delgado
REVIEWS • 323 learn the identity of what they have been reading up to that BRAY, E.F. de. 1992. A Frenchman in search of Franklin: De point. The document identified as HBCA E.37/3, which Bray’s Arctic journal, 1852–1854. Edited by William Barr. Barr, following Anderson, refers to as a full journal Toronto and Buffalo: University of Toronto Press. (p. 166, n.1), turns out to be what I would call Anderson’s PELLY, D. 1981. Expedition: An Arctic journey through history on field notes, written daily during the expedition. In con- George Back’s River. Toronto: Betelgeuse. trast, the document that Barr has referred to in footnotes as the “fair copy of Anderson’s journal” (HBCA B.200/a/ I.S. MacLaren 31), although based on those field notes, was written after Canadian Studies Program the expedition: it shows signs of revision and narrative Department of Political Science polish. Barr’s use of the term journal to refer to both University of Alberta documents is misleading, as it blurs that important distinc- Edmonton, Alberta, Canada tion. Furthermore, justification for subordinating Stewart’s T6G 2H4 journal (Provincial Archives of Alberta 74.1/137) to Anderson’s is rendered only implicitly: Stewart’s is “gen- erally less detailed than” Anderson’s (p. 166–167). One is ACROSS THE TOP OF THE WORLD: THE QUEST FOR left to infer that the editing accords with the chain of THE NORTHWEST PASSAGE. By JAMES P. DELGADO. command, Stewart being Anderson’s junior. None of these Vancouver and Toronto: Douglas & McIntyre, 1999. -
European Patent Bulletin 1988/32
Bib'iotnek , EPA r.p'0 GEB 10.08.1988 j 10. AUG. 1SS3 1 Eirrgegsngpn 0277113-0277939 ISSN 0170-9305 Europäisches European Bulletin européen Patentblatt Patent Bulletin des brevets Inhalt Contents Sommaire I. Veröffentlichte Anmeldungen 10 I. Published Applications 10 I. Demandes publiées 10 1.1 Geordnet nach der Internationalen 10 1.1 Arranged in accordance with the 10 1.1 Classées selon la classification 10 Patentklassifikation International patent classification internationale des brevets 1.2(1) Int. Anmeldungen (Art. 158(1)) 113 1.2(1) Int. applications (Art. 158(1)) 113 1.2(1) Demandes int. (art. 158(1)) 113 1.2 (2) Int. Anmeldungen, die nicht in die 117 1.2 (2) Int. applications not entering the 117 1.2 (2) Demandes int. non entrées dans la 117 europäische Phase eingetreten sind European phase phase européenne 1.3(1) Geordnet nach Veröffentlichungs- 118 1.3 (1) Arranged by publication number 118 1.3(1) Classées selon les numéros de 118 nummern publication 1.3 (2) Geordnet nach Anmeldenummern 125 1.3 (2) Arranged by application number 125 1.3 (2) Classées selon les numéros des 125 demandes 1.4 Geordnet nach Namen der 133 1.4 Arranged by name of applicant 133 1.4 Classées selon les noms des 133 Anmelder demandeurs 1.5 Geordnet nach benannten 148 1.5 Arranged by designated Contracting 148 1.5 Classées selon les Etats contractants 148 Vertragsstaaten States désignés 1.6(1) Nach Erstellung des europäischen 177 1.6(1) Documents discovered after 177 1.6(1) Documents découverts après 177 Recherchenberichts ermittelte neue completion of the -
Model Panel Discussion
Model Panel Discussion Dorothy Koch Sunling Gong Mark Flanner Arctic Workshop New York January 2007 Model Panel Discussion Dorothy Koch, Sunling Gong, Mark Flanner Model uncertainties as well as global warming are amplified in the Arctic: i) Emission inputs (especially for fires) ii) transport to Arctic iii) removal in the Arctic environment iv) parameterization of climate effects *What measurements would help most to constrain models? Model Panel Dorothy Koch: Columbia University, GISS - Model performance in the Arctic - Sources of Arctic aerosols Where do (AeroCom) models distribute their loads? GISS MOZART ULAQ Textor et al., ACP, 2006 AeroCom BC models in Denali and Barrow Alaska Denali Barrow The unexamined life is not worth living -Socrates BC Models in Denali, Alaska BC Models in Barrow, Alaska BC Models in Denali, Alaska BC Models in Barrow, Alaska % BC load change for 40% ice scavenging % BC load Standard BC load assuming 5% ice Enhancing ice scavenging removal has big (relative to rain) effect at the poles. (Note: GISS model has large fraction of ice- % change in BC load clouds) BC snow concentration Observations compiled by Flanner et al., submitted GISS model Arctic BC is generally smaller than observed ng/g Arctic AOD origins: GISS model Koch and Hansen, JGR (2005); Koch et al., JGR, in press AODx10 Arctic surface concentration origins: GISS model Koch and Hansen, JGR (2005); Koch et al., JGR, in press Sectoral sources Residential Transport Power Biomass burning Industry Arctic BC sectoral origins: GISS model Koch et al., JGR, in press AOD Surface Emission trends during the past century Total Emission histories Europe+SE_Asia+ N_Am+Russia Sulfur Van Aardenne et al., 2001 Europe Using these N. -
Particle-Laden Eurasian Arctic Sea Ice: Observations from July and August 1987
Particle-laden Eurasian Arctic sea ice: observations from July and August 1987 STEPHANIE PFIRMAN, JEAN-CLAUDE GASCARD, INGO WOLLENBURG, PETA MUDIE AND ANDREA ABELMANN Pfirman, S., Gascard, J.-C., Wollenburg, I., Mudie, P. & Abelmann, A. 1989: Particle-laden Eurasian Arctic sea ice: observations from July and August 1987. Polar Research 7, 5M6. During the summer 1987 expedition of the polar research vessel 'Polarstern' in the Eurasian Basin of the Arctic Ocean, sea ice at about 84-86"N and 2@3OoE was found to have high concentrations of particulate material. The particle-laden ice occurred in patches which often darkened more than half the ice surface at our northernmost positions. Much of this ice appeared to be within :he Siberian Branch of the Transpolar Drift stream, which transports deformed, multi-year ice from the Siberian shelves westward across the Eurasian Basin. Lithogenic sediment, which is the major component of the particulate material, may have been incorporated during ice formation on the shallow Siberian seas. Diatoms collected from the particle- rich ice surfaces support this conclusion, as assemblages were dominated by a marine benthic species similar to that reported from sea ice off the coast of northeast Siberia. Based on drift trajectories of buoys deployed on the ice it appears that much of the particle-laden ice exited the Arctic Ocean through the Fram Strait and joined the East Greenland Current. Very different sea ice characteristics were found east of the Yermak Plateau and north of Svalbard and Frans Josef Land up to about 83-84"N. Here sea ice was thinner, less deformed, with lower amounts of lithogenic sediment and diatoms. -
Unit 3. Antarctic Oceanography Lesson 1
ANTARCTIC Unit 3. Antarctic Oceanography Lesson 1. – Overview and Research Stations Lesson Objectives: • Introduces the continent of Antarctica and the oceans that surround it • The student will learn about the geography, history and climate. • The second section of this chapter discusses research stations and the scientists who live on the frozen continent. Antarctica is a continent located form 25 million years ago. The at the southern-most point of ice in Antarctica locks up more the globe. Millions of years ago, than two-thirds of the planet's this landmass was attached to fresh water. If the Antarctic ice a giant landmass that consisted were to melt, the sea would rise of modern-day South America, almost 200 feet. It is the only India and Africa. Powerful underground forces ripped a large piece of land from this giant landmass, which then drifted to its current position at the bottom of the globe. It is surrounded on all sides by the Indian, Pacific and Atlantic Oceans. continent that man had left untouched for Antarctica's cold, thick hard millions of years. covering, called an Antarctica is ice considered the sheet, coldest and driest continent on began to earth. Temperatures decrease regions inland. Temperatures as one moves from the coastal during the long, dark winters ©PROJECT OCEANOGRAPHY ANTARCTIC OCEANOGRAPHY 87 ANTARCTIC range from –4° F to –22° F on Blizzards are produced not by the coast, -40° F to –90° F falling snow, but when high inland. During the summers, winds (100- 200mph) blow coastal temperatures average ground snow around, creating 32° F (occasionally climbing to blinding conditions and 50° F), while the inland summer snowdrifts that can cover local temperatures range from –4° F research stations in an hour. -
History of Antarctica - Wikipedia, the Free Encyclopedia Page 1 of 13
History of Antarctica - Wikipedia, the free encyclopedia Page 1 of 13 Coordinates: 67°15′S 39°35′E History of Antarctica From Wikipedia, the free encyclopedia For the natural history of the Antarctic continent, see Antarctica. The history of Antarctica emerges from early Western theories of a vast continent, known as Terra Australis, believed to exist in the far south of the globe. The term Antarctic, referring to the opposite of the Arctic Circle, was coined by Marinus of Tyre in the 2nd century AD. The rounding of the Cape of Good Hope and Cape Horn in the 15th and 16th centuries proved that Terra Australis Incognita ("Unknown Southern Land"), if it existed, was a continent in its own right. In 1773 James Cook and his crew crossed the Antarctic Circle for the first time but although they discovered nearby islands, they did not catch sight of Antarctica itself. It is believed he was as close as 150 miles from the mainland. In 1820, several expeditions claimed to have been the first to have sighted the ice shelf or the continent. A Russian expedition was led by Fabian Gottlieb von Bellingshausen and Mikhail Lazarev, a British expedition was captained by Edward Bransfield and an American sealer Nathaniel Palmer participated. The first landing was probably just over a year later when American Captain John Davis, a sealer, set foot on the ice. Several expeditions attempted to reach the South Pole in the early 20th century, during the 'Heroic Age of Antarctic Exploration'. Many resulted in injury and death. Norwegian Roald Amundsen finally reached the Pole on December 14, 1911, following a dramatic race with the Englishman Robert Falcon Scott. -
Dr. John L. Isbell Department of Geosciences, University of Wisconsin-Milwaukee P.O
Dr. John L. Isbell Department of Geosciences, University of Wisconsin-Milwaukee P.O. Box 413, Milwaukee, WI 53201 Phone: (414) 229-2877 e-mail: [email protected] http://www.uwm.edu/People/jisbell/index.html EDUCATION 1990 Ph.D., Geology. THE OHIO STATE UNIVERSITY, Columbus, Ohio. Dissertation Topic: Fluvial sedimentology and basin analysis of the Permian Fairchild and Buckley Formations, Beardmore Glacier Region, and the Weller Coal Measures, southern Victoria Land, Antarctica. Dissertation Advisor: Dr. James W. Collinson. 1985 M.S., Geology. NORTHERN ILLINOIS UNIVERSITY, DeKalb, Illinois. Thesis topic: Palynology and sedimentology of Pennsylvanian strata in the northwestern portion of the Illinois Basin. Thesis advisors: Dr. Ross D. Powell and Dr. Hsin Yi Ling. 1981 B.A., Geology. AUGUSTANA COLLEGE, Rock Island, Illinois. Advisors: Dr. Richard Anderson and Dr. Fred H. Behnken. POSITIONS HELD 9/04-Present Professor: Department of Geosciences, The University of Wisconsin-Milwaukee. Clastic sedimentologist. 9/09-8/12 Department Chair: Department of Geosciences, The University of Wisconsin- Milwaukee. 9/98-9/04 Associate Professor: Department of Geosciences, The University of Wisconsin- Milwaukee. Clastic sedimentologist. 9/92-8/98 Assistant Professor: Department of Geosciences, The University of Wisconsin- Milwaukee. Clastic sedimentologist. 5/95-97 Project Contributor: Geological Evolution and Hydrocarbon Plays of the Southern South Atlantic. A joint international project utilizing the specialties of geologists from the Cambridge Arctic Shelf Programme, Cambridge, U.K.; Centro de Investigaciones Geologicas, La Plata, Argentina; University of Aberdeen, Scotland; Institute of Geophysics at the University of Texas-Austin; University of Cambridge, U.K.; and the Department of Geosciences at the University of Wisconsin-Milwaukee.