Polish Geographical Names of Undersea and Antarctic Features the Names Which “Escape” the Definition of Exonym and Endonym
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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 -
F!L3ljnew CITATIONS in COASTAL TOPICS • a
·/f1!f!!II:. f!l3lJNEW CITATIONS IN COASTAL TOPICS • A ., Addis, R.P.; Garstand, M., and Emmitt, G.D., J9R4. Downdrafts from tropical oceanic cumuli. Boundary-Layer Meteorology. 28(1-2).23-49. Admiraal, W.; Laane, R.W.P.M., and Peletier, H., 1984. Participation of diotoms in the amino-acid cycle of coastal waters uptake and excretion in cultures. Marine Ecology - Prowess Sf-ries. I ~(:1I. :lO:1-306. Ahmed, 8.T.; King, 8. L., and Clayton, J.R., 1984. Organic-mattler diagenesis in the anoxic sediments of Saanich Inlet. British Columbia. Canada - a case for highly evolved community interactions. Marine Chemistry. 14(3),233-252 Ajebouri, M.M. and Trollope, D.H., 1984. Indicator hacte'ia in fresh water and marine moUusks. HydrobioloRY, 111 (2), 9:l-1 02. Alam, M.; Piper, D.J.W., and Cooke, H.B.8., 198:\. Late Quaternarv stratigraphy and paleooceanography of the Crand Banks continental margin, eastern Canada. Boreas. \2(41. 25:1-2GI AIdabas, M.A.; Hybbard, F.H. , and McManus, J., 1984. The shell of Mytilus as an indicator of zonal variations of water quality within an estuary. Estuarine. Coastal and SI"'lf Science. I H(:ll. 2G:I-270. Allen, D.M., 1984. Population dynamics of the mysid shrimp Mysidop.,i., bili,-loll'i Tattersall. W.M. in a tern perate estuary. Jour nal of Crustacean Biology_ 4( 1).25':14 Allen, L.G. and Demartin, E.E., 198:\. Temporal and spatial patterns of nearshore distribution and abundance of the pelagic fishes off San Onofre Oceanside. Califol1lia. Fishery Rulll·tin, RI(:11. -
1 We Thank the Referees for Their Careful Review
We thank the referees for their careful review and thoughtful comments. Below please see our point-by-point responses and changes made to the manuscript. Referee report #1 Thank you for responding to my comments. It is now clearer what is going on, but some additional enhancements are desirable. You need to state clearly in the abstract and probably in the manuscript as well that you are using pre-industrial conditions to examine sea-ice generated Antarctic precipitation variability in the absence of anthropogenic forcing. This should appear explicitly in the first sentence of the abstract, I think, rather than being implicit here and throughout the manuscript. I am recommending minor revisions, but think that this is a very important aspect to address comprehensively to make the intent and methodology of your extensive work obvious to the reader. Done as suggested. Now the first sentence of the abstract reads “We conduct sensitivity experiments using a general circulation model that has an explicit water source tagging capability forced by prescribed composites of pre-industrial sea ice concentrations (SIC) and corresponding sea surface temperatures (SST) to understand the impact of sea ice anomalies on regional evaporation, moisture transport, and source–receptor relationships for Antarctic precipitation in the absence of anthropogenic forcing.” A similar statement is also made in the summary paragraph of the Introduction section: “In this study, we aim to understand the impact of SO sea ice anomalies associated with internal variability (in the absence of anthropogenic forcing) on local evaporation, moisture transport and source–receptor relationships for moisture and precipitation over Antarctica using a GCM that has an explicit water source tagging capability.” Section 3.2: You attribute southerly katabatic flow to the polar high. -
PROGETTO ANTARTIDE Rapporto Sulla Campagna Antartica Estate Australe 1996
PROGRAMMA NAZIONALE DI RICERCHE IN ANTARTIDE Rapporto sulla Campagna Antartica Estate Australe 1996 - 97 Dodicesima Spedizione PROGETTO ANTARTIDE ANT 97/02 PROGRAMMA NAZIONALE DI RICERCHE IN ANTARTIDE Rapporto sulla Campagna Antartica Estate Australe 1996 - 97 Dodicesima Spedizione A cura di J. Mϋller, T. Pugliatti, M.C. Ramorino, C.A. Ricci PROGETTO ANTARTIDE ENEA - Progetto Antartide Via Anguillarese,301 c.p.2400,00100 Roma A.D. Tel.: 06-30484816,Fax:06-30484893,E-mail:[email protected] I N D I C E Premessa SETTORE 1 - EVOLUZIONE GEOLOGICA DEL CONTINENTE ANTARTICO E DELL'OCEANO MERIDIONALE Area Tematica 1a Evoluzione Geologica del Continente Antartico Progetto 1a.1 Evoluzione del cratone est-antartico e del margine paleo-pacifico del Gondwana.3 Progetto 1a.2 Evoluzione mesozoica e cenozoica del Mare di Ross ed aree adiacenti..............11 Progetto 1a.3 Magmatismo Cenozoico del margine occidentale antartico..................................17 Progetto 1a.4 Cartografia geologica, geomorfologica e geofisica ...............................................18 Area Tematica 1b-c Margini della Placca Antartica e Bacini Periantartici Progetto 1b-c.1 Strutture crostali ed evoluzione cenozoica della Penisola Antartica e del margine coniugato cileno ......................................................................................25 Progetto 1b-c.2 Indagini geofisiche sul sistema deposizionale glaciale al margine pacifico della Penisola Antartica.........................................................................................42 -
A NEWS BULLETIN Published Quarterly by the NEW ZEALAND
A N E W S B U L L E T I N p u b l i s h e d q u a r t e r l y b y t h e NEW ZEALAND ANTARCTIC SOCIETY THESE VISITORS TO LAKE FRYXELL IN THE TAYLOR VALLEY ARE LIKE DWARFS AGAINST THE TOWERING CANADA GLACIER WHICH FLOWS DOWN FROM THE ASGAARD RANGE. —Photo by R. K. McBride. Antarctic Division, D.S.I.R. September 1972 «i (Successor to "Antarctic News Bulletin") Vol. 6, No. 7 67th ISSUE Editor: H. F. GRIFFITHS, 14 Woodchester Avenue, Christchurch 1. Assistant Editor: J. M. CAFFIN, 35 Chepstow Avenue, Christchurch 5. Address all contributions, enquiries, etc., to the Editor. All Business Communications, Subscriptions, etc., to: The Secretary, New Zealand Antarctic Society, P.O. Box 1223, Christchurch, N.Z CONTENTS ARTICLES SECOND-IN-COMMAND POLAR ACTIVITIES NEW ZEALAND 222, 225, 231, 240, 243, 251, 253 U.S.A 226, 232, 252 AUSTRALIA 236 UNITED KINGDOM 234 U.S.S.R 238, 239, 241 SOUTH AFRICA 242, 250 CZECHOSLOVAKIA 235 SUB-ANTARCTIC CAMPBELL ISLAND GENERAL LONE TRIP TO POLE DISCOVERY EXPEDITION LETTERS WHALING QUOTAS FIXED ANTARCTIC BOOKSHELF Fifteen years have passed since the International Geophysical Year of 1957-58 and it might be thought that the Antarctic Continent, through the continuing research carried out by the participating nations, would by now have yielded up all its secrets. But this is a false premise; new discoveries in the various branches of science have either highlighted gaps in our knowledge or have pointed the way to investigation in new fields. -
Data Structure
Data structure – Water The aim of this document is to provide a short and clear description of parameters (data items) that are to be reported in the data collection forms of the Global Monitoring Plan (GMP) data collection campaigns 2013–2014. The data itself should be reported by means of MS Excel sheets as suggested in the document UNEP/POPS/COP.6/INF/31, chapter 2.3, p. 22. Aggregated data can also be reported via on-line forms available in the GMP data warehouse (GMP DWH). Structure of the database and associated code lists are based on following documents, recommendations and expert opinions as adopted by the Stockholm Convention COP6 in 2013: · Guidance on the Global Monitoring Plan for Persistent Organic Pollutants UNEP/POPS/COP.6/INF/31 (version January 2013) · Conclusions of the Meeting of the Global Coordination Group and Regional Organization Groups for the Global Monitoring Plan for POPs, held in Geneva, 10–12 October 2012 · Conclusions of the Meeting of the expert group on data handling under the global monitoring plan for persistent organic pollutants, held in Brno, Czech Republic, 13-15 June 2012 The individual reported data component is inserted as: · free text or number (e.g. Site name, Monitoring programme, Value) · a defined item selected from a particular code list (e.g., Country, Chemical – group, Sampling). All code lists (i.e., allowed values for individual parameters) are enclosed in this document, either in a particular section (e.g., Region, Method) or listed separately in the annexes below (Country, Chemical – group, Parameter) for your reference. -
Species Status Assessment Emperor Penguin (Aptenodytes Fosteri)
SPECIES STATUS ASSESSMENT EMPEROR PENGUIN (APTENODYTES FOSTERI) Emperor penguin chicks being socialized by male parents at Auster Rookery, 2008. Photo Credit: Gary Miller, Australian Antarctic Program. Version 1.0 December 2020 U.S. Fish and Wildlife Service, Ecological Services Program Branch of Delisting and Foreign Species Falls Church, Virginia Acknowledgements: EXECUTIVE SUMMARY Penguins are flightless birds that are highly adapted for the marine environment. The emperor penguin (Aptenodytes forsteri) is the tallest and heaviest of all living penguin species. Emperors are near the top of the Southern Ocean’s food chain and primarily consume Antarctic silverfish, Antarctic krill, and squid. They are excellent swimmers and can dive to great depths. The average life span of emperor penguin in the wild is 15 to 20 years. Emperor penguins currently breed at 61 colonies located around Antarctica, with the largest colonies in the Ross Sea and Weddell Sea. The total population size is estimated at approximately 270,000–280,000 breeding pairs or 625,000–650,000 total birds. Emperor penguin depends upon stable fast ice throughout their 8–9 month breeding season to complete the rearing of its single chick. They are the only warm-blooded Antarctic species that breeds during the austral winter and therefore uniquely adapted to its environment. Breeding colonies mainly occur on fast ice, close to the coast or closely offshore, and amongst closely packed grounded icebergs that prevent ice breaking out during the breeding season and provide shelter from the wind. Sea ice extent in the Southern Ocean has undergone considerable inter-annual variability over the last 40 years, although with much greater inter-annual variability in the five sectors than for the Southern Ocean as a whole. -
Late Pleistocene Interactions of East and West Antarctic Ice-Flow Regim.Es: Evidence From
J oumal oJ Glaciology, r·ol. 42, S o. 142, 1996 Late Pleistocene interactions of East and West Antarctic ice-flow regim.es: evidence from. the McMurdo Ice Shelf THO}'IAS B . KELLOGG, TERRY H UG HES AND D .\VJD!\ E. KELLOGG Depa rtmen t oJ Geo logical Sciences alld Institute for QJlatemm) Studies, UI/ iversilj' oJ ,\Jail/ e, Orono , "faine 04469. [j.S. A. ABSTRACT. \Ve prese nt new interpreta ti ons of d eglacia tion in M cMurdo Sound and the wes tern R oss Sea, with o bservati onall y based reconstructi ons of interacti ons between Eas t a nd \Ves t Antarcti c ice a t the las t glacial maximum (LG YI ), 16 000, 12 000, 8000 a nd 4000 BP. At the LG M , East Anta rctic ice fr om Muloek Glacier spli t; one bra nch turned wes tward south of R oss Tsland b ut the other bra nch rounded R oss Island before fl owing south"'est in to lVf cMurdo Sound. This fl ow regime, constrained b y a n ice sa ddle north of R n. s Isla nd, is consisten t wi th the reconstruc ti on of Stuiyer a nd others (198I a ) . After the LG lVI. , grounding-line retreat was m ost ra pid in areas \~ ' i th greates t wa ter d epth, es pecially a long th e Vic toria Land coast. By 12 000 BP , the ice-flow regime in :'.1cMurdo Sound c ha nged to through-flowing l\1ulock G lacier ice, with lesse r contributions from K oettlitz, Blue a nd F crra r Glaciers, because the formcr ice saddle north of R oss Isla nd was repl aced by a d om e. -
Pw-Zoom” – the Uav of Warsaw University of Technology
ARCHIVEOFMECHANICALENGINEERING VOL. LXIV 2017 Number 1 DOI: 10.1515/meceng-2017-0003 Key words: UAV, unmanned aircraft, photogrammetry mission, orthophotomaps MIROSŁAW RODZEWICZ,1 DOMINIK GŁOWACKI,1 JAROSŁAW HAJDUK2 SOME DYNAMIC ASPECTS OF PHOTOGRAMMETRY MISSIONS PERFORMED BY “PW-ZOOM” – THE UAV OF WARSAW UNIVERSITY OF TECHNOLOGY The article presents the analyses of the flights carried out the by the Unmanned Aerial Vehicle (UAV) named PW-ZOOM used to perform a photogrammetric mission and monitoring of fauna in Antarctic areas. The analyses focus on the deviations of the optical axis of the photo-camera which occurred during photogrammetric flights carried out on the same route but during several Antarctic expeditions performed in subsequent years (2014 and 2015). The results were subjected to correlation tests with weather conditions (wind speed and variability). The basis for these analyses are the data from the onboard signal recorder integrated with an autopilot. 1. Introduction MONICA is the acronym for the Polish-Norwegian project funded by the Norway Grants programme entitled „Monitoring the impact of climate change on Antarctic ecosystems”. The project is carried out under the patronage of the Na- tional Centre for Research and Development and involves three partner institutions: the Polish Academy of Sciences, the Warsaw University of Technology, and the Norwegian Northern Research Institute. The objective of the project was to study the impact of climate change on the Antarctic ecosystem and biodiversity by moni- toring penguin populations, which are the bio-indicator of the abundance of marine waters in the Antarctic region [1] (Fig.1), and performing photogrammetric work on the selected areas called the ASPA (Antarctic Special Protected Areas ASPA 128 and ASPA 151) on King George Island, the largest of the South Shetland Islands (Fig.2). -
Zeszyt 10. Morza I Oceany
Uwaga: Niniejsza publikacja została opracowana według stanu na 2008 rok i nie jest aktualizowana. Zamieszczony na stronie internetowej Komisji Standaryzacji Nazw Geograficznych poza Granica- mi Rzeczypospolitej Polskiej plik PDF jest jedynie zapisem cyfrowym wydrukowanej publikacji. Wykaz zalecanych przez Komisję polskich nazw geograficznych świata (Urzędowy wykaz polskich nazw geograficznych świata), wraz z aktualizowaną na bieżąco listą zmian w tym wykazie, zamieszczo- ny jest na stronie internetowej pod adresem: http://ksng.gugik.gov.pl/wpngs.php. KOMISJA STANDARYZACJI NAZW GEOGRAFICZNYCH POZA GRANICAMI RZECZYPOSPOLITEJ POLSKIEJ przy Głównym Geodecie Kraju NAZEWNICTWO GEOGRAFICZNE ŚWIATA Zeszyt 10 Morza i oceany GŁÓWNY URZĄD GEODEZJI I KARTOGRAFII Warszawa 2008 KOMISJA STANDARYZACJI NAZW GEOGRAFICZNYCH POZA GRANICAMI RZECZYPOSPOLITEJ POLSKIEJ przy Głównym Geodecie Kraju Waldemar Rudnicki (przewodniczący), Andrzej Markowski (zastępca przewodniczącego), Maciej Zych (zastępca przewodniczącego), Katarzyna Przyszewska (sekretarz); członkowie: Stanisław Alexandrowicz, Andrzej Czerny, Janusz Danecki, Janusz Gołaski, Romuald Huszcza, Sabina Kacieszczenko, Dariusz Kalisiewicz, Artur Karp, Zbigniew Obidowski, Jerzy Ostrowski, Jarosław Pietrow, Jerzy Pietruszka, Andrzej Pisowicz, Ewa Wolnicz-Pawłowska, Bogusław R. Zagórski Opracowanie Kazimierz Furmańczyk Recenzent Maciej Zych Komitet Redakcyjny Andrzej Czerny, Joanna Januszek, Sabina Kacieszczenko, Dariusz Kalisiewicz, Jerzy Ostrowski, Waldemar Rudnicki, Maciej Zych Redaktor prowadzący Maciej -
Advisory Committee on Reactor Safeguards (ACRS)
Federal Register / Vol. 77, No. 95 / Wednesday, May 16, 2012 / Notices 28903 FOR FURTHER INFORMATION CONTACT: Dates Detailed meeting agendas and meeting Polly A. Penhale at the above address or October 1, 2012 to December 30, 2012. transcripts are available on the NRC (703) 292–7420. Web site at http://www.nrc.gov/reading- Nadene G. Kennedy, rm/doc-collections/acrs. Information SUPPLEMENTARY INFORMATION: The Permit Officer, Office of Polar Programs. regarding topics to be discussed, National Science Foundation, as [FR Doc. 2012–11840 Filed 5–15–12; 8:45 am] changes to the agenda, whether the directed by the Antarctic Conservation BILLING CODE 7555–01–P meeting has been canceled or Act of 1978 (Pub. L. 95–541), as rescheduled, and the time allotted to amended by the Antarctic Science, present oral statements can be obtained Tourism and Conservation Act of 1996, from the Web site cited above or by has developed regulations for the NUCLEAR REGULATORY contacting the identified DFO. establishment of a permit system for COMMISSION Moreover, in view of the possibility that various activities in Antarctica and the schedule for ACRS meetings may be designation of certain animals and Advisory Committee on Reactor adjusted by the Chairman as necessary certain geographic areas requiring Safeguards (ACRS) Meeting of the to facilitate the conduct of the meeting, special protection. The regulations ACRS Subcommittee on Fukushima; persons planning to attend should check establish such a permit system to Notice of Meeting with these references if such designate Antarctic Specially Protected The ACRS Subcommittee on rescheduling would result in a major Areas. -
List of Place-Names in Antarctica Introduced by Poland in 1978-1990
POLISH POLAR RESEARCH 13 3-4 273-302 1992 List of place-names in Antarctica introduced by Poland in 1978-1990 The place-names listed here in alphabetical order, have been introduced to the areas of King George Island and parts of Nelson Island (West Antarctica), and the surroundings of A. B. Dobrowolski Station at Bunger Hills (East Antarctica) as the result of Polish activities in these regions during the period of 1977-1990. The place-names connected with the activities of the Polish H. Arctowski Station have been* published by Birkenmajer (1980, 1984) and Tokarski (1981). Some of them were used on the Polish maps: 1:50,000 Admiralty Bay and 1:5,000 Lions Rump. The sheet reference is to the maps 1:200,000 scale, British Antarctic Territory, South Shetland Islands, published in 1968: King George Island (sheet W 62 58) and Bridgeman Island (Sheet W 62 56). The place-names connected with the activities of the Polish A. B. Dobrowolski Station have been published by Battke (1985) and used on the map 1:5,000 Antarctic Territory — Bunger Oasis. Agat Point. 6211'30" S, 58'26" W (King George Island) Small basaltic promontory with numerous agates (hence the name), immediately north of Staszek Cove. Admiralty Bay. Sheet W 62 58. Polish name: Przylądek Agat (Birkenmajer, 1980) Ambona. 62"09'30" S, 58°29' W (King George Island) Small rock ledge, 85 m a. s. 1. {ambona, Pol. = pulpit), above Arctowski Station, Admiralty Bay, Sheet W 62 58 (Birkenmajer, 1980). Andrzej Ridge. 62"02' S, 58° 13' W (King George Island) Ridge in Rose Peak massif, Arctowski Mountains.