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A Decade of Antarctic Science Support Through Amps
A DECADE OF ANTARCTIC SCIENCE SUPPORT THROUGH AMPS BY JORDAN G. POWERS, KEVIN W. MANNING, DAVID H. BROMWICH, JOHN J. CASSANO, AND ARTHUR M. CAYETTE AMPS, a real-time mesoscale modeling system, has provided a decade of service for scientific and logistical needs and has helped advance polar numerical weather prediction as well as understanding of Antarctica. ith 2011 marking the 100th anniversary of Roald Amundsen’s being the first to reach W the South Pole, the Antarctic endeavor has come a long way. The capabilities to support it have as well. In the critical area of weather forecasting, the Antarctic Mesoscale Prediction System (AMPS) has exemplified this progress for the past decade. AMPS is a real-time implementation of the Weather Research and Forecasting model (WRF; Skamarock et al. 2008) to support the U.S. Antarctic Program (USAP). Because the need for accurate weather fore- casting in Antarctica has been acute since the earliest explorations, AMPS has been a vital effort. AMPS began in 2000, when the National Science Foundation’s (NSF’s) Office of Polar Programs (OPP) sought to improve the weather forecasting support for FIG. 1. Antarctica, with referenced locations and the USAP. The concern at the time was the numerical regions shown. weather prediction (NWP) guidance available to the USAP forecasters, who were relying on an assortment It became evident early in the effort that the of models (mostly global) that were tailored neither to system could be of value to Antarctic activities their needs nor to their singular area of responsibility. beyond those tied to the McMurdo forecasters. -
University Microfilms, Inc., Ann Arbor, Michigan GEOLOGY of the SCOTT GLACIER and WISCONSIN RANGE AREAS, CENTRAL TRANSANTARCTIC MOUNTAINS, ANTARCTICA
This dissertation has been /»OOAOO m icrofilm ed exactly as received MINSHEW, Jr., Velon Haywood, 1939- GEOLOGY OF THE SCOTT GLACIER AND WISCONSIN RANGE AREAS, CENTRAL TRANSANTARCTIC MOUNTAINS, ANTARCTICA. The Ohio State University, Ph.D., 1967 Geology University Microfilms, Inc., Ann Arbor, Michigan GEOLOGY OF THE SCOTT GLACIER AND WISCONSIN RANGE AREAS, CENTRAL TRANSANTARCTIC MOUNTAINS, ANTARCTICA DISSERTATION Presented in Partial Fulfillment of the Requirements for the Degree Doctor of Philosophy in the Graduate School of The Ohio State University by Velon Haywood Minshew, Jr. B.S., M.S, The Ohio State University 1967 Approved by -Adviser Department of Geology ACKNOWLEDGMENTS This report covers two field seasons in the central Trans- antarctic Mountains, During this time, the Mt, Weaver field party consisted of: George Doumani, leader and paleontologist; Larry Lackey, field assistant; Courtney Skinner, field assistant. The Wisconsin Range party was composed of: Gunter Faure, leader and geochronologist; John Mercer, glacial geologist; John Murtaugh, igneous petrclogist; James Teller, field assistant; Courtney Skinner, field assistant; Harry Gair, visiting strati- grapher. The author served as a stratigrapher with both expedi tions . Various members of the staff of the Department of Geology, The Ohio State University, as well as some specialists from the outside were consulted in the laboratory studies for the pre paration of this report. Dr. George E. Moore supervised the petrographic work and critically reviewed the manuscript. Dr. J. M. Schopf examined the coal and plant fossils, and provided information concerning their age and environmental significance. Drs. Richard P. Goldthwait and Colin B. B. Bull spent time with the author discussing the late Paleozoic glacial deposits, and reviewed portions of the manuscript. -
Review of the Geology and Paleontology of the Ellsworth Mountains, Antarctica
U.S. Geological Survey and The National Academies; USGS OF-2007-1047, Short Research Paper 107; doi:10.3133/of2007-1047.srp107 Review of the geology and paleontology of the Ellsworth Mountains, Antarctica G.F. Webers¹ and J.F. Splettstoesser² ¹Department of Geology, Macalester College, St. Paul, MN 55108, USA ([email protected]) ²P.O. Box 515, Waconia, MN 55387, USA ([email protected]) Abstract The geology of the Ellsworth Mountains has become known in detail only within the past 40-45 years, and the wealth of paleontologic information within the past 25 years. The mountains are an anomaly, structurally speaking, occurring at right angles to the Transantarctic Mountains, implying a crustal plate rotation to reach the present location. Paleontologic affinities with other parts of Gondwanaland are evident, with nearly 150 fossil species ranging in age from Early Cambrian to Permian, with the majority from the Heritage Range. Trilobites and mollusks comprise most of the fauna discovered and identified, including many new genera and species. A Glossopteris flora of Permian age provides a comparison with other Gondwana floras of similar age. The quartzitic rocks that form much of the Sentinel Range have been sculpted by glacial erosion into spectacular alpine topography, resulting in eight of the highest peaks in Antarctica. Citation: Webers, G.F., and J.F. Splettstoesser (2007), Review of the geology and paleontology of the Ellsworth Mountains, Antarctica, in Antarctica: A Keystone in a Changing World – Online Proceedings of the 10th ISAES, edited by A.K. Cooper and C.R. Raymond et al., USGS Open- File Report 2007-1047, Short Research Paper 107, 5 p.; doi:10.3133/of2007-1047.srp107 Introduction The Ellsworth Mountains are located in West Antarctica (Figure 1) with dimensions of approximately 350 km long and 80 km wide. -
Of Penguins and Polar Bears Shapero Rare Books 93
OF PENGUINS AND POLAR BEARS Shapero Rare Books 93 OF PENGUINS AND POLAR BEARS EXPLORATION AT THE ENDS OF THE EARTH 32 Saint George Street London W1S 2EA +44 20 7493 0876 [email protected] shapero.com CONTENTS Antarctica 03 The Arctic 43 2 Shapero Rare Books ANTARCTIca Shapero Rare Books 3 1. AMUNDSEN, ROALD. The South Pole. An account of “Amundsen’s legendary dash to the Pole, which he reached the Norwegian Antarctic Expedition in the “Fram”, 1910-1912. before Scott’s ill-fated expedition by over a month. His John Murray, London, 1912. success over Scott was due to his highly disciplined dogsled teams, more accomplished skiers, a shorter distance to the A CORNERSTONE OF ANTARCTIC EXPLORATION; THE ACCOUNT OF THE Pole, better clothing and equipment, well planned supply FIRST EXPEDITION TO REACH THE SOUTH POLE. depots on the way, fortunate weather, and a modicum of luck”(Books on Ice). A handsomely produced book containing ten full-page photographic images not found in the Norwegian original, First English edition. 2 volumes, 8vo., xxxv, [i], 392; x, 449pp., 3 folding maps, folding plan, 138 photographic illustrations on 103 plates, original maroon and all full-page images being reproduced to a higher cloth gilt, vignettes to upper covers, top edges gilt, others uncut, usual fading standard. to spine flags, an excellent fresh example. Taurus 71; Rosove 9.A1; Books on Ice 7.1. £3,750 [ref: 96754] 4 Shapero Rare Books 2. [BELGIAN ANTARCTIC EXPEDITION]. Grande 3. BELLINGSHAUSEN, FABIAN G. VON. The Voyage of Fete Venitienne au Parc de 6 a 11 heurs du soir en faveur de Captain Bellingshausen to the Antarctic Seas 1819-1821. -
Trophic Interactions Within the Ross Sea Continental Shelf Ecosystem Walker O
Phil. Trans. R. Soc. B (2007) 362, 95–111 doi:10.1098/rstb.2006.1956 Published online 6 December 2006 Trophic interactions within the Ross Sea continental shelf ecosystem Walker O. Smith Jr1,*, David G. Ainley2 and Riccardo Cattaneo-Vietti3 1Virginia Institute of Marine Sciences, College of William and Mary, Gloucester Point, VA 23062, USA 2H.T. Harvey and Associates, 3150 Almaden Expressway, Suite 145, San Jose, CA 95118, USA 3Dipartimento per lo Studio del Territorio e delle sue Risorse, Universita` di Genova, Corso Europa 26, 16132 Genova, Italy The continental shelf of the Ross Sea is one of the Antarctic’s most intensively studied regions. We review the available data on the region’s physical characteristics (currents and ice concentrations) and their spatial variations, as well as components of the neritic food web, including lower and middle levels (phytoplankton, zooplankton, krill, fishes), the upper trophic levels (seals, penguins, pelagic birds, whales) and benthic fauna. A hypothetical food web is presented. Biotic interactions, such as the role of Euphausia crystallorophias and Pleuragramma antarcticum as grazers of lower levels and food for higher trophic levels, are suggested as being critical. The neritic food web contrasts dramatically with others in the Antarctic that appear to be structured around the keystone species Euphausia superba. Similarly, we suggest that benthic–pelagic coupling is stronger in the Ross Sea than in most other Antarctic regions. We also highlight many of the unknowns within the food web, and discuss the impacts of a changing Ross Sea habitat on the ecosystem. Keywords: Ross Sea; neritic food web; bio-physical coupling; ecosystem function; ecosystem structure; pelagic–benthic coupling 1. -
PDF-TITEL-AA-CHILE-EMPEORSADVENTURE Kopie.Pages
Antarktis Flug-Expeditionen EMPEROR PENGUINS Besuch der Kaiserpinguin-Kolonie in der Gould-Bucht ex Punta Arenas / Chile via Basecamp Union Glaciar POLARADVENTURES Schiffs- und Flug-Expeditionen in Arktis und Antarktis Reiseagentur Heinrich-Böll-Str. 40 * D-21335 Lüneburg * Deutschland Tel +49-4131- 223474 Fax +49-4131-54255 [email protected] www.polaradventures.de Saison 2021/22 Veranstalter Direkt-Angebote ab-bis Punta Arenas (Chile) für individuelle Planungen alle Abfahrten der Saison inkl. englischsprachiger Termine POLARADVENTURES Schiffs- und Flug-Expeditionen in Arktis und Antarktis Reiseagentur * Heinrich-Böll-Str. 40 * D-21335 Lüneburg * Deutschland Tel +49-4131- 223474 Fax +49-4131-54255 [email protected] www.polaradventures.de EMPEROR PENGUINS A PHOTOGRAPHER’S PARADISE Immerse yourself in the sights and sounds of the Gould Bay Emperor Penguin Colony on the remote coast of the Weddell Sea. Camp on the same sea ice where thousands of birds come to raise and feed their young. Photograph majestic emperors and their chicks against a spectacular backdrop of ice cliffs, pressure ridges, and icebergs. Spot petrels and seals amongst the endless white expanse. Fall asleep to a chorus of trumpeting calls and wake to find curious penguins outside your tent. Our remote field camp offers you unparalleled access to the emperors as you witness their amazing adaptations to the Antarctic environment alongside our expert guides. ITINERARY Arrival Day Punta Arenas, Chile Pre-departure Day Luggage Pick-Up & Briefing Day 1 Fly to Antarctica Day 2 Explore Union Glacier Day 3 Fly to Emperor Colony Day 4-6 Live with the Emperors Day 7 Return to Union Glacier Day 8 Explore Union Glacier Day 9 Return to Chile Flexible Departure Day Fly Home *Subject to change based on weather and flight conditions. -
A Satellite Case Study of a Katabatic Surge Along the Transantarctic Mountains D
This article was downloaded by: [Ohio State University Libraries] On: 07 March 2012, At: 15:04 Publisher: Taylor & Francis Informa Ltd Registered in England and Wales Registered Number: 1072954 Registered office: Mortimer House, 37-41 Mortimer Street, London W1T 3JH, UK International Journal of Remote Sensing Publication details, including instructions for authors and subscription information: http://www.tandfonline.com/loi/tres20 A satellite case study of a katabatic surge along the Transantarctic Mountains D. H. BROMWICH a a Byrd Polar Research Center, The Ohio State Universit, Columbus, Ohio, 43210, U.S.A Available online: 17 Apr 2007 To cite this article: D. H. BROMWICH (1992): A satellite case study of a katabatic surge along the Transantarctic Mountains, International Journal of Remote Sensing, 13:1, 55-66 To link to this article: http://dx.doi.org/10.1080/01431169208904025 PLEASE SCROLL DOWN FOR ARTICLE Full terms and conditions of use: http://www.tandfonline.com/page/terms-and-conditions This article may be used for research, teaching, and private study purposes. Any substantial or systematic reproduction, redistribution, reselling, loan, sub-licensing, systematic supply, or distribution in any form to anyone is expressly forbidden. The publisher does not give any warranty express or implied or make any representation that the contents will be complete or accurate or up to date. The accuracy of any instructions, formulae, and drug doses should be independently verified with primary sources. The publisher shall not be liable for any loss, actions, claims, proceedings, demand, or costs or damages whatsoever or howsoever caused arising directly or indirectly in connection with or arising out of the use of this material. -
'The Long Silence'
Just on a hundred years ago, on 31 March 1909, a small crowd of people gathered in the pre- dawn gloom of Darling Harbour, waiting for a steamer to arrive. Professor T.W.Edgeworth David was returning to Sydney after an absence of 15 months, during which time he had served as leader of the scientific team on Ernest Shackleton’s Antarctic expedition, undertaken a climb of the volcanic Mt Erebus and successfully completed a hazardous journey to the vicinity of the South Magnetic Pole. He was returning to Australia a popular hero. Many in the waiting crowd were students, young men and women from David’s geology department at the University of Sydney. It was a cold morning and people were muffled in scarves and overcoats. They stood around in subdued conversation or passed the time watching the loading of coal on the many ships berthed there under the glare of huge electric lights. At 5am the first rays of sun appeared and soon afterwards a vessel glided into view through the fog. The Sydney Mail described the arrival: ‘ A tall figure on the steamer’s deck was looking eagerly at the crowd on the wharf. There was no mistaking that old, familiar form.’ An undergraduate yelled, ‘“I see you’ve got your old brown hat on...” And, greeted with smiles and hand-wringing, Professor David was home from Antarctica.’ * * * * * * * In 1907 Edgeworth David had learnt that Ernest Shackleton, a veteran of Robert Scott’s polar expedition of 1901/2, was raising funds for a new expedition to the Antarctic. -
Leadership Lessons from Sir Douglas Mawson
LEADERSHIP LESSONS FROM SIR DOUGLAS MAWSON Sir Douglas Mawson was one of the most courageous and adventurous men Australia has produced. Through his determination and efforts he added to the Commonwealth an area in Antarctica almost as large as Australia itself. He was born in Yorkshire, England May 1882 and at the age of four his parents migrated to Sydney. He was educated at the University of Sydney and played a leading role in founding the Science Society. His great interest was geology and in 1902 he joined expeditions to survey the land around Mittagong and later the New Hebrides Islands. In 1905 he was appointed Lecturer in Mineralogy and Petrology at the University of Adelaide which he served in various capacities until his death. In 1907 a tour of the Snowy Mountains became his first experience of a glacial environment with an ascent of Mount Kosciusko and the beginning of his interest in Antarctica. At this time Britain, Germany and Sweden were involved in Antarctica, Ernest Shackleton was determined to reach the South Pole and in 1907 lead a party with Mawson joining as physicist and surveyor of the expedition. They reached the continent in February 1908 and Shackleton decided that Mawson, Professor Edgeworth David and Dr Forbes MacKay should travel 1800km to the Magnetic Pole. During the expedition they met very bad surfaces and some blizzards and they had underestimated the distance to the Magnetic Pole. While they reached their destination all were in poor condition with only seal meat to eat. They struggled back over hundreds of kilometres of ice caps and at last saw their ship, the Nimrod, less than a kilometre away when suddenly Mawson fell six metres down a crevasse. -
Meet... Douglas Mawson
TEACHERS’ RESOURCES RECOMMENDED FOR Lower and upper primary CONTENTS 1. Plot summary 1 2. About the author 2 3. About the illustrator 2 4. Interview with the author 2 5. Pre-reading questions 2 6. Key study topics 3 7. Other books in this series 4 8. Worksheets 5 KEY CURRICULUM AREAS Learning areas: History, English, Literacy THEMES Australian History Exploration Antarctica PREPARED BY Meet Douglas Mawson Penguin Random House Australia PUBLICATION DETAILS Written by Mike Dumbleton ISBN: 9780857981950 (hardback) Illustrated by Snip Green ISBN: 9780857981974 (ebook) ISBN: 9780857981967 (paperback) These notes may be reproduced free of charge for use and study within schools but they may not be PLOT SUMMARY reproduced (either in whole or in part) and offered for commercial sale. The year 2014 marks the 100th anniversary of the first Australian Antarctic Expedition (1911–14), led Visit penguin.com.au/teachers to find out how our fantastic Penguin Random House Australia books by Douglas Mawson. can be used in the classroom, sign up to the teachers’ newsletter and follow us on In this book, we follow Mawson and his team on @penguinteachers. their journey to Antarctica, as well as on their dangerous and challenging trek across the frozen Copyright © Penguin Random House Australia continent as they attempt to gather scientific and 2014 geological information. Meet Douglas Mawson Mike Dumbleton & Snip Green ABOUT THE AUTHOR 4. What was the most challenging part of the project? Mike Dumbleton is a writer with many educational It was a challenge to tell the story in a way that and children’s books to his credit. -
Rather Than Imposing Thematic Unity Or Predefining a Common Theoretical
The Supernatural Arctic: An Exploration Shane McCorristine, University College Dublin Abstract The magnetic attraction of the North exposed a matrix of motivations for discovery service in nineteenth-century culture: dreams of wealth, escape, extreme tourism, geopolitics, scientific advancement, and ideological attainment were all prominent factors in the outfitting expeditions. Yet beneath this „exoteric‟ matrix lay a complex „esoteric‟ matrix of motivations which included the compelling themes of the sublime, the supernatural, and the spiritual. This essay, which pivots around the Franklin expedition of 1845-1848, is intended to be an exploration which suggests an intertextuality across Arctic time and geography that was co-ordinated by the lure of the supernatural. * * * Introduction In his classic account of Scott‟s Antarctic expedition Apsley Cherry- Garrard noted that “Polar exploration is at once the cleanest and most isolated way of having a bad time which has been devised”.1 If there is one single question that has been asked of generations upon generations of polar explorers it is, Why?: Why go through such ordeals, experience such hardship, and take such risks in order to get from one place on the map to another? From an historical point of view, with an apparent fifty per cent death rate on polar voyages in the long nineteenth century amid disaster after disaster, the weird attraction of the poles in the modern age remains a curious fact.2 It is a less curious fact that the question cui bono? also featured prominently in Western thinking about polar exploration, particularly when American expeditions entered the Arctic 1 Apsley Cherry-Garrard, The Worst Journey in the World. -
Mid-Holocene Pulse of Thinning in the Weddell Sea Sector of the West Antarctic Ice Sheet
ARTICLE Received 9 Feb 2016 | Accepted 9 Jul 2016 | Published 22 Aug 2016 DOI: 10.1038/ncomms12511 OPEN Mid-Holocene pulse of thinning in the Weddell Sea sector of the West Antarctic ice sheet Andrew S. Hein1, Shasta M. Marrero1, John Woodward2, Stuart A. Dunning2,3, Kate Winter2, Matthew J. Westoby2, Stewart P.H.T. Freeman4, Richard P. Shanks4 & David E. Sugden1 Establishing the trajectory of thinning of the West Antarctic ice sheet (WAIS) since the last glacial maximum (LGM) is important for addressing questions concerning ice sheet (in)stability and changes in global sea level. Here we present detailed geomorphological and cosmogenic nuclide data from the southern Ellsworth Mountains in the heart of the Weddell Sea embayment that suggest the ice sheet, nourished by increased snowfall until the early Holocene, was close to its LGM thickness at 10 ka. A pulse of rapid thinning caused the ice elevation to fall B400 m to the present level at 6.5–3.5 ka, and could have contributed 1.4–2 m to global sea-level rise. These results imply that the Weddell Sea sector of the WAIS contributed little to late-glacial pulses in sea-level rise but was involved in mid-Holocene rises. The stepped decline is argued to reflect marine downdraw triggered by grounding line retreat into Hercules Inlet. 1 School of GeoSciences, University of Edinburgh, Drummond Street, Edinburgh EH8 9XP, UK. 2 Department of Geography, Northumbria University, Ellison Place, Newcastle upon Tyne NE1 8ST, UK. 3 School of Geography, Politics and Sociology, Newcastle University, Newcastle upon Tyne NE1 7RU, UK.