2000 Svalbard Workshop Report (PDF 2.5
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Arctic Expedition12° 16° 20° 24° 28° 32° Spitsbergen U Svalbard Archipelago 80° 80°
distinguished travel for more than 35 years Voyage UNDER THE Midnight Sun Arctic Expedition12° 16° 20° 24° 28° 32° Spitsbergen u Svalbard Archipelago 80° 80° 80° Raudfjorden Nordaustlandet Woodfjorden Smeerenburg Monaco Glacier The Arctic’s 79° 79° 79° Kongsfjorden Svalbard King’s Glacier Archipelago Ny-Ålesund Spitsbergen Longyearbyen Canada 78° 78° 78° i Greenland tic C rcle rc Sea Camp Millar A U.S. North Pole Russia Bellsund Calypsobyen Svalbard Archipelago Norway Copenhagen Burgerbukta 77° 77° 77° Cruise Itinerary Denmark Air Routing Samarin Glacier Hornsund Barents Sea June 20 to 30, 2022 4° 8° Spitsbergen12° u Samarin16° Glacier20° u Calypsobyen24° 76° 28° 32° 36° 76° Voyage across the Arctic Circle on this unique 11-day Monaco Glacier u Smeerenburg u Ny-Ålesund itinerary featuring a seven-night cruise round trip Copenhagen 1 Depart the U.S. or Canada aboard the Five-Star Le Boréal. Visit during the most 2 Arrive in Copenhagen, Denmark enchanting season, when the region is bathed in the magical 3 Copenhagen/Fly to Longyearbyen, Spitsbergen, light of the Midnight Sun. Cruise the shores of secluded Norway’s Svalbard Archipelago/Embark Le Boréal 4 Hornsund for Burgerbukta/Samarin Glacier Spitsbergen—the jewel of Norway’s rarely visited Svalbard 5 Bellsund for Calypsobyen/Camp Millar archipelago enjoy expert-led Zodiac excursions through 6 Cruising the Arctic Ice Pack sandstone mountain ranges, verdant tundra and awe-inspiring 7 MåkeØyane/Woodfjorden/Monaco Glacier ice formations. See glaciers calve in luminous blues and search 8 Raudfjorden for Smeerenburg for Arctic wildlife, including the “King of the Arctic,” the 9 Ny-Ålesund/Kongsfjorden for King’s Glacier polar bear, whales, walruses and Svalbard reindeer. -
Air Ambulance Services in the Arctic 1999-2009: a Norwegian Study Jan Norum1,2,3*, Trond M Elsbak3
Norum and Elsbak International Journal of Emergency Medicine 2011, 4:1 http://www.intjem.com/content/4/1/1 ORIGINALRESEARCH Open Access Air ambulance services in the Arctic 1999-2009: a Norwegian study Jan Norum1,2,3*, Trond M Elsbak3 Abstract Background: Air ambulance services in the Arctic have to deal with remote locations, long distances, rough weather conditions and seasonable darkness. Despite these challenges, the people living in the area expect a high quality of specialist health care. Aims: The objective of this study was to analyse the air ambulance operations performed in the Norwegian Arctic and study variations in diagnoses and flight patterns around the year. Methods: A retrospective analysis. All air ambulance operations performed during the time 1999 – 2009 period were analysed. The subjects were patients transported and flights performed. The primary outcome measures were patients’ diagnoses and task patterns around the year. Results: A total of 345 patients were transported and 321 flights performed. Coronary heart and vascular disease, bone fractures and infections were the most common diagnoses. Most patients (85%) had NACA score 3 or 4. Half of all fractures occurred in April and August. Most patients were males (66%), and one fourth was not Norwegian. The median flying time (one way) was 3 h 33 m. Ten percent of the flights were delayed, and only 14% were performed between midnight and 8.00 AM. The period April to August was the busiest one (58% of operations). Conclusions: Norway has run a safe air ambulance service in the Arctic for the last 11 years. In the future more shipping and polar adventure operations may influence the need for air ambulances, especially during summer and autumn. -
Market Risk Index 120 Amundsen Sea 90 60 30 0 30 60 90 120
COUNTRY RISK MAP 2010 150 120 90 60 30 0 30 60 90 120 150 180 ARCTIC OCEAN FRANZ JOSEF ARCTIC OCEAN LAND SEVERNAYA ARCTIC OCEAN ZEMLYA Ellesmere Island QUEEN ELIZABETH Longyearbyen NEW SIBERIAN ISLANDS Svalbard NOVAYA Kara Sea ISLANDS Greenland Sea ZEMLYA Laptev Sea Banks (NORWAY) Barents Sea Island Greenland East Siberian Sea Beaufort Sea Ban Wrangel (DENMARK) Island Victoria Bay Island Ban Jan Mayen Norwegian Chukchi (NORWAY) Island Sea Sea Arctic Circle (66°33') Arctic Circle (66°33') NORWAY Great Nuuk ICELAND White Sea U. S. Bear Lake (Godthåb) SWEDEN Provideniya Davis Denmark Strait Reykjavík Faroe Islands FINLAND Lake Strait (DEN.) Gulf R U S S I A Tórshavn of Ladoga Lake Great Bothnia Onega Slave Lake Hudson Oslo Helsinki 60 60 Bay Stockholm Tallinn Gulf of Alaska Rockall EST. Labrador (U.K.) Baltic Bering Sea Riga S North Sea LAT. Sea DENMARK Moscow Sea Copenhagen LITH. Lake RUSSIA Sea of C A N A D A UNITED Vilnius Baikal S Minsk N D Dublin Isle of KINGDOM S Okhotsk LA Man IS (U.K.) BELARUS T IA N Lake IRELAND Amsterdam Berlin Warsaw U.S. LE U Winnipeg Kamchatskiy A NETH. Astana Sakhalin A Island of L D S London Brussels POLAND E U T A N GERMANY Prague Kyiv I A N I S L Newfoundland Celtic BELGIUM LUX. Sea Guernsey (U.K.) Luxembourg CZECH REP. U K R A I N E Jersey (U.K.) SLOVAKIA Gulf of Paris Vienna Bratislava S K A Z A K H S T A N Ulaanbaatar KURIL Lake St. -
Petroleum, Coal and Research Drilling Onshore Svalbard: a Historical Perspective
NORWEGIAN JOURNAL OF GEOLOGY Vol 99 Nr. 3 https://dx.doi.org/10.17850/njg99-3-1 Petroleum, coal and research drilling onshore Svalbard: a historical perspective Kim Senger1,2, Peter Brugmans3, Sten-Andreas Grundvåg2,4, Malte Jochmann1,5, Arvid Nøttvedt6, Snorre Olaussen1, Asbjørn Skotte7 & Aleksandra Smyrak-Sikora1,8 1Department of Arctic Geology, University Centre in Svalbard, P.O. Box 156, 9171 Longyearbyen, Norway. 2Research Centre for Arctic Petroleum Exploration (ARCEx), University of Tromsø – the Arctic University of Norway, P.O. Box 6050 Langnes, 9037 Tromsø, Norway. 3The Norwegian Directorate of Mining with the Commissioner of Mines at Svalbard, P.O. Box 520, 9171 Longyearbyen, Norway. 4Department of Geosciences, University of Tromsø – the Arctic University of Norway, P.O. Box 6050 Langnes, 9037 Tromsø, Norway. 5Store Norske Spitsbergen Kulkompani AS, P.O. Box 613, 9171 Longyearbyen, Norway. 6NORCE Norwegian Research Centre AS, Fantoftvegen 38, 5072 Bergen, Norway. 7Skotte & Co. AS, Hatlevegen 1, 6240 Ørskog, Norway. 8Department of Earth Science, University of Bergen, P.O. Box 7803, 5020 Bergen, Norway. E-mail corresponding author (Kim Senger): [email protected] The beginning of the Norwegian oil industry is often attributed to the first exploration drilling in the North Sea in 1966, the first discovery in 1967 and the discovery of the supergiant Ekofisk field in 1969. However, petroleum exploration already started onshore Svalbard in 1960 with three mapping groups from Caltex and exploration efforts by the Dutch company Bataaffse (Shell) and the Norwegian private company Norsk Polar Navigasjon AS (NPN). NPN was the first company to spud a well at Kvadehuken near Ny-Ålesund in 1961. -
Thermohaline Circulation (From Britannica)
Thermohaline circulation (from Britannica) The general circulation of the oceans consists primarily of the wind-driven currents. These, however, are superimposed on the much more sluggish circulation driven by horizontal differences in temperature and salinity—namely, the thermohaline circulation. The thermohaline circulation reaches down to the seafloor and is often referred to as the deep, or abyssal, ocean circulation. Measuring seawater temperature and salinity distribution is the chief method of studying the deep-flow patterns. Other properties also are examined; for example, the concentrations of oxygen, carbon-14, and such synthetically produced compounds as chlorofluorocarbons are measured to obtain resident times and spreading rates of deep water. In some areas of the ocean, generally during the winter season, cooling or net evaporation causes surface water to become dense enough to sink. Convection penetrates to a level where the density of the sinking water matches that of the surrounding water. It then spreads slowly into the rest of the ocean. Other water must replace the surface water that sinks. This sets up the thermohaline circulation. The basic thermohaline circulation is one of sinking of cold water in the polar regions, chiefly in the northern North Atlantic and near Antarctica. These dense water masses spread into the full extent of the ocean and gradually upwell to feed a slow return flow to the sinking regions. A theory for the thermohaline circulation pattern was proposed by Stommel and Arnold Arons in 1960. In the Northern Hemisphere, the primary region of deep water formation is the North Atlantic; minor amounts of deep water are formed in the Red Sea and Persian Gulf. -
Climate in Svalbard 2100
M-1242 | 2018 Climate in Svalbard 2100 – a knowledge base for climate adaptation NCCS report no. 1/2019 Photo: Ketil Isaksen, MET Norway Editors I.Hanssen-Bauer, E.J.Førland, H.Hisdal, S.Mayer, A.B.Sandø, A.Sorteberg CLIMATE IN SVALBARD 2100 CLIMATE IN SVALBARD 2100 Commissioned by Title: Date Climate in Svalbard 2100 January 2019 – a knowledge base for climate adaptation ISSN nr. Rapport nr. 2387-3027 1/2019 Authors Classification Editors: I.Hanssen-Bauer1,12, E.J.Førland1,12, H.Hisdal2,12, Free S.Mayer3,12,13, A.B.Sandø5,13, A.Sorteberg4,13 Clients Authors: M.Adakudlu3,13, J.Andresen2, J.Bakke4,13, S.Beldring2,12, R.Benestad1, W. Bilt4,13, J.Bogen2, C.Borstad6, Norwegian Environment Agency (Miljødirektoratet) K.Breili9, Ø.Breivik1,4, K.Y.Børsheim5,13, H.H.Christiansen6, A.Dobler1, R.Engeset2, R.Frauenfelder7, S.Gerland10, H.M.Gjelten1, J.Gundersen2, K.Isaksen1,12, C.Jaedicke7, H.Kierulf9, J.Kohler10, H.Li2,12, J.Lutz1,12, K.Melvold2,12, Client’s reference 1,12 4,6 2,12 5,8,13 A.Mezghani , F.Nilsen , I.B.Nilsen , J.E.Ø.Nilsen , http://www.miljodirektoratet.no/M1242 O. Pavlova10, O.Ravndal9, B.Risebrobakken3,13, T.Saloranta2, S.Sandven6,8,13, T.V.Schuler6,11, M.J.R.Simpson9, M.Skogen5,13, L.H.Smedsrud4,6,13, M.Sund2, D. Vikhamar-Schuler1,2,12, S.Westermann11, W.K.Wong2,12 Affiliations: See Acknowledgements! Abstract The Norwegian Centre for Climate Services (NCCS) is collaboration between the Norwegian Meteorological In- This report was commissioned by the Norwegian Environment Agency in order to provide basic information for use stitute, the Norwegian Water Resources and Energy Directorate, Norwegian Research Centre and the Bjerknes in climate change adaptation in Svalbard. -
Icepeople Stormy Sendoff
FREE Weather summary Cloudy and partly cloudy with occasional snow and temperatures near -10C through next week. icepeople Full forecast page 3 The world's northernmost alternative newspaper Vol. 9, Issue 1 January 3, 2017 www.icepeople.net 'Longyearbyen at its best:' Modern SVALBARD'S 10 STRANGEST STORIES OF 2016 tragedies, triumphs part of traditional tributes during Syttende Mai celebration Page 7 “ To believe that the governor can rescue people out, regardless of circumstances, is wrong. There is no guarantee for that. - Per Andreassen, police lieutenant Svalbard governor's office ” Late update: 12 apartments vacated again due to building, infrastructure damage. icepeople.net GREENPEACE BRITISH ANTARCTIC SURVEY MARK SABBATINI / ICEPEOPLE A pianist on a glacier, a research vessel suffering from an identity crisis and a gigantic mailbox belonging to the outlaw Santa kept things weird in 2016. WIGGINGWIGGING OUTOUT See DOCK, page 12 Boaty McBoatface, Aquaman, Pokémon among stars in Svalbard's version of the year of surreality By MARK SABBATINI will of the people. A political ad where an in- yet again. Nuclear armageddon, yet again. Editor nocent little girl was obliterated by a weapon When it came to the ways we were weird, A travesty of an election that ignored the of mass destruction. Battling alien invaders, See SURREAL, page 6 Related coverage: • Letters to the Future: grope and change...7 Stormy sendoff • Fleeing Svalbard is easy – sort of……....11 Blizzard buries cars and homes, exposes kindness and resolve By MARK SABBATINI fatal avalanche a year ago. But it didn't cause Editor any tragedies and, while many experienced has- ROLF STANGE MAKSYM BOREIKO Of course, 2016 had to screw us over one sles and minor damage, it was also indiciative A tourist is dwarfed by a drift near Spitsbergen last time with a storm resembling that from the See STORM, page 4 Hotel after a major snowstorm last week. -
Terrestrial Inputs Govern Spatial Distribution of Polychlorinated Biphenyls (Pcbs) and Hexachlorobenzene (HCB) in an Arctic Fjord System (Isfjorden, Svalbard)*
Environmental Pollution 281 (2021) 116963 Contents lists available at ScienceDirect Environmental Pollution journal homepage: www.elsevier.com/locate/envpol Terrestrial inputs govern spatial distribution of polychlorinated biphenyls (PCBs) and hexachlorobenzene (HCB) in an Arctic fjord system (Isfjorden, Svalbard)* * Sverre Johansen a, b, c, Amanda Poste a, Ian Allan c, Anita Evenset d, e, Pernilla Carlsson a, a Norwegian Institute for Water Research, Tromsø, Norway b Norwegian University of Life Sciences, Ås, Norway c Norwegian Institute for Water Research, Oslo, Norway d Akvaplan-niva, Tromsø, Norway e UiT, The Arctic University of Norway, Tromsø, Norway article info abstract Article history: Considerable amounts of previously deposited persistent organic pollutants (POPs) are stored in the Received 20 July 2020 Arctic cryosphere. Transport of freshwater and terrestrial material to the Arctic Ocean is increasing due to Received in revised form ongoing climate change and the impact this has on POPs in marine receiving systems is unknown This 11 March 2021 study has investigated how secondary sources of POPs from land influence the occurrence and fate of Accepted 13 March 2021 POPs in an Arctic coastal marine system. Available online 17 March 2021 Passive sampling of water and sampling of riverine suspended particulate matter (SPM) and marine sediments for analysis of polychlorinated biphenyls (PCBs) and hexachlorobenzene (HCB) was carried out Keywords: Particle transport in rivers and their receiving fjords in Isfjorden system in Svalbard. Riverine SPM had low contaminant < S e Terrestrial runoff concentrations ( level of detection-28 pg/g dw PCB14,16 100 pg/g dw HCB) compared to outer marine Environmental contaminants sediments 630-880 pg/g dw SPCB14,530e770 pg/g dw HCB). -
Seasonal Dynamics of the Marine CO System in Adventfjorden, a West
RESEARCH ARTICLE Seasonal dynamics of the marine CO2 system in Adventfjorden, a west Spitsbergen fjord Ylva Ericson1,2, Melissa Chierici1,3, Eva Falck1,2, Agneta Fransson4, Elizabeth Jones3 & Svein Kristiansen5 1Department of Arctic Geophysics, University Centre in Svalbard, Longyearbyen, Norway; 2Geophysical Institute, University of Bergen, Bergen, Norway; 3Institute of Marine Research, Fram Centre, Tromsø, Norway; 4Norwegian Polar Institute, Fram Centre, Tromsø, Norway; 5Department of Arctic and Marine Biology, UiT—The Arctic University of Norway, Tromsø, Norway Abstract Keywords Marine carbonate system; aragonite; Time series of the marine CO2 system and related parameters at the IsA Sta- net community production; Arctic fjord tion, by Adventfjorden, Svalbard, were investigated between March 2015 biogeochemistry; Svalbard and November 2017. The physical and biogeochemical processes that govern changes in total alkalinity (TA), total dissolved inorganic carbon (DIC) and the Correspondence Ylva Ericson, Department of Arctic saturation state of the calcium carbonate mineral aragonite (ΩAr) were assessed on a monthly timescale. The major driver for TA and DIC was changes in salin- Geophysics, University Centre in Svalbard, ity, caused by river runoff, mixing and advection. This accounted for 77 and PO Box 156, NO-9171 Longyearbyen, Norway. E-mail: [email protected] 45%, respectively, of the overall variability. It contributed minimally to the variability in ΩAr (5%); instead, biological activity was responsible for 60% of Abbreviations the monthly variations. For DIC, the biological activity was also important, con- ArW: Arctic water; AW: Atlantic water; tributing 44%. The monthly effect of air–sea CO2 fluxes accounted for 11 and CC: coastal current; CTD: conductivity– temperature–depth instrument; DIC: 15% of the total changes in DIC and ΩAr, respectively. -
Arctic Environments
Characteristics of an arctic environment and the physical geography of Svalbard - ‘geography explained’ fact sheet The Arctic environment is little studied at Key Stage Three yet it is an excellent basis for an all-encompassing study of place or as a case study to illustrate key concepts within a specific theme. Svalbard, an archipelago lying in the Arctic Ocean north of mainland Europe, about midway between Norway and the North Pole, is a place with an awesome landscape and unique geography that includes issues and themes of global, regional and local importance. A study of Svalbard could allow pupils to broaden and deepen their knowledge and understanding of different aspects of the seven geographical concepts that underpin the revised Geography Key Stage Three Programme of Study. Many pupils will have a mental image of an Arctic landscape, some may have heard of Svalbard. A useful starting point for study is to explore these perceptions using visual prompts and big questions – where is the Arctic/Svalbard? What is it like? What is happening there? Why is it like this? How will it change? Svalbard exemplifies the distinctive physical and human characteristics of the Arctic and yet is also unique amongst Arctic environments. Perceptions and characteristics of the Arctic may be represented in many ways, including art and literature and the pupil’s own geographical imagination of the place. Maps and photographs are vital in helping pupils develop spatial understanding of locations, places and processes and the scale at which they occur. Source: commons.wikimedia.org/wiki/Image:W_W_Svalbard... 1 Longyearbyen, Svalbard’s capital Source:http://www.photos- The landscape of Western Svalbard voyages.com/spitzberg/images/spitzberg06_large.jpg Source: www.hi.is/~oi/svalbard_photos.htm Where is Svalbard? Orthographic map projection centred on Svalbard and showing location relative to UK and EuropeSource: www.answers.com/topic/orthographic- projection.. -
Ny-Ålesund Research Station
Ny-Ålesund Research Station Research Strategy Applicable from 2019 DEL XX / SEKSJONSTITTEL Preface Svalbard research is characterised by a high degree of interna- tional collaboration. In Ny-Ålesund more than 20 research About the Research Council of Norway institutes have long-term research and monitoring activities. The station is one of four research localities in Svalbard (Ny-Ålesund, Longyearbyen, Barentsburg and Hornsund). The Research Council of Norway is a national strategic and research community, trade and industry and the public Close cooperation between these communities is essential funding agency for research activities. The Council serves as administration. It is the task of the Research Council to identify for the further development of Ny-Ålesund. the key advisor on research policy issues to the Norwegian Norway’s research needs and recommend national priorities Photo: John-Arne Røttingen Government, the government ministries, and other central and to use different funding schemes to help to translate In 2016, the Norwegian Government announced (Meld.St.32 institutions and groups involved in research and development national research policy goals into action. The Research Council (2015-2016)) the development of a research strategy for the (R&D). The Research Council also works to increase financial provides a central meeting place for those who fund, carry out Ny-Ålesund research station. Guidelines and principles for investment in, and raise the quality of, Norwegian R&D and and utilise research and works actively to promote the research activity were established by the government in 2018 to promote innovation in a collaborative effort between the internationalisation of Norwegian research. -
Limits of Acceptable Change Caused by Local Activities in Ny-Ålesund
Limits of acceptable change caused by local activities in Ny-Ålesund Report from a pre-project, containing a proposal for a main project Gunnar Sander, Norwegian Polar Institute 1 Preface Ny-Ålesund has been established as a research town on the assumption that this is an ideal area to study an environment shaped only by natural forces. Consequently the need to keep the environ- mental impacts resulting from local human activities at a low level has been emphasized in many policy statements from the Norwegian government and the actors in Ny-Ålesund. Following up on such policy objectives and recommendations from earlier Environmental Impact Assessments (EIAs) prepared for Ny-Ålesund, Kings Bay initiated a project to operationalize the environmental limits of the operations. During the work, it was clear that it would not be possible to do this without better information about environmental conditions in Ny-Ålesund. New fieldwork would be required to collect data and conduct detailed assessment as to which degree observed changes can be attributed to local activities. The steering group therefore decided to prepare a pre- project, planning a main project that will allow for better definitions of environmental limits. It decided to focus on three areas that according to the EIAs are likely to be most negatively affected by station activities: air quality, vegetation and birds. This report consists of a general part containing an update on the EIAs from Ny-Ålesund with recom- mendations on the general environmental work, and a framework for a main project. Detailed project descriptions of sub-projects on air quality, vegetation and birds are found in annexes.