PCB on Svalbard
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Handbok07.Pdf
- . - - - . -. � ..;/, AGE MILL.YEAR$ ;YE basalt �- OUATERNARY votcanoes CENOZOIC \....t TERTIARY ·· basalt/// 65 CRETACEOUS -� 145 MESOZOIC JURASSIC " 210 � TRIAS SIC 245 " PERMIAN 290 CARBONIFEROUS /I/ Å 360 \....t DEVONIAN � PALEOZOIC � 410 SILURIAN 440 /I/ ranite � ORDOVICIAN T 510 z CAM BRIAN � w :::;: 570 w UPPER (J) PROTEROZOIC � c( " 1000 Ill /// PRECAMBRIAN MIDDLE AND LOWER PROTEROZOIC I /// 2500 ARCHEAN /(/folding \....tfaulting x metamorphism '- subduction POLARHÅNDBOK NO. 7 AUDUN HJELLE GEOLOGY.OF SVALBARD OSLO 1993 Photographs contributed by the following: Dallmann, Winfried: Figs. 12, 21, 24, 25, 31, 33, 35, 48 Heintz, Natascha: Figs. 15, 59 Hisdal, Vidar: Figs. 40, 42, 47, 49 Hjelle, Audun: Figs. 3, 10, 11, 18 , 23, 28, 29, 30, 32, 36, 43, 45, 46, 50, 51, 52, 53, 54, 60, 61, 62, 63, 64, 65, 66, 67, 68, 69, 71, 72, 75 Larsen, Geir B.: Fig. 70 Lytskjold, Bjørn: Fig. 38 Nøttvedt, Arvid: Fig. 34 Paleontologisk Museum, Oslo: Figs. 5, 9 Salvigsen, Otto: Figs. 13, 59 Skogen, Erik: Fig. 39 Store Norske Spitsbergen Kulkompani (SNSK): Fig. 26 © Norsk Polarinstitutt, Middelthuns gate 29, 0301 Oslo English translation: Richard Binns Editor of text and illustrations: Annemor Brekke Graphic design: Vidar Grimshei Omslagsfoto: Erik Skogen Graphic production: Grimshei Grafiske, Lørenskog ISBN 82-7666-057-6 Printed September 1993 CONTENTS PREFACE ............................................6 The Kongsfjorden area ....... ..........97 Smeerenburgfjorden - Magdalene- INTRODUCTION ..... .. .... ....... ........ ....6 fjorden - Liefdefjorden................ 109 Woodfjorden - Bockfjorden........ 116 THE GEOLOGICAL EXPLORATION OF SVALBARD .... ........... ....... .......... ..9 NORTHEASTERN SPITSBERGEN AND NORDAUSTLANDET ........... 123 SVALBARD, PART OF THE Ny Friesland and Olav V Land .. .123 NORTHERN POLAR REGION ...... ... 11 Nordaustlandet and the neigh- bouring islands........................... 126 WHA T TOOK PLACE IN SVALBARD - WHEN? .... -
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. -
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. -
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. -
Foraminifera1 Stratigraphy of Raised Marine Deposits, Representing Isotope Stage 5, Prins Karls Forland, Western Sval Bard
Foraminifera1 stratigraphy of raised marine deposits, representing isotope stage 5, Prins Karls Forland, western SVal bard HELENE BERGSTEN. TORBJORN ANDERSON and OLAFUR INGOLFSSON Bergsten, H., Andersson. T. & Ingolfsson, 0. 1998: Foraminiferd stratigraphy of raised marine deposits, representing isotope stage 5. Prins Karls Forland, western Svalbard. Polar Research 17(1). 81-91. Two raised marine sequences from Prim Karls Forland, western Svalbard, interpreted to have been deposited during part of isotope substage Se (Eemian) and substage 5a, were studied for foraminifera content. Time constraints are given by I4C ages, infrared stimulated luminescence age estimates and amino acid ratios in suhfossil marine molluscs. A diamicton (unit B) separates the two marine sequences and reflects an advancement of local glaciers sometime late in isotope stage 5. The two marine sequences contain diverse benthic foraminifera1 faunas, indicating periods of a relatively warm and seasonally ice-free marine shelf environment. Compared to the lowermost sequence (unit A), the upper marine sequence (unit C) seems to reflect a more shallow environment that could have resulted from the global lowering of the sea level towards the end of isotope stage 5. Our results further emphasise the problem of biostratigraphic distinction between interglacial and interstadial deposits at high latitudes, with temperature conditions for substage Sa close to those of substage 5e and present conditions. Helene Bergsten, Torbjorn Andersson and Olufur Ingdlfsson, Earth Sciences Centre, Goteborg University, Box 460, S-405 30 Goteborg, Sweden. Introduction Chronology and glacial history The Poolepynten site is situated on Prins Karls Sediments in the Poolepynten sections are ex- Forland, western Svalbard at N78'27'El l"40' posed in up to 10 metre high coastal cliffs over a (Fig. -
Heavy Rain Events in Svalbard Summer and Autumn of 2016 to 2018
Heavy Rain Events in Svalbard Summer and Autumn of 2016 to 2018 Ola Bakke Aashamar Thesis submitted for the degree of Master of Science in Meteorology Department of Geosciences Faculty of Mathematics and Natural Sciences University of Oslo Department of Arctic Geophysics The University Centre in Svalbard August 15, 2019 2 “ Når merket vel dere byfolk her i deres stengte gater selv det minste pust av den frihet som tindrer over Ishavets veldige rom? Sto en eneste av dere noensinne ensom under Herrens øyne i et øde av snø og natt? Stirret dere noen gang opp i polarlandets flammende nordlys og forstod de tause toner som strømmet under stjernene? Hva vet dere om de makter som taler i stormer, som roper i snøløsningens skred og som jubler i fuglefjellenes vårskrik? Ingenting. “ - Fritt etter John Giæver, Ishavets glade borgere (1956) 3 Acknowledgements First of all, I am forever grateful to my main supervisor Marius Jonassen, who with his great insight and supportive comments gave me all the motivation and help I needed along the way towards this master thesis. Big round of applause to all the amazing students and staff at UNIS who I was lucky to meet during my stays in Svalbard, and the people at MetOs in Oslo. The times shared with you inspire me both personally and professionally, and I will always keep the memories! Then I want to thank Grete Stavik-Døvle, Terje Berntsen, Frode Stordal and Karl-Johan Ullavik Bakken for admitting and guiding two lost NTNU students into studies at UiO. If not for you, who knows what would have happened. -
Tertiary Fold-And-Thrust Belt of Spitsbergen Svalbard
Winfried K. Dallmann • Arild Andersen • Steffen G. Bergh • Harmond D. Maher Jr. • Yoshihide Ohta Tertiary fold-and-thrust belt of Spitsbergen Svalbard ' ~dl... ,, !!~"\\ MEDDELELSER NR.128 9,.~,f OSLO 1993 k ·pOlARll'l'>'\ MEDDELELSER NR. 128 WINFRIED K. DALLMANN, ARILD ANDRESEN, STEFFEN G. BERGH, HARMON D. MAHER Jr. & YOSHIHIDE OHTA Tertiary f old-and-thrust belt of Spitsbergen Svalbard COMPILATION MAP, SUMMARY AND BIBLIOGRAPHY NORSK POLARINSTITUTT OSLO 1993 Andresen, Arild: Univ. Oslo, Institutt for geologi, Pb. 1047 Blindern, N-0316 Oslo Bergh, Steffen G.: Univ. Tromsø, Institutt for biologi og geologi, N-9037 Tromsø Dallmann, Winfried K.: Norsk Polarinstitutt, Pb. 5072 Majorstua, N-0301 Oslo Maher, Harmon D., Jr.: Univ. Nebraska, Dept. of Geography and Geology, Omaha, USA-Nebraska 68182-0199 Ohta, Yoshihide: Norsk Polarinstitutt, Pb. 5072 Majorstua, N-0301 Oslo ISBN 82-7666-065-7 Printed December 1993 Cover photo by W. K. Dallmann: Folded Triassic sandstones and shales within the interior part of the Tertiary fold-and-thrust belt at Curie Sklodowskafjellet, Wedel Jarlsberg Land, Svalbard. CONTENTS: Introduction 5 Map data and explanatory remarks 6 Sources, compilation and accuracy of the geological base map 7 Explanation of map elements 7 Stratigraphy 7 Structure 8 Outline of the Tertiary fold-and-thrust belt of Spitsbergen 10 Tectonic setting 10 Dimensions and directions 11 Structural subdivision and characteristics 13 Interior part of foldbelt 13 Western Basement High 15 Forlandsundet Graben 16 Central Tertiary Basin 16 Billefjorden Fault Zone 17 Lomfjorden Fault Zone 17 Structural descriptions (including explanation of cross sections) 17 Sørkapp-Hornsund area 17 Interior Wedel Jarlsberg Land/Torell Land - Bellsund 19 Western and Central Nordenskiold Land 21 Oscar li Land 22 Brøggerhalvøya 24 Billefjorden - Eastern Nordenskiold Land 24 Agardhbukta - Negribreen 25 Bibliography 29 Maps and map descriptions 29 Proceedings of symposia etc. -
P-092 Cornice Dynamics Above Nybyen in Svalbards High Arctic
2010 International Snow Science Workshop P-092 Cornice dynamics above Nybyen in Svalbards high arctic landscape Stephan C. Vogel1 Markus Eckerstorfer1 Hanne Christiansen1, 2 1. Arctic Geology Department, University Centre in Svalbard, Longyearbyen, Norway; 2. Department of Geosciences, University of Oslo, Oslo, Norway The development of cornices, their cracking and consequent failures largely controlled by meteorology along the Gruvefjellet plateau ridge was investigated in the two consecutive snow seasons of 2009 and 2010. These natural processes endanger life and infrastructure in Longyearbyen, Svalbard’s main settlement in the High Arctic. Two automatic time lapse cameras provided up to 6 daily pictures of the entire Gruvefjellet slope from the valley bottom and monitored the cornice development and tension cracking from the ridgeline. Further- more stakes on the plateau were used to record snow depth distribution and cornice growth. 45 field trips up the plateau were carried out to study the processes and to manually measure cornice crack opening rates. Meteorological data were recorded by an automatic weather station situated on the Gruvefjellet plateau source area. Both snow seasons indicated that cornices were built up by a low number of distinct storm events and that cornice scouring due to high wind speeds is rather limited. In 2009 the first cornice cracks were observed in mid April, while in 2010, probably due to persistent warm weather in combination with large amounts of rain, cornice cracks were already developing at the end of January. Cornice crack measurements showed a linear de- velopment, indicating the major influence of gravity. 177 cornice failures have been recorded, whereof 11 were “D3-R3” and “D3-R4” avalanches which nearly reached housing infrastructure. -
Svalbard (Norway)
Svalbard (Norway) Cross border travel - People - Depending on your citizenship, you may need a visa to enter Svalbard. - The Norwegian authorities do not require a special visa for entering Svalbard, but you may need a permit for entering mainland Norway /the Schengen Area, if you travel via Norway/the Schengen Area on your way to or from Svalbard. - It´s important to ensure that you get a double-entry visa to Norway so you can return to the Schengen Area (mainland Norway) after your stay in Svalbard! - More information can be found on the Norwegian directorate of immigration´s website: https://www.udi.no/en/ - Find more information about entering Svalbard on the website of the Governor of Svalbard: https://www.sysselmannen.no/en/visas-and-immigration/ - Note that a fee needs to be paid for all visa applications. Covid-19 You can find general information and links to relevant COVID-19 related information here: https://www.sysselmannen.no/en/corona-and-svalbard/ Note that any mandatory quarantine must be taken in mainland Norway, not on Svalbard! Find more information and quarantine (hotels) here: https://www.regjeringen.no/en/topics/koronavirus-covid- 19/the-corona-situation-more-information-about-quarantine- hotels/id2784377/?fbclid=IwAR0CA4Rm7edxNhpaksTgxqrAHVXyJcsDBEZrtbaB- t51JTss5wBVz_NUzoQ You can find further information regarding the temporary travel restrictions here: https://nyalesundresearch.no/covid-info/ - Instrumentation (import/export) - In general, it is recommended to use a shipping/transport agency. - Note that due to limited air cargo capacity to and from Ny-Ålesund, cargo related to research activity should preferably be sent by cargo ship. -
Springtime Nitrogen Oxides and Tropospheric Ozone in Svalbard: Local and Long-Range Transported Air Pollution
EGU21-9126 https://doi.org/10.5194/egusphere-egu21-9126 EGU General Assembly 2021 © Author(s) 2021. This work is distributed under the Creative Commons Attribution 4.0 License. Springtime nitrogen oxides and tropospheric ozone in Svalbard: local and long-range transported air pollution Alena Dekhtyareva1, Mark Hermanson2, Anna Nikulina3, Ove Hermansen4, Tove Svendby5, Kim Holmén6, and Rune Graversen7 1Geophysical Institute, University of Bergen and Bjerknes Centre for Climate Research, Bergen, Norway ([email protected]) 2Hermanson and Associates LLC, Minneapolis, USA 3Department of Research Coordination and Planning, Arctic and Antarctic Research Institute, Russia 4Department of Monitoring and Information Technology, NILU - Norwegian Institute for Air Research, Norway 5Department of Atmosphere and Climate, NILU - Norwegian Institute for Air Research, Norway 6International director, Norwegian Polar Institute, Longyearbyen, Norway 7Department of Physics and Technology, UiT The Arctic University of Norway, Tromsø, Norway Svalbard is a near pristine Arctic environment, where long-range transport from mid-latitudes is an important air pollution source. Thus, several previous studies investigated the background nitrogen oxides (NOx) and tropospheric ozone (O3) springtime chemistry in the region. However, there are also local anthropogenic emission sources on the archipelago such as coal power plants, ships and snowmobiles, which may significantly alter in situ atmospheric composition. Measurement results from three independent research projects were combined to identify the effect of emissions from various local sources on the background concentration of NOx and O3 in Svalbard. The hourly meteorological and chemical data from the ground-based stations in Adventdalen, Ny-Ålesund and Barentsburg were analysed along with daily radiosonde soundings and weekly data from O3 sondes. -
Variability of Fast-Ice Thickness in Spitsbergen Fjords
Annals of Glaciology 44 2006 231 Variability of fast-ice thickness in Spitsbergen fjords Sebastian GERLAND, Richard HALL* Norwegian Polar Institute, Polar Environmental Centre, NO-9296 Tromsø, Norway E-mail: [email protected] ABSTRACT. Detailed measurements of sea-ice thickness and snow on sea ice were recorded at different locations in fjords along the western coast of Spitsbergen, the largest island in the Svalbard archipelago, in 2004. Data corresponding to the ice situation before and after melt onset were collected for Kongsfjorden and Van Mijenfjorden, while Hornsund was investigated once during early spring. Profiles of total thickness (snow plus ice thickness) were measured, together with some snow-thickness measure- ments. Total thicknesses were measured with a portable electromagnetic instrument and at selected sites by drilling. The three fjords show some differences in measured thicknesses, connected to individual conditions. However, total thickness does not differ substantially between the three fjords before melt onset. The modal total thickness for all three fjords before melt onset was 1.075 m, and the corresponding modal snow thickness was 0.225 m (bin width 0.05 m). Long-term Kongsfjorden ice-thickness data since 1997 show that the maximum ice thickness varies significantly interannually, as observed at other Arctic sites. The average maximum ice thickness for Kongsfjorden was 0.71 m (years 1997–98, 2000 and 2002–05), and the respective average maximum snow thickness was 0.22 m. In Kongsfjorden, 2004 was the year with highest maximum total thickness and snow thickness relative to the other years. INTRODUCTION Characteristics of fast-ice formation and evolution in The variability, distribution and trends of sea-ice thickness Kongsfjorden differ from those in most other high-Arctic are central issues in current polar climate research (e.g.