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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 -
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. -
Why the 'Infrastructure PM' Can't Give Antarctica the Cold Shoulder
Please do not remove this page Why the ‘infrastructure PM’ can’t give Antarctica the cold shoulder McCallum, Adrian B https://research.usc.edu.au/discovery/delivery/61USC_INST:ResearchRepository/12126045700002621?l#13127312320002621 McCallum, A. B. (2013). Why the “infrastructure PM” can’t give Antarctica the cold shoulder. The Conversation, 5 December 2013. https://research.usc.edu.au/discovery/fulldisplay/alma99448982602621/61USC_INST:ResearchRepository Document Type: Published Version USC Research Bank: https://research.usc.edu.au [email protected] CC BY V4.0 Copyright © 2013 The Conversation Media Group. This work is licensed under a Creative Commons Attribution 4.0 International License (http://creativecommons.org/licenses/by/4.0/) Downloaded On 2021/10/02 23:37:22 +1000 Please do not remove this page 26/02/2016 Why the 'infrastructure PM' can't give Antarctica the cold shoulder Why the ‘infrastructure PM’ can’t give Antarctica the cold shoulder December 6, 2013 6.35am AEDT Tractors and quad bikes – seen here at Australia’s Mawson Station – are only two of many forms of transport used in Antarctica. Chris Wilson/Australian Antarctic Division Adrian McCallum Lecturer in Science and Engineering, University of the Sunshine Coast Prime Minister Tony Abbott recently declared that he wanted to be known as the “infrastructure prime minister”. But what of Australia’s iciest infrastructure – that located in Antarctica? A 20year strategic plan for Australia’s Antarctic future was recently commissioned by the federal government, but it will be another six months before Tony Press, exdirector of the Australian Antarctic Division, reveals his “blueprint”. So what is best practice when it comes to polar infrastructure, and where should Australia be heading to maintain our status as a leader in Antarctic science and operations? Stations The British Antarctic Survey completed construction of their new Halley VI Station on the floating Brunt Ice Shelf, atop the Weddell Sea, East Antarctica in 2012. -
Polarforschungsagenda Status Und Perspektiven Der Deutschen
Polarforschungsagenda 2030 Status und Perspektiven der deutschen Polarforschung DFG-Statusbericht des Deutschen Nationalkomitees SCAR/IASC Polarforschungsagenda 2030 Status und Perspektiven der deutschen Polarforschung DFG-Statusbericht des Deutschen Nationalkomitees für Scientific Committee on Antarctic Research (SCAR) und International Arctic Science Committee (IASC) Deutsches Nationalkomitee SCAR/IASC Prof. G. Heinemann (Vorsitzender) Universität Trier, Fachbereich Raum- und Umweltwissenschaften Postanschrift: Behringstr. 21, 54296 Trier Telefon: +49/651/201-4630 Telefax: +49/651/201-3817 E-Mail: [email protected] www.scar-iasc.de Juli 2017 Das vorliegende Werk wurde sorgfältig erarbeitet. Dennoch übernehmen Autoren, Herausgeber und Verlag für die Richtigkeit von Angaben, Hinweisen und Ratschlägen sowie für eventuelle Druckfehler keine Haftung. Alle Rechte, insbesondere die der Übersetzung in andere Sprachen, vorbehalten. Kein Teil dieser Publikation darf ohne schrift- liche Genehmigung des Verlages in irgendeiner Form – durch Photokopie, Mikroverfilmung oder irgendein anderes Verfahren – reproduziert oder in eine von Maschinen, insbesondere von Datenverarbeitungsmaschinen, verwendbare Sprache übertra- gen oder übersetzt werden. Die Wiedergabe von Warenbezeichnungen, Handelsnamen oder sonstigen Kennzeichen in diesem Buch berechtigt nicht zu der Annahme, dass diese von jedermann frei benutzt werden dürfen. Vielmehr kann es sich auch dann um eingetragene Warenzeichen oder sonstige gesetzlich geschützte Kennzeichen handeln, wenn sie nicht eigens als solche markiert sind. All rights reserved (including those of translation into other languages). No part of this book may be reproduced in any form – by photoprinting, microfilm, or any other means – nor transmitted or translated into a machine language without written permission from the publishers. Registered names, trademarks, etc. used in this book, even when not specifically marked as such, are not to be considered unprotected by law. -
Hnitflrcitilc
HNiTflRCiTilC A NEWS BULLETIN published quarterly by the NEW ZEALAND ANTARCTIC SOCIETY (INC) ,m — i * Halley, the British Antarctic Survey's station on the Brunt Ice Shelf, Coats Land,, was rebuilt last season for the third time since 1956-57. This picture taken in March shows one of the four wooden tubes, each of which houses a two-storey building, under construction in a pre-shaped and compacted snow hollow. BAS Copyngh! Registered at Post Office Headquarters, Vol. 10, No. 2 Wellington, New Zealand, as a magazine. SOUTH GEORGIA -.. SOUTH SANDWICH Is «C*2K SOUTH ORKNEY Is x \ 6SignyluK //o Orcadas arg SOUTH AMERICA / /\ ^ Borga T"^00Molodezhnaya \^' 4 south , * /weooEii \ ft SA ' r-\ *r\USSR --A if SHETLAND ,J£ / / ^^Jf ORONMIIDROWNING MAUD LAND' E N D E R B Y \ ] > * \ /' _ "iV**VlX" JN- S VDruzhnaya/General /SfA/ S f Auk/COATS ' " y C O A TBelirano SLd L d l arg L A N D p r \ ' — V&^y D««hjiaya/cenera.1 Beld ANTARCTIC •^W^fCN, uSS- fi?^^ /K\ Mawson \ MAC ROBERTSON LAN0\ \ *usi \ /PENINSULA' ^V^/^CRp^e J ^Vf (set mjp Mow) C^j V^^W^gSobralARG - Davis aust L Siple USA Amundsen-Scon OUEEN MARY LAND flMimy ELLSWORTH , U S A / ^ U S S R ') LAND °Vos1okussR/ r». / f c i i \ \ MARIE BYRO fee Shelf V\ . IAND WILKES LAND Scon ROSS|N2i? SEA jp>r/VICTORIAIj^V .TERRE ,; ' v / I ALAND n n \ \^S/ »ADEUL. n f i i f / / GEORGE V Ld .m^t Dumom d'Urville iranu Leningradskayra V' USSR,.'' \ -------"'•BAlLENYIs^ ANTARCTIC PENINSULA 1 Teniente Matienzo arc 2 Esperanza arg 3 Almirante Brown arg 4 Petrel arg 5 Decepcion arg 6 Vicecomodoro Marambio arg ' ANTARCTICA 7 Ariuro Prat chile 500 1000 Miles 8 Bernardo O'Higgms chile 9 Presidente Frei chile - • 1000 Kilomnre 10 Stonington I. -
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. -
Mount Harding, Grove Mountains, East Antarctica
MEASURE 2 - ANNEX Management Plan for Antarctic Specially Protected Area No 168 MOUNT HARDING, GROVE MOUNTAINS, EAST ANTARCTICA 1. Introduction The Grove Mountains (72o20’-73o10’S, 73o50’-75o40’E) are located approximately 400km inland (south) of the Larsemann Hills in Princess Elizabeth Land, East Antarctica, on the eastern bank of the Lambert Rift(Map A). Mount Harding (72°512 -72°572 S, 74°532 -75°122 E) is the largest mount around Grove Mountains region, and located in the core area of the Grove Mountains that presents a ridge-valley physiognomies consisting of nunataks, trending NNE-SSW and is 200m above the surface of blue ice (Map B). The primary reason for designation of the Area as an Antarctic Specially Protected Area is to protect the unique geomorphological features of the area for scientific research on the evolutionary history of East Antarctic Ice Sheet (EAIS), while widening the category in the Antarctic protected areas system. Research on the evolutionary history of EAIS plays an important role in reconstructing the past climatic evolution in global scale. Up to now, a key constraint on the understanding of the EAIS behaviour remains the lack of direct evidence of ice sheet surface levels for constraining ice sheet models during known glacial maxima and minima in the post-14 Ma period. The remains of the fluctuation of ice sheet surface preserved around Mount Harding, will most probably provide the precious direct evidences for reconstructing the EAIS behaviour. There are glacial erosion and wind-erosion physiognomies which are rare in nature and extremely vulnerable, such as the ice-core pyramid, the ventifact, etc. -
Downloaded 10/01/21 06:40 AM UTC 3112 JOURNAL of CLIMATE VOLUME 10
DECEMBER 1997 VAN DEN BROEKE ET AL. 3111 Representation of Antarctic Katabatic Winds in a High-Resolution GCM and a Note on Their Climate Sensitivity MICHIEL R. VAN DEN BROEKE Norwegian Polar Institute, Oslo, Norway RODERIK S. W. VAN DE WAL Institute for Marine and Atmospheric Research, Utrecht University, Utrecht, the Netherlands MARTIN WILD Department of Geography, Swiss Federal Institute of Technology, Zurich, Switzerland (Manuscript received 7 October 1996, in ®nal form 25 April 1997) ABSTRACT A high-resolution GCM (ECHAM-3 T106, resolution 1.1831.18) is found to simulate many characteristic features of the Antarctic climate. The position and depth of the circumpolar storm belt, the semiannual cycle of the midlatitude westerlies, and the temperature and wind ®eld over the higher parts of the ice sheet are well simulated. However, the strength of the westerlies is overestimated, the annual latitudinal shift of the storm belt is suppressed, and the wintertime temperature and wind speed in the coastal areas are underestimated. These errors are caused by the imperfect simulation of the position of the subtropical ridge, the prescribed sea ice characteristics, and the smoothened model topography in the coastal regions. Ice shelves in the model are erroneously treated as sea ice, which leads to a serious overestimation of the wintertime surface temperature in these areas. In spite of these de®ciencies, the model results show much improvement over earlier simulations. In a climate run, the model was forced to a new equilibrium state under enhanced greenhouse conditions (IPCC scenario A, doubled CO2), which enables us to cast a preliminary look at the climate sensitivity of Antarctic katabatic winds. -
Introducing Katabatic Winds in Global ERA40 Fields to Simulate Their
Introducing katabatic winds in global ERA40 fields to simulate their impacts on the Southern Ocean and sea-ice Pierre Mathiot, Bernard Barnier, Hubert Gallée, Jean-Marc Molines, Julien Le Sommer, Mélanie Juza, Thierry Penduff To cite this version: Pierre Mathiot, Bernard Barnier, Hubert Gallée, Jean-Marc Molines, Julien Le Sommer, et al.. In- troducing katabatic winds in global ERA40 fields to simulate their impacts on the Southern Ocean and sea-ice. Ocean Modelling, Elsevier, 2010, 35 (3), pp.146-160. 10.1016/j.ocemod.2010.07.001. hal-00570152 HAL Id: hal-00570152 https://hal.archives-ouvertes.fr/hal-00570152 Submitted on 13 Feb 2020 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. Introducing katabatic winds in global ERA40 fields to simulate their impacts on the Southern Ocean and sea-ice Pierre Mathiot a,d,*, Bernard Barnier a, Hubert Gallée b, Jean Marc Molines a, Julien Le Sommer a, Mélanie Juza a, Thierry Penduff a,c a LEGI UMR5519, CNRS, UJF, Grenoble, France b LGGE UMR5183, CNRS, UJF, Grenoble, France c FSU, Department of Oceanography, The Florida State University, Tallahassee, FL, United States d TECLIM, Earth and Life Institute, Université Catholique de Louvain, Louvain la Neuve, Belgium A medium resolution (10–20 km around Antarctica) global ocean/sea-ice model is used to evaluate the impact of katabatic winds on sea-ice and hydrography. -
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. -
Italian Contribution to Space Weather
Italian Contribution to Space Weather Vincenzo Romano Istituto Nazionale di Geofisica e Vulcanologia (INGV) [email protected] Thanks to: Mauro Messerotti (INAF), Daniele Biron (ITAF-COMET), Paola De Michelis (INGV), Francesca Zuccarello (Uni CT), Alessandro Bemporad (INAF), Ester Antonucci (INAF), Domenico Di Mauro (INGV). Lili Cafarella (INGV), Marco Pietrella (INGV), Anna Milillo (INAF), Francesco Berilli (UniTOV), Marco Stangalini (INAF), Mirko Piersanti (Uni AQ), Federica Marcucci (INAF), Lucilla Alfonsi (INGV), Enrico Zuccheretti (INGV), Massimo Materassi (ISC-CNR), Loredana Perrone (INGV), Stefania Lepidi (INGV), Yenca Migoya-Orue (ICTP), Fabio Reale (UNIPA), Roberto Piazzesi (INAF) Ionosonde and Pamela autoscaling SuperDarn Solar Orbiter Themis UN COPUOS 54rd Session STSC January-February 2017. Outline • Italian strategic Initiatives • Solar physics • Interplanetary space physics • Solar-Terrestrial physics • Upper atmosphere physics Ionosonde and Pamela autoscaling SuperDarn Solar Orbiter Themis Italian Space Weather strategic initiatives Pamela Ionosonde and autoscaling Solar Orbiter SuperDarn Themis World Meteorological Organization Congress Resolution 38 (Cg-17) ― “Four-year Plan for WMO Coordination of Space Weather Activities”. Since 2012 Italy joined the WMO Space Weather initiative Inter-programme Coordination Team on SW, ITAF – INAF - INGV Space Weather italian initiative for operations SW nowcasting and safety support Space Weather knowledge is not only for safety but also for capacity augmentation, as weather. Solar physics to Space Weather Solar Physics activities in Trieste ESA Space Weather Working Team, Steering Board Member European Space Weather Week Programme Committee, Chair NATO Science for Peace (SfP) Project 984894 on “Ionospheric Monitoring”, Co-Director Solar Orbiter/METIS Co-Investigator, Responsible for the Italian segment data handling Solar Physics Group in Catania Personnel V. -
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.