Wastewater Treatment in Antarctica
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For Land-Fast Sea Ice at Prydz Bay, East Antarctica: an Operational Service for CHINARE
Annals of Glaciology Fast Ice Prediction System (FIPS) for land-fast sea ice at Prydz Bay, East Antarctica: an operational service for CHINARE Jiechen Zhao1,2, Bin Cheng3 , Timo Vihma3, Petra Heil4, Fengming Hui5,6, Article Qi Shu7,2 , Lin Zhang1 and Qinghua Yang8,6 Cite this article: Zhao J, Cheng B, Vihma T, Heil P, Hui F, Shu Q, Zhang L, Yang Q (2020). 1Key Laboratory of Marine Hazards Forecasting, National Marine Environmental Forecasting Centre (NMEFC), Fast Ice Prediction System (FIPS) for land-fast Ministry of Natural Resources, Beijing 100081, China; 2Laboratory for Regional Oceanography and Numerical sea ice at Prydz Bay, East Antarctica: an Modelling, Qingdao National Laboratory for Marine Science and Technology, Qingdao 266237, China; 3Finnish operational service for CHINARE. Annals of Meteorological Institute (FMI), Helsinki 00101, Finland; 4Australia Antarctic Division & Australian Antarctic Glaciology 61(83), 271–283. https://doi.org/ Programmer Partnership, Private Bag 80, Hobart, TAS 7001, Australia; 5School of Geospatial Engineering and 10.1017/aog.2020.46 Science, Sun Yat-sen University, Zhuhai 519082, China; 6Southern Marine Science and Engineering Guangdong 7 Received: 26 November 2019 Laboratory (Zhuhai), Zhuhai 519082, China; First Institute of Oceanography, Ministry of Natural Resources, 8 Revised: 1 June 2020 Qingdao 266061, China and School of Atmospheric Sciences, and Guangdong Province Key Laboratory for Accepted: 2 June 2020 Climate Change and Natural Disaster Studies, Sun Yat-sen University, Zhuhai 519082, China First published online: 9 July 2020 Key words: Abstract Antarctica; land-fast sea ice; operational A Fast Ice Prediction System (FIPS) was constructed and is the first regional land-fast sea-ice service; Prydz Bay; snow and ice thickness; forecasting system for the Antarctic. -
Arctic and Antarctic Research Institute” Russian Antarctic Expedition
FEDERAL SERVICE OF RUSSIA FOR HYDROMETEOROLOGY AND ENVIRONMENTAL MONITORING State Institution “Arctic and Antarctic Research Institute” Russian Antarctic Expedition QUARTERLY BULLETIN ʋ2 (51) April - June 2010 STATE OF ANTARCTIC ENVIRONMENT Operational data of Russian Antarctic stations St. Petersburg 2010 FEDERAL SERVICE OF RUSSIA FOR HYDROMETEOROLOGY AND ENVIRONMENTAL MONITORING State Institution “Arctic and Antarctic Research Institute” Russian Antarctic Expedition QUARTERLY BULLETIN ʋ2 (51) April - June 2010 STATE OF ANTARCTIC ENVIRONMENT Operational data of Russian Antarctic stations Edited by V.V. Lukin St. Petersburg 2010 Editor-in-Chief - M.O. Krichak (Russian Antarctic Expedition –RAE) Authors and contributors Section 1 M. O. Krichak (RAE), Section 2 Ye. I. Aleksandrov (Department of Meteorology) Section 3 G. Ye. Ryabkov (Department of Long-Range Weather Forecasting) Section 4 A. I. Korotkov (Department of Ice Regime and Forecasting) Section 5 Ye. Ye. Sibir (Department of Meteorology) Section 6 I. V. Moskvin, Yu.G.Turbin (Department of Geophysics) Section 7 V. V. Lukin (RAE) Section 8 B. R. Mavlyudov (RAS IG) Section 9 V. L. Martyanov (RAE) Translated by I.I. Solovieva http://www.aari.aq/, Antarctic Research and Russian Antarctic Expedition, Reports and Glossaries, Quarterly Bulletin. Acknowledgements: Russian Antarctic Expedition is grateful to all AARI staff for participation and help in preparing this Bulletin. For more information about the contents of this publication, please, contact Arctic and Antarctic Research Institute of Roshydromet Russian Antarctic Expedition Bering St., 38, St. Petersburg 199397 Russia Phone: (812) 352 15 41; 337 31 04 Fax: (812) 337 31 86 E-mail: [email protected] CONTENTS PREFACE……………………….…………………………………….………………………….1 1. DATA OF AEROMETEOROLOGICAL OBSERVATIONS AT THE RUSSIAN ANTARCTIC STATIONS…………………………………….…………………………3 2. -
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 -
Station Sharing in Antarctica
IP 94 Agenda Item: ATCM 7, ATCM 10, ATCM 11, ATCM 14, CEP 5, CEP 6b, CEP 9 Presented by: ASOC Original: English Station Sharing in Antarctica 1 IP 94 Station Sharing in Antarctica Information Paper Submitted by ASOC to the XXIX ATCM (CEP Agenda Items 5, 6 and 9, ATCM Agenda Items 7, 10, 11 and 14) I. Introduction and overview As of 2005 there were at least 45 permanent stations in the Antarctic being operated by 18 countries, of which 37 were used as year-round stations.i Although there are a few examples of states sharing scientific facilities (see Appendix 1), for the most part the practice of individual states building and operating their own facilities, under their own flags, persists. This seems to be rooted in the idea that in order to become a full Antarctic Treaty Consultative Party (ATCP), one has to build a station to show seriousness of scientific purpose, although formally the ATCPs have clarified that this is not the case. The scientific mission and international scientific cooperation is nominally at the heart of the ATS,ii and through SCAR the region has a long-established scientific coordination body. It therefore seems surprising that half a century after the adoption of this remarkable Antarctic regime, we still see no truly international stations. The ‘national sovereign approach’ continues to be the principal driver of new stations. Because new stations are likely to involve relatively large impacts in areas that most likely to be near pristine, ASOC submits that this approach should be changed. In considering environmental impact analyses of proposed new station construction, the Committee on Environmental Protection (CEP) presently does not have a mandate to take into account opportunities for sharing facilities (as an alternative that would reduce impacts). -
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. -
Application of a New Polarimetric Filter to Radarsat-2 Data of Deception Island (Antarctic Peninsula Region) for Surface Cover Characterization
APPLICATION OF A NEW POLARIMETRIC FILTER TO RADARSAT-2 DATA OF DECEPTION ISLAND (ANTARCTIC PENINSULA REGION) FOR SURFACE COVER CHARACTERIZATION a b c a S. Guillaso ,∗ T. Schmid , J. Lopez-Mart´ ´ınez , O. D’Hondt a Technische Universitat¨ Berlin, Computer Vision and Remote Sensing, Berlin, Germany - [email protected] b CIEMAT, Madrid, Spain - [email protected] c Universidad Autonoma´ de Madrid, Spain - [email protected] KEY WORDS: SAR, Antarctica, Surface characterization, Geomorphology, Soils, Polarimetry, Speckle Filtering, Image interpretation ABSTRACT: In this paper, we describe a new approach to analyse and quantify land surface covers on Deception Island, a volcanic island located in the Northern Antarctic Peninsula region by means of fully polarimetric RADARSAT-2 (C-Band) SAR image. Data have been filtered by a new polarimetric speckle filter (PolSAR-BLF) that is based on the bilateral filter. This filter is locally adapted to the spatial structure of the image by relying on pixel similarities in both the spatial and the radiometric domains. Thereafter different polarimetric features have been extracted and selected before being geocoded. These polarimetric parameters serve as a basis for a supervised classification using the Support Vector Machine (SVM) classifier. Finally, a map of landform is generated based on the result of the SVM results. 1. INTRODUCTION Ice-free land surfaces of the Northern Antarctica Peninsula region are under the influence of freeze-thaw cycling effects on differ- ent parent materials. This is mainly due to the particular climatic conditions of the so called Maritime Antarctica and because this region is one the the fastest warming areas of the southern hemi- sphere. -
Southern Hemisphere Mid- and High-Latitudinal AOD, CO, NO2, And
Ahn et al. Progress in Earth and Planetary Science (2019) 6:34 Progress in Earth and https://doi.org/10.1186/s40645-019-0277-y Planetary Science RESEARCH ARTICLE Open Access Southern Hemisphere mid- and high- latitudinal AOD, CO, NO2, and HCHO: spatiotemporal patterns revealed by satellite observations Dha Hyun Ahn1, Taejin Choi2, Jhoon Kim1, Sang Seo Park3, Yun Gon Lee4, Seong-Joong Kim2 and Ja-Ho Koo1* Abstract To assess air pollution emitted in Southern Hemisphere mid-latitudes and transported to Antarctica, we investigate the climatological mean and temporal trends in aerosol optical depth (AOD), carbon monoxide (CO), nitrogen dioxide (NO2), and formaldehyde (HCHO) columns using satellite observations. Generally, all these measurements exhibit sharp peaks over and near the three nearby inhabited continents: South America, Africa, and Australia. This pattern indicates the large emission effect of anthropogenic activities and biomass burning processes. High AOD is also found over the Southern Atlantic Ocean, probably because of the sea salt production driven by strong winds. Since the pristine Antarctic atmosphere can be polluted by transport of air pollutants from the mid-latitudes, we analyze the 10-day back trajectories that arrive at Antarctic ground stations in consideration of the spatial distribution of mid-latitudinal AOD, CO, NO2, and HCHO. We find that the influence of mid-latitudinal emission differs across Antarctic regions: western Antarctic regions show relatively more back trajectories from the mid-latitudes, while the eastern Antarctic regions do not show large intrusions of mid-latitudinal air masses. Finally, we estimate the long-term trends in AOD, CO, NO2, and HCHO during the past decade (2005–2016). -
MEMBER COUNTRY: Russia National Report to SCAR for Year: 2008-09 Activity Contact Name Address Telephone Fax Email Web Site
MEMBER COUNTRY: Russia National Report to SCAR for year: 2008-09 Activity Contact Name Address Telephone Fax Email web site National SCAR Committee SCAR Delegates Russian National Committee on Antarctic Research Institute of Geography, Staromonetny per.29, 1) Delegate V.M.Kotlyakov 109017 Moskow, Russia 74,959,590,032 74,959,590,033 [email protected] Russian National Committee on Antarctic Research Institute of Geography, Staromonetny per.29, 2) Alternate Delegate M.Yu.Moskalev-sky 109017 Moskow, Russia 74,959,590,032 74,959,590,033 [email protected] Standing Scientific Groups Life Sciences Institute of Oceanology, Russian Academy of Sciences, Nakhimovsky prosp.36, Delegate Melnikov Igor 117852 Moscow, Russia 74951292018 74951245983 [email protected] www.paiceh.ru Geosciences VNIIOkeangeologia, Angliysky Ave, 1, Leitchenkov 190121 St.Petersburg, Delegate German Russia 78123123551 78127141470 [email protected] Physical Sciences Arctic and Antarctic Research Institute Ul.Beringa, 38, Klepikov 199226 St.Petersburg, 78123522827 Delegate Aleksander Russia 78123520226 78123522688 [email protected] www.aari.aq 1 Activity Contact Name Address Telephone Fax Email web site Scientific Research Program ACE None AGCS Delegate Arctic and Antarctic Research Institute Ul.Beringa, 38, Klepikov 199226 St.Petersburg, 1) Aleksander Russia 78123520226 78123522688 [email protected] www.aari.ru Arctic and Antarctic Research Institute Ul.Beringa, 38, 199226 St.Petersburg, 2) LagunVictor Russia 78123522950 78123522688 [email protected] www.aari.aq EBA None ICESTAR -
CCN Measurements at the Princess Elisabeth Antarctica Research
bs CCN measurements at the Princess Elisabeth Antarctica Research Station during three austral summers Paul Herenz1, Heike Wex1, Alexander Mangold2, Quentin Laffineur2, Irina V. Gorodetskaya3,4, Zoë L. Fleming5, Marios Panagi5, and Frank Stratmann1 1Leibniz Institute for Tropospheric Research, Leipzig, Germany 2Royal Meteorological Institute of Belgium, Brussels, Belgium 3Centre for Environmental and Marine Studies, Department of Physics, University of Aveiro, Aveiro, Portugal 4Department of Earth and Environmental Sciences, KU Leuven, Belgium 5National Centre for Atmospheric Science, Department of Chemistry, University of Leicester, Leicester, UK Correspondence to: Heike Wex ([email protected]) Abstract. For three austral summer seasons (2013-2016, each from December to February) aerosol particles arriving at the Belgian Antarctic research station Princess Elisabeth (PE), in Dronning Maud Land in East Antarctica were characterized. in terms 5 ofThis included number concentrations of total aerosol particles (NCN) and cloud condensation nuclei (NCCN), the particle number size distribution (PNSD), the aerosol particle hygroscopicity and the influence of the air mass origin on NCN and −3 −3 NCCN. In general NCN was found to range from 40 to 6700 cm with a median of 333 cm , while NCCN was found to cover a range between less than 10 and 1300 cm−3 for supersaturations (SS) between 0.1 and 0.7 %. It is shown that the aerosol is Aitken mode dominated and is , being characterized by a significant amount of freshly, small, and therefore likely secondarily -
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Science in the Snow Appendix 1 SCAR Members Full members (31) (Associate Membership) Full Membership Argentina 3 February 1958 Australia 3 February 1958 Belgium 3 February 1958 Chile 3 February 1958 France 3 February 1958 Japan 3 February 1958 New Zealand 3 February 1958 Norway 3 February 1958 Russia (assumed representation of USSR) 3 February 1958 South Africa 3 February 1958 United Kingdom 3 February 1958 United States of America 3 February 1958 Germany (formerly DDR and BRD individually) 22 May 1978 Poland 22 May 1978 India 1 October 1984 Brazil 1 October 1984 China 23 June 1986 Sweden (24 March 1987) 12 September 1988 Italy (19 May 1987) 12 September 1988 Uruguay (29 July 1987) 12 September 1988 Spain (15 January 1987) 23 July 1990 The Netherlands (20 May 1987) 23 July 1990 Korea, Republic of (18 December 1987) 23 July 1990 Finland (1 July 1988) 23 July 1990 Ecuador (12 September 1988) 15 June 1992 Canada (5 September 1994) 27 July 1998 Peru (14 April 1987) 22 July 2002 Switzerland (16 June 1987) 4 October 2004 Bulgaria (5 March 1995) 17 July 2006 Ukraine (5 September 1994) 17 July 2006 Malaysia (4 October 2004) 14 July 2008 Associate Members (12) Pakistan 15 June 1992 Denmark 17 July 2006 Portugal 17 July 2006 Romania 14 July 2008 261 Appendices Monaco 9 August 2010 Venezuela 23 July 2012 Czech Republic 1 September 2014 Iran 1 September 2014 Austria 29 August 2016 Colombia (rejoined) 29 August 2016 Thailand 29 August 2016 Turkey 29 August 2016 Former Associate Members (2) Colombia 23 July 1990 withdrew 3 July 1995 Estonia 15 June -
IP31 XII Special Consultative Meeting October, 2000 Traité De L'antarctique Original: English E XII Réunion Consultative Spéciale
Antarctic Treaty XII SATCM/IP31 XII Special Consultative Meeting October, 2000 Traité de l'Antarctique Original: English XIIe Réunion consultative spéciale Tratado Antártico Agenda Item XII Reunión Consultiva Especial (CEP) 4e Антарктический Договор XII Специальное Консультативное Совещание Environmental protection activities at the Russian Antarctic station Progress in 1999-2000 Submitted by Russian Federation Environmental protection activities at the Russian Antarctic station Progress in 1999-2000 (Special ATCM, 11-16 September, 2000,CEP III, IP, Item 4a, submitted by the Russian Federation) The Antarctic field base Druzhnaya-4 and the Progress station were set up on the Amery Ice Shelf and in the Larsemann Hills oasis as the basic points for organizing Russian geological-geophysical studies of the area of Prince Charles Mountains and the Lambert glacier in 1987 and 1988, respectively. During the 1988-1989 season, the Progress station was moved to a new location closer to the ship unloading area. During the 1990-1992 period, large construction activities were undertaken at the Progress station presenting the first stage of establishing a large Antarctic base with the design dimensions similar to the USA McMurdo station. With this aim, a package of the necessary design-construction documentation was developed meeting the standard-legal base existing at that time in the USSR including the environmental protection issues. It also included the documentation on construction of the snow-ice runway to receive heavy wheeled aircraft. The political and economical changes that occurred in the country in the late 1980s-early 1990s interrupted these activities resulting in the temporary closing down of the station in 1992. -
Advances in Seismic Monitoring at Deception Island Volcano
ANNALS OF GEOPHYSICS, 57, 3, 2014, SS0321; doi:10.4401/ag-6378 Special section: Geophysical monitorings at the Earth’s polar regions Advances in seismic monitoring at Deception Island volcano (Antarctica) since the International Polar Year Enrique Carmona1, Javier Almendros1,2,*, Rosa Martín1, Guillermo Cortés1, Gerardo Alguacil1,2, Javier Moreno1, José Benito Martín1, Antonio Martos1, Inmaculada Serrano1,2, Daniel Stich1,2, Jesús M. Ibáñez1,2 1 Instituto Andaluz de Geofísica, Universidad de Granada, Granada, Spain 2 Departamento de Física Teórica y del Cosmos, Universidad de Granada, Granada, Spain Article history Received June 30, 2013; accepted October 25, 2013. Subject classification: Volcano monitoring, Seismic network, Seismic array, Deception Island volcano, International Polar Year. ABSTRACT of the most visited places in Antarctica both by sci- Deception Island is an active volcano located in the south Shetland Is- entists and tourists, which emphasizes the impor- lands, Antarctica. It constitutes a natural laboratory to test geophysical tance of volcano surveillance and monitoring. instruments in extreme conditions, since they have to endure not only the Antarctic climate but also the volcanic environment. Deception is one of the most visited places in Antarctica, both by scientists and tourists, which emphasize the importance of volcano monitoring. Seismic monitoring has been going on since 1986 during austral summer surveys. The recorded data include volcano-tectonic earthquakes, long-period events and volcanic tremor, among