Antarctic Primer
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Introduction Itinerary
ANTARCTICA - AKADEMIK SHOKALSKY TRIP CODE ACHEIWM DEPARTURE 10/02/2022 DURATION 25 Days LOCATIONS East Antarctica INTRODUCTION This is a 25 day expedition voyage to East Antarctica starting and ending in Invercargill, New Zealand. The journey will explore the rugged landscape and wildlife-rich Subantarctic Islands and cross the Antarctic circle into Mawsonâs Antarctica. Conditions depending, it will hope to visit Cape Denison, the location of Mawsonâs Hut. East Antarctica is one of the most remote and least frequented stretches of coast in the world and was the fascination of Australian Antarctic explorer, Sir Douglas Mawson. A true Australian hero, Douglas Mawson's initial interest in Antarctica was scientific. Whilst others were racing for polar records, Mawson was studying Antarctica and leading the charge on claiming a large chunk of the continent for Australia. On his quest Mawson, along with Xavier Mertz and Belgrave Ninnis, set out to explore and study east of the Mawson's Hut. On what began as a journey of discovery and science ended in Mertz and Ninnis perishing and Mawson surviving extreme conditions against all odds, with next to no food or supplies in the bitter cold of Antarctica. This expedition allows you to embrace your inner explorer to the backdrop of incredible scenery such as glaciers, icebergs and rare fauna while looking out for myriad whale, seal and penguin species. A truly unique journey not to be missed. ITINERARY DAY 1: Invercargill Arrive at Invercargill, New Zealand’s southernmost city. Established by Scottish settlers, the area’s wealth of rich farmland is well suited to the sheep and dairy farms that dot the landscape. -
Annual Report COOPERATIVE INSTITUTE for RESEARCH in ENVIRONMENTAL SCIENCES
2015 Annual Report COOPERATIVE INSTITUTE FOR RESEARCH IN ENVIRONMENTAL SCIENCES COOPERATIVE INSTITUTE FOR RESEARCH IN ENVIRONMENTAL SCIENCES 2015 annual report University of Colorado Boulder UCB 216 Boulder, CO 80309-0216 COOPERATIVE INSTITUTE FOR RESEARCH IN ENVIRONMENTAL SCIENCES University of Colorado Boulder 216 UCB Boulder, CO 80309-0216 303-492-1143 [email protected] http://cires.colorado.edu CIRES Director Waleed Abdalati Annual Report Staff Katy Human, Director of Communications, Editor Susan Lynds and Karin Vergoth, Editing Robin L. Strelow, Designer Agreement No. NA12OAR4320137 Cover photo: Mt. Cook in the Southern Alps, West Coast of New Zealand’s South Island Birgit Hassler, CIRES/NOAA table of contents Executive summary & research highlights 2 project reports 82 From the Director 2 Air Quality in a Changing Climate 83 CIRES: Science in Service to Society 3 Climate Forcing, Feedbacks, and Analysis 86 This is CIRES 6 Earth System Dynamics, Variability, and Change 94 Organization 7 Management and Exploitation of Geophysical Data 105 Council of Fellows 8 Regional Sciences and Applications 115 Governance 9 Scientific Outreach and Education 117 Finance 10 Space Weather Understanding and Prediction 120 Active NOAA Awards 11 Stratospheric Processes and Trends 124 Systems and Prediction Models Development 129 People & Programs 14 CIRES Starts with People 14 Appendices 136 Fellows 15 Table of Contents 136 CIRES Centers 50 Publications by the Numbers 136 Center for Limnology 50 Publications 137 Center for Science and Technology -
A Sheffield Hallam University Thesis
The polar sublime in contemporary poetry of Arctic and Antarctic exploration. JACKSON, Andrew Buchanan. Available from the Sheffield Hallam University Research Archive (SHURA) at: http://shura.shu.ac.uk/20170/ A Sheffield Hallam University thesis This thesis is protected by copyright which belongs to the author. The content must not be changed in any way or sold commercially in any format or medium without the formal permission of the author. When referring to this work, full bibliographic details including the author, title, awarding institution and date of the thesis must be given. Please visit http://shura.shu.ac.uk/20170/ and http://shura.shu.ac.uk/information.html for further details about copyright and re-use permissions. jj Learning and information Services I Adsetts Centre, City Campus * Sheffield S1 1WD 102 156 549 0 REFERENCE ProQuest Number: 10700005 All rights reserved INFORMATION TO ALL USERS The quality of this reproduction is dependent upon the quality of the copy submitted. In the unlikely event that the author did not send a com plete manuscript and there are missing pages, these will be noted. Also, if material had to be removed, a note will indicate the deletion. uest ProQuest 10700005 Published by ProQuest LLC(2017). Copyright of the Dissertation is held by the Author. All rights reserved. This work is protected against unauthorized copying under Title 17, United States C ode Microform Edition © ProQuest LLC. ProQuest LLC. 789 East Eisenhower Parkway P.O. Box 1346 Ann Arbor, Ml 48106- 1346 The Polar Sublime in Contemporary Poetry of Arctic and Antarctic Exploration Andrew Buchanan Jackson A thesis submitted in partial fulfilment of the requirements of Sheffield Hallam University for the degree of Doctor of Philosophy September 2015 Abstract In this thesis I formulate the concept of a polar sublime, building on the work of Chauncy Loomis and Francis Spufford, and use this new framework for the appraisal of contemporary polar-themed poetry. -
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. -
Growth and Seasonal Energetics of the Antarctic Bivalve Laternula Elliptica from King George Island, Antarctica
MARINE ECOLOGY PROGRESS SERIES Vol. 257: 99–110, 2003 Published August 7 Mar Ecol Prog Ser Growth and seasonal energetics of the Antarctic bivalve Laternula elliptica from King George Island, Antarctica In-Young Ahn1,*, Jeonghee Surh2, You-Gyoung Park2, Hoonjeong Kwon2, Kwang-Sik Choi3, Sung-Ho Kang1, Heeseon J. Choi1, Ko-Woon Kim1, Hosung Chung1 1Polar Sciences Laboratory, Korea Ocean Research & Development Institute (KORDI), Ansan, PO Box 29, Seoul 425-600, Republic of Korea 2Department of Food and Nutrition, Seoul National University, Sillim-dong, Kwanak-ku, Seoul 151-742, Republic of Korea 3Department of Aquaculture, Cheju National University, Ara-1-dong, Cheju 690-756, Republic of Korea ABSTRACT: The Antarctic marine environment is characterized by extreme seasonality in primary production, and herbivores must cope with a prolonged winter period of food shortage. In this study, tissue mass and biochemical composition were determined for various tissues of the bivalve Later- nula elliptica (King & Broderip) over a 2 yr period, and its storage and use of energy reserves were investigated with respect to seasonal changes in food level and water temperature. Total ash-free dry mass (AFDM) accumulated rapidly following phytoplankton blooms (with peak values immediately before and after spawning) and was depleted considerably during the spawning and winter periods. Most of the variation was in the muscle, gonads and digestive gland. Spawning peaked in January and February and caused considerable protein and lipid losses in the muscle, gonads and digestive gland. In winter (March to August), the muscle and digestive gland lost considerable mass, while gonad mass increased; this suggests that the muscle tissue and digestive gland serve as major energy depots for both maintenance metabolism and gonad development in winter. -
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. -
A History of the Exploitation of the Ross Sea, Antarctica David G
Polar Record 46 (238): 233–243 (2010). c Cambridge University Press 2009. doi:10.1017/S003224740999009X 233 ! A history of the exploitation of the Ross Sea, Antarctica David G. Ainley H.T. Harvey and Associates, 983 University Avenue, Building D, Los Gatos, CA 95032, USA ([email protected]) Received March 2009 ABSTRACT. Recent analyses of anthropogenic impacts on marine systems have shown that the Ross Sea is the least affected stretch of ocean on Earth, although historical effects were not included in those studies. Herein the literature is reviewed in order to quantify the extent of extraction of biological resources from the Ross Sea continental shelf and slope from the start of the 20th century. There was none before that time. An intense extraction of Weddell seals Leptonychotes weddellii by the expeditions of the ‘heroic’ period and then by New Zealand to feed sled dogs in the 1950–1980s caused the McMurdo Sound population to decrease permanently. Otherwise no other sealing occurred. Blue whales Balaenoptera musculus intermedia were extirpated from waters of the shelf break front during the 1920s, and have not reappeared. Minke whales B. bonaerensis probably expanded into the blue whale vacated habitat, but were then hunted during the 1970–1980s; their population has since recovered. Some minke whales are now taken in ‘scientific whaling’, twice more from the slope compared to the shelf. Other hunted cetaceans never occurred over the shelf and very few ever occurred in slope waters, and therefore their demise from whaling does not apply to the Ross Sea. No industrial fishing occurred in the Ross Sea until the 1996–1997 summer, when a fishery for Antarctic toothfish Dissostichus mawsoni was initiated, especially along the slope. -
Chinstrap Penguin Declines
Author's personal copy Polar Biol DOI 10.1007/s00300-012-1230-3 ORIGINAL PAPER First direct, site-wide penguin survey at Deception Island, Antarctica, suggests significant declines in breeding chinstrap penguins Ron Naveen • Heather J. Lynch • Steven Forrest • Thomas Mueller • Michael Polito Received: 18 April 2012 / Revised: 25 July 2012 / Accepted: 31 July 2012 Ó Springer-Verlag 2012 Abstract Deception Island (62°570S, 60°380W) is one of 1986/1987. A comparative analysis of high-resolution satel- the most frequently visited locations in Antarctica, prompt- lite imagery for the 2002/2003 and the 2009/2010 seasons ing speculation that tourism may have a negative impact suggests a 39 % (95th percentile CI = 6–71 %) decline on the island’s breeding chinstrap penguins (Pygoscelis (from 85,473 ± 23,352 to 52,372 ± 14,309 breeding pairs) antarctica). Discussions regarding appropriate management over that 7-year period and provides independent confirma- of Deception Island and its largest penguin colony at Baily tion of population decline in the abundance of breeding Head have thus far operated in the absence of concrete chinstrap penguins at Baily Head. The decline in chinstrap information regarding the current size of the penguin popu- penguins at Baily Head is consistent with declines in this lation at Deception Island or long-term changes in abun- species throughout the region, including sites that receive dance. In the first ever field census of individual penguin little or no tourism; as a consequence of regional environ- nests at Deception Island (December 2–14, 2011), we find mental changes that currently represent the dominant influ- 79,849 breeding pairs of chinstrap penguins, including ence on penguin dynamics, we cannot ascribe any direct link 50,408 breeding pairs at Baily Head and 19,177 breeding between chinstrap declines and tourism from this study. -
Emperor Island, Dion Islands, Marguerite Bay, Antarctic Peninsula
From Measure 1 (2002) Management Plan for Antarctic Specially Protected Area No. 107 EMPEROR ISLAND, DION ISLANDS, MARGUERITE BAY, ANTARCTIC PENINSULA 1. Description of values to be protected The Dion Islands (Latitude 67°52’ S, Longitude 68°42’ W), on the western side of the central Antarctic Peninsula in north-western Marguerite Bay, were originally designated as Specially Protected Area (SPA) No. 8 through Recommendation IV-8 in 1966 after a proposal by the United Kingdom. All of the islands in the Dion Islands archipelago were included. Values protected under the original designation were described as the presence of the only colony of emperor penguins (Aptenodytes forsteri) known to exist on the west side of the Antarctic Peninsula and that the isolation of this colony from others of the same species makes it of outstanding scientific interest. A management plan for the Area was adopted through Recommendation XVI-6 (1990), which reaffirmed the values of the Area. The boundaries were extended to include the intervening sea between the islands to ensure protection of the emperors at sea or on sea-ice in the immediate vicinity. Attention was drawn to the additional important value of the colony being one of only two known in which breeding occurs on land. It was also noted as the most northerly and probably the smallest of Emperor colonies, with annual numbers fluctuating around 150 pairs. The values of the emperor penguin colony are reaffirmed in this revised management plan. The boundaries of the Area are now defined more precisely. -
Management Plan for Antarctic Specially Protected Area No
Management Plan for Antarctic Specially Protected Area No. 108 GREEN ISLAND, BERTHELOT ISLANDS, ANTARCTIC PENINSULA 1. Description of values to be protected Green Island (Latitude 65°19' S, Longitude 64°09' W, approximately 0.2 km2), Berthelot Islands, Grandidier Channel, Antarctic Peninsula, was originally designated as a Specially Protected Area through Recommendation IV-9 (1966, SPA No. 9) after a proposal by the United Kingdom. It was designated on the grounds that the vegetation “is exceptionally rich, [and] is probably the most luxuriant anywhere on the west side of the Antarctic Peninsula”. The Recommendation noted: “in some places the humus is 2 metres thick and that this area, being of outstanding scientific interest, should be protected because it is probably one of the most diverse Antarctic ecosystems”. A Management Plan for the site was prepared by the United Kingdom and adopted through Recommendation XVI-6 (1991). The original reasons for designation were extended and elaborated, although following comparisons to other sites in the vicinity, Green Island was no longer considered to be particularly diverse. The vegetation on the island was described as extensive on the north-facing slopes, with well-developed continuous banks of moss turf formed by Chorisodontium aciphyllum and Polytrichum strictum that, over much of their extent, overlie peat of more than one metre in depth. Antarctic hair grass (Deschampsia antarctica), one of only two native vascular plants that grow south of 56°S, was noted as frequent in small patches near a blue-eyed cormorant (Phalacrocorax atriceps) colony. The colony of blue- eyed cormorants, located on the steep, rocky northwestern corner of the island, was noted as being possibly one of the largest along the Antarctic Peninsula. -
GSA TODAY • Southeastern Section Meeting, P
Vol. 5, No. 1 January 1995 INSIDE • 1995 GeoVentures, p. 4 • Environmental Education, p. 9 GSA TODAY • Southeastern Section Meeting, p. 15 A Publication of the Geological Society of America • North-Central–South-Central Section Meeting, p. 18 Stability or Instability of Antarctic Ice Sheets During Warm Climates of the Pliocene? James P. Kennett Marine Science Institute and Department of Geological Sciences, University of California Santa Barbara, CA 93106 David A. Hodell Department of Geology, University of Florida, Gainesville, FL 32611 ABSTRACT to the south from warmer, less nutrient- rich Subantarctic surface water. Up- During the Pliocene between welling of deep water in the circum- ~5 and 3 Ma, polar ice sheets were Antarctic links the mean chemical restricted to Antarctica, and climate composition of ocean deep water with was at times significantly warmer the atmosphere through gas exchange than now. Debate on whether the (Toggweiler and Sarmiento, 1985). Antarctic ice sheets and climate sys- The evolution of the Antarctic cryo- tem withstood this warmth with sphere-ocean system has profoundly relatively little change (stability influenced global climate, sea-level his- hypothesis) or whether much of the tory, Earth’s heat budget, atmospheric ice sheet disappeared (deglaciation composition and circulation, thermo- hypothesis) is ongoing. Paleoclimatic haline circulation, and the develop- data from high-latitude deep-sea sed- ment of Antarctic biota. iments strongly support the stability Given current concern about possi- hypothesis. Oxygen isotopic data ble global greenhouse warming, under- indicate that average sea-surface standing the history of the Antarctic temperatures in the Southern Ocean ocean-cryosphere system is important could not have increased by more for assessing future response of the Figure 1. -
36. Comparison of Winter and Summer Growth Stages of the Diatom Eucampia Antarctica from the Kerguelen Plateau and South of the Antarctic Convergence Zone1
Barron, J., Larsen, B., et al., 1991 Proceedings of the Ocean Drilling Program, Scientific Results, Vol. 119 36. COMPARISON OF WINTER AND SUMMER GROWTH STAGES OF THE DIATOM EUCAMPIA ANTARCTICA FROM THE KERGUELEN PLATEAU AND SOUTH OF THE ANTARCTIC CONVERGENCE ZONE1 Greta A. Fryxell2 ABSTRACT On ODP Leg 119, specimens collected of Eucampia antarctica (Castracane) Mangin var. antarctica exhibited mor- phological and distribution patterns that contrasted with those of Eucampia antarctica var. recta (Mangin) G. Fryxell et Prasad. E. antarctica var. antarctica was found over the northern Kerguelen Plateau, north of the summer Antarctic Convergence Zone, in the subpolar plankton and in the sediments. E. antarctica var. recta was found close to the conti- nent in Prydz Bay. It was also collected near and under the ice in the northern Weddell Sea on a National Science Foun- dation Division of Polar Programs project (1983-1988). A key feature for distinguishing the two varieties in the field is the growth habit, with curvature in broad girdle view of the nominate, subpolar variety in both the winter stage and the more lightly silicified summer stage. A low ratio of terminal to intercalary valves results from the repeated division of the original doublets into chains of considerable length of the winter stage. Small spines around the elevations of one valve serve to clasp the sibling valve and maintain the chain formation. Cells of E. antarctica var. recta tend to be somewhat larger than E. antarctica var. antarctica, and they form chains that are straight in broad girdle view but slightly curved in narrow girdle view.