Novosti Sist. Nizsh. Rast. 48: 374–379
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Exceptional Retreat of Novaya Zemlya's Marine
The Cryosphere, 11, 2149–2174, 2017 https://doi.org/10.5194/tc-11-2149-2017 © Author(s) 2017. This work is distributed under the Creative Commons Attribution 3.0 License. Exceptional retreat of Novaya Zemlya’s marine-terminating outlet glaciers between 2000 and 2013 J. Rachel Carr1, Heather Bell2, Rebecca Killick3, and Tom Holt4 1School of Geography, Politics and Sociology, Newcastle University, Newcastle-upon-Tyne, NE1 7RU, UK 2Department of Geography, Durham University, Durham, DH13TQ, UK 3Department of Mathematics & Statistics, Lancaster University, Lancaster, LA1 4YF, UK 4Centre for Glaciology, Department of Geography and Earth Sciences, Aberystwyth University, Aberystwyth, SY23 4RQ, UK Correspondence to: J. Rachel Carr ([email protected]) Received: 7 March 2017 – Discussion started: 15 May 2017 Revised: 20 July 2017 – Accepted: 24 July 2017 – Published: 8 September 2017 Abstract. Novaya Zemlya (NVZ) has experienced rapid ice al., 2013). This ice loss is predicted to continue during loss and accelerated marine-terminating glacier retreat dur- the 21st century (Meier et al., 2007; Radic´ et al., 2014), ing the past 2 decades. However, it is unknown whether and changes are expected to be particularly marked in the this retreat is exceptional longer term and/or whether it has Arctic, where warming of up to 8 ◦C is forecast (IPCC, persisted since 2010. Investigating this is vital, as dynamic 2013). Outside of the Greenland Ice Sheet, the Russian high thinning may contribute substantially to ice loss from NVZ, Arctic (RHA) accounts for approximately 20 % of Arctic but is not currently included in sea level rise predictions. glacier ice (Dowdeswell and Williams, 1997; Radic´ et al., Here, we use remotely sensed data to assess controls on NVZ 2014) and is, therefore, a major ice reservoir. -
Hot Spots Tackling Environmental Challenges in the Barents Region
Hot Spots Tackling environmental challenges in the Barents Region The unique and highly Contents 3 Case studies Preface sensitive natural ‘environmental hot spots’, was prepared by Preface environment of the Barents Region is ex- the Arctic Monitoring and Assessment Pro- 16 posed to a multitude of threats that need to gramme of the Arctic Council (AMAP) and 4 It all depends be addressed through extensive internation- NEFCO. Over the years, the report has served Co-operation on Lake Onega al efforts. The accelerating climate change is as a frame of reference and compass for on Barents already visible in the Barents region; moreo- tangible projects and measures to address environmental 22 ver, airborne emissions and discharges from environmental issues.. hot spots More heat with less energy industrial facilities have an impact on the As we gather in Inari, Finland, for a meet- 6 ecosystem and cause health problems. En- ing of the BEAC Ministers of Environment Fund Manager’s 26 vironmental pollution transcends national in December 2013, it is time to bring it all Overview Towards a borders and therefore it is important that together and draw conclusions. What envi- 01 cleaner Komi environmental initiatives are addressed by ronmental problems have been attended to ER G 8 international co-operation. and what remains to be done to achieve a Chair’s 30 This year marks the 20th anniversary of cleaner environment in the Barents Region? ASTENBER Overview The hunt the establishment of the Barents Euro-Arctic We will approach these issues partly by pre- R for clean water Council and the Kirkenes Declaration signed senting tangible examples in this brochure atrik P 10 by Norway, Sweden, Denmark, Finland, Ice- of successful environmental projects imple- Environmental 34 land, Russia and the EU. -
Analysis and Prediction of Changes in the Temperature of the Pure Freshwater Ice Column in the Antarctic and the Arctic
Analysis and prediction of changes in the temperature of the pure freshwater ice column in the Antarctic and the Arctic A.A. Fedotov, V.V. Kaniber, P.V. Khrapov Abstract – This paper investigates the initial boundary value problem for a non-stationary one-dimensional heat equation that simulates the temperature distribution in freshwater ice near the Earth's poles. The mathematical model has been constructed taking into account solid-liquid phase transitions. Data from meteorological stations were used to determine the model parameters, with the help of which the necessary physical and thermophysical characteristics of the computational domain were obtained. For the numerical solution of the problem, the finite volume method (FVM) was used. In order to analyze changes in the temperature field of ice and determine the time required to reach a non-stationary periodic regime, graphs of temperature versus depth were plotted for January at two stations. The study of the results showed that it takes about 50 years of modeling with constant initial data for the temperature of an ice layer up to 20 m deep to reach the periodic regime. For the obtained periodic regime, the temperature versus depth dependences for each month were plotted, and the depth of the active layer, as well as the depth of zero annual amplitudes were found for each meteorological station. A forecast of the ice temperature regime for 2100 was modeled for three Representative Concentration Pathway (RCP) scenarios of global warming: moderate RCP2.6, corresponding to the current emissions of RCP7 and adopted at the Paris Agreement in 2015 RCP1.9. -
Durham Research Online
Durham Research Online Deposited in DRO: 10 October 2017 Version of attached le: Published Version Peer-review status of attached le: Peer-reviewed Citation for published item: Carr, J. Rachel and Bell, Heather and Killick, Rebecca and Holt, Tom (2017) 'Exceptional retreat of Novaya Zemlya's marine-terminating outlet glaciers between 2000 and 2013.', The cryosphere., 11 (5). pp. 2149-2174. Further information on publisher's website: https://doi.org/10.5194/tc-11-2149-2017 Publisher's copyright statement: c Author(s) 2017. This work is distributed under the Creative Commons Attribution 3.0 License. Additional information: Use policy The full-text may be used and/or reproduced, and given to third parties in any format or medium, without prior permission or charge, for personal research or study, educational, or not-for-prot purposes provided that: • a full bibliographic reference is made to the original source • a link is made to the metadata record in DRO • the full-text is not changed in any way The full-text must not be sold in any format or medium without the formal permission of the copyright holders. Please consult the full DRO policy for further details. Durham University Library, Stockton Road, Durham DH1 3LY, United Kingdom Tel : +44 (0)191 334 3042 | Fax : +44 (0)191 334 2971 https://dro.dur.ac.uk The Cryosphere, 11, 2149–2174, 2017 https://doi.org/10.5194/tc-11-2149-2017 © Author(s) 2017. This work is distributed under the Creative Commons Attribution 3.0 License. Exceptional retreat of Novaya Zemlya’s marine-terminating outlet glaciers between 2000 and 2013 J. -
NATIONAL REPORT by RUSSIA – SEPTEMBER 2015 Enhanced Black Carbon and Methane Emissions Reductions– an Arctic Council Framework for Action
NATIONAL REPORT BY RUSSIA – SEPTEMBER 2015 Enhanced Black Carbon and Methane Emissions Reductions– an Arctic Council Framework for Action Ministry of Natural Resources and Environment of the Russian Federation NATIONAL REPORT ON THE ACTIONS ON BLACK CARBON AND METHANE EMISSIONS REDUCTION in accordance with the Framework for Action on Enhanced Black Carbon and Methane Emissions Reductions (April 24, 2015, Iqaluit, Canada) Moscow, 2015 2 Table of Contents 1. Introduction 3 2. Black Carbon Emissions 4 3. Methane Emissions 9 4. National Actions on Emissions Reduction 14 5. Best Practices and International Cooperation 17 6. Activities Aimed at the Improvement of the Situation in the Arctic 19 Region 7. Conclusion 21 3 Introduction The Arctic is one of the most sensitive regions of the planet in terms of climate change. Changes in the climate and environment of the Arctic have widespread effects on societies and the whole ecosystem, as well as repercussions around the world. This makes evident the need to undertake urgent measures both nationally and globally for climate change mitigation and adaptation. Climate change and technological breakthroughs are opening the Arctic, its riches and resources, to commercial development. We welcome the adoption of the Framework for Action on Enhanced Black Carbon and Methane Emissions Reductions by the Arctic Council. From our perspective, it is a timely step towards dealing with climate and environmental challenges in the Arctic region. The Arctic Zone of the Russian Federation is the largest in the world; no other country has such vast territories above the Arctic Circle. 2.4 million people live in the Arctic. -
4604. Declaration
Page 1 4450. Declaration By a decree dated 15 January 1985, the USSR Council of Ministers approved a list of the geographical co-ordinates of the points defining the position of the baselines for measuring the breadth of the territorial sea, the exclusive economic zone and the continental shelf of the USSR off the continental coast and islands of the Arctic Ocean and the Baltic and Black seas, as given below. The same decree establishes that the waters of the White Sea south of the line connecting Cape Svyatoy Nos with Cape Kanin Nos, the waters of Cheshskaya/Bay south of the line connecting Cape Mikulkin with Cape Svyatoy/Nos (Timansky), and the waters of Baidaratskaya Bay south-east of the line connecting Cape Yuribeisalya with Cape Belushy Nos are, as waters historically belonging to the USSR, internal waters. Arctic Ocean Co-ordinates Point Geographical location North East number of point latitude longitude 1 Boundary sign No. 415 (sea buoy) 69°47'41" 30°49'15" 2 Cape Nemetsky 69°57.2' 31°56.7' 3 Islet to the east of Cape 69 57.2 31 57.2 Nemetsky 4 Cape Kekursky 69 56.7 32 03.5 5 Islet to the south-east of 69 56.4 32 05.4 Cape Kekursky 6 Islet off Cape Lognavolok 69 46.2 32 57.4 7 Islet off Cape Laush 69 44.5 33 04.8 Thence following the low-water line to point 8 8 Rybachy Peninsula, Cape 69 42.9 33 07.9 Tsypnavolok 9 Kil'din Island, north-west coast 69 22.8 34 01.8 Thence following the low-water line to point 10 10 Kil'din Island, eastern 69 20.0 34 24.2 extremity 11 Cape to the east of Cape 69 15.2 35 15.2 Teribersky 12 Cape to the -
Årsmelding Annual Report 2019 Norsk Polarinstitutt Norwegian Polar Institute
ÅRSMELDING ANNUAL REPORT 2019 NORSK POLARINSTITUTT NORWEGIAN POLAR INSTITUTE 1 Norsk Polarinstitutt i verden / Norwegian Polar Institute in the world Norsk Polarinstitutt holder til i Framsenteret i Tromsø – et nettverk av 20 institusjoner med kunnskap om nordområdene. Instituttet har i tillegg medarbeidere stasjonerte i Ny-Ålesund og Longyearbyen på Svalbard og på Trollstasjonen i Dronning Maud Land i Antarktis. The Norwegian Polar Institute is situated in Tromsø at the Fram Centre, a network of 20 institutions with specialist knowledge about the High North. In addition, the Institute has personnel in Ny-Ålesund and Longyearbyen in Svalbard, and at the Troll Research Station in Dronning Maud Land in Antarctica. Kart/Map: Anders Skoglund, NP / NPI 2 Innhold . Contents Side . Page Forord 4 Mandat og finansiering 5 Forvaltningsmyndighet 5 Organisasjon og ledelse 6 Økonomi 6 Forvaltning, rådgivning og forskning 7 Logistikk og infrastruktur 25 Markeringer og hendelser 27 Artikler . Articles Antarktistraktaten 60 år 30 Celebrating 60 years of the Antarctic Treaty 32 FF Kronprins Haakon på førstereis til Kong Håkon VII Hav 34 The RV Kronprins Haakon on its maiden voyage to the Kong Håkon VII Hav 36 På tokt i nordlige havområder 38 On a research cruise in northern waters 40 Ny-Ålesund forskningsstasjon _ ny rolle for Norsk Polarinstitutt 42 Ny-Ålesund Research Station _ a new role for the Norwegian Polar Institute 44 Annual Report 2019 (in English) 46 Utgivelser . Publications . Fagfellevurderte artikler . Peer-reviewed journal papers 65 Norsk Polarinstitutt forkortes flere steder til NP i bildetekstene. I den elektroniske versjonen er det lenket til publikasjonene som det refereres til i publikasjonsoversikten. -
ARCTIC FLOATING UNIVERSITY PROGRAM 8–28 July 2017
ARCTIC FLOATING UNIVERSITY PROGRAM 8–28 July 2017 Saturday 8th 12.00 Departure of RV «Professor Molchanov» from Arkhanglesk Introductory meeting of the expedition participants, safety traing 14.00 – 15.00 Lunch Evacuation training from the vessel 18.00 – 19.00 Dinner Presentation of the expedition route Announcements on tomorrow schedule Introduction of the expedition members Sunday 9th 8.00-9.00 Breakfast Lecture: Introduction to physical oceanography (Vesman Anna, Arctic and Antarctic Research Institute ) Lecture: Weather and climate. Factors of climate formation (Urazgildeeva Aleksandra, Arctic and Antarctic Research Institute) 12.00-13.00 Lunch Lecture: XVIth century : "Reaching China,’Discovering' of Northern Russia" (Hösli Eric, Federal Polytechnic School of Lausanne) Lecture: Formation of landscapes in polar regions of the Earth - geographical zonality, factors and processes (Goryachkin Sergey, Institute of Geography, Russian Academy of Sciences ) Group work 18.00 -19.00 Dinner Lecture: Regional Geology of the Barents-Kara continental margin of Eurasia (Dmitry Metelkin, Novosibirsk State University) Announcements on tomorrow schedule Monday 10th 8.00-9.00 Breakfast Lecture: The Arctic Ocean (Vesman Anna, Arctic and Antarctic Research Institute ) Lecture: Features of climate formation in the Arctic (Urazgildeeva Aleksandra, Arctic and Antarctic Research Institute) 12.00-13.00 Lunch Lecture: XVIIIth and XIXth century : "Is There a Passage between Asia and America?” (Hösli Eric, Federal Polytechnic School of Lausanne) Lecture: Geoecological characteristics of European Arctic archipelagos and coasts and global change challenges (Goryachkin Sergey, Institute of Geography, Russian Academy of Sciences ) Group work 18.00 -19.00 Dinner Lecture: The Intrigue of Mesozoic Magmatism on the Franz Josef Land Archipelago: a Hot Spot or a Failed Rift? (Mikhaltsov Nikolay, Novosibirsk State University) Announcements on tomorrow schedule Tuesday 11th 8.00-9.00 Breakfast Lecture: The features of hydrological regime of the Barents Sea. -
FIRST ANNOUNCEMENT “Arctic Floating University -2017” Expedition Project «ARCTICUM INCOGNITA»
FIRST ANNOUNCEMENT “Arctic Floating University -2017” Expedition Project «ARCTICUM INCOGNITA» Expedition Dates: July 08-28, 2017 Expedition Duration: 20 days Expedition Organizers: Northern (Arctic) Federal University named after M.V. Lomonosov; Russian Hydrometeorological Agency (RosHydroMet) Expedition Route: Arkhangelsk – the Zhelaniya Cape (Novaya Zemlya) – Hall Island (Franz Josef Land) – Heiss Island (Franz Josef Land) – Jackson Island (Franz Josef Land) – Rudolf Island (Franz Josef Land) – Hooker Island (Franz Josef Land) – Northbrook Island (Franz Josef Land) – Bell Island (Franz Josef Land) – Arkhangelsk. Expedition participants: 58 people (undergraduates, post-graduates, research fellows of Russian and foreign scientific and academic institutions) Partners participating in the expedition: Russian Geographical Society, Russian Arctic National Park, Lomonosov Moscow State University, University of Geneva, University of Lausanne, Federal Polytechnic School of Lausanne. Aims of the expedition: acquiring new knowledge about the state and changes in the ecosystem of the coastal areas of Franz Josef Land archipelago; training young specialists of the Arctic-focused subjects: hydrometeorology, ecology, arctic biology, geography, ethnopolitology, international law etc. RESEARCH PROGRAM: assessment of state and degree of contamination within the local island territories of the former economic activities in the areas of work for the elimination of accumulated environmental damage; study of the species diversity of living organisms and populations in the archipelago of Franz Josef Land and adjacent waters in the context of climate change; study of historical and cultural heritage of the Russian Arctic National park for the purposes of development of tourism and educational activities; study of adaptive mechanisms of the human organism to the conditions of the High Arctic. EDUCATIONAL PROGRAM: The Program focuses on the bachelor, master and PhD students. -
Sea Ice Studies in the Northern Sea Route by Use of Synthetic Aperture Radar
NERSCNERSC Nansen Environmental and Telemark University College Remote Sensing Center Sea Ice Studies in the Northern Sea Route by use of Synthetic Aperture Radar by Maria Lundhaug Dr. Ing. Thesis February 2002 the Norwegian University of Science and Technology URN:NBN:no-2344 Abstract The main objective of this thesis is to contribute to the understanding of sea ice pro- cesses in the Northern Sea Route, mainly with use of remote sensing data from Synthetic Aperture Radar (SAR). Multivariate data analysis is the main tool used in this work. SAR signatures of different sea ice types and open water in winter were studied, and separation of water and sea ice types using different multivariate regression algorithms was done. Polynya areas along the coasts were investigated. Structure characteristics of different sea ice types and open water were investigated. The summer sea ice in the Laptev Sea was also studied. The Laptev Sea as well as other parts of the Northern Sea Route are expected to become important areas for future oil and gas exploration and exploitation. Results from a statistical analysis of 105 SAR images and corresponding meteorological data are presented, covering parts of the Pechora and Kara Sea in the Russian Arctic. Wind, temperature and other variables for the SAR sample areas were collected, and a manual sea ice classification of the SAR samples was performed. All variables were input to different multivariate regression techniques. First, ice was separated from water. Next, young ice was separated from rough first year ice. The study indicated that the mean and standard deviation of the backscattering coefficients together with temperature values were the most important information to separate the classes. -
Of the Russian Arctic Islands in the Barents Sea
Polar Biology https://doi.org/10.1007/s00300-018-2425-z ORIGINAL PAPER Moths and butterfies (Insecta: Lepidoptera) of the Russian Arctic islands in the Barents Sea J. Kullberg1 · B. Yu. Filippov2 · V. M. Spitsyn2,3 · N. A. Zubrij2,3 · M. V. Kozlov4 Received: 28 April 2018 / Revised: 10 October 2018 / Accepted: 22 October 2018 © The Author(s) 2018 Abstract Faunistic data are scarce for the Lepidoptera from the Arctic islands of European Russia. New sampling and revision of the earlier fndings have revealed the occurrence of 60 species of moths and butterfies on Kolguev, Vaygach and Dolgij Islands and on the Novaya Zemlya archipelago. The faunas of Kolguev and Dolgij Islands (19 and 18 species, respectively) include typical moths of the northern taiga (Aethes deutschiana, Syricoris lacunana and Xanthorhoe designata), and the low num- bers of species discovered on these islands have resulted primarily from low collecting eforts. By contrast, the fauna of Vaygach Island (22 species) is relatively well known and includes several high Arctic species, such as Xestia aequaeva, X. liquidaria and X. lyngei. Nevertheless, Vaygach Island is depauperated even relative to the fauna of Amderma (29 species), which is located on the continent next to the Vaygach Island. The fauna of Novaya Zemlya totals 30 species, but only eight of these were collected from the Northern Island, mostly near Matochkin Shar strait. Noteworthy is the record of Plutella polaris from Novaya Zemlya: this species was recently re-discovered in Svalbard, where the type series was collected in 1873. Udea itysalis, described from North America, is reported here for the frst time from Europe. -
2009 Book Sedimentationhistor
Lecture Notes in Earth Sciences 118 Editors: J. Reitner, Gottingen¨ M. H. Trauth, Potsdam K. Stuwe,¨ Graz D. Yuen, USA Founding Editors: G. M. Friedman, Brooklyn and Troy A. Seilacher, Tubingen¨ and Yale M.A. Levitan · Yu.A.Lavrushin Sedimentation History in the Arctic Ocean and Subarctic Seas for the Last 130 kyr 123 Dr.M.A.Levitan Dr. Yu. A. Lavrushin Russian Academy of Sciences Russian Academy of Sciences Vernadsky Inst. Geochemistry Inst. Geology Analytical Chemistry Pyzhevsky per. 7 Kosygina Str. 19 Moscow Moscow Russia 119017 Russia 119991 [email protected] [email protected] ISSN 0930-0317 ISBN 978-3-642-00287-8 e-ISBN 978-3-642-00288-5 DOI 10.1007/978-3-642-00288-5 Springer Dordrecht Heidelberg London New York Library of Congress Control Number: 2009926693 c Springer-Verlag Berlin Heidelberg 2009 This work is subject to copyright. All rights are reserved, whether the whole or part of the material is concerned, specifically the rights of translation, reprinting, reuse of illustrations, recitation, broadcasting, reproduction on microfilm or in any other way, and storage in data banks. Duplication of this publication or parts thereof is permitted only under the provisions of the German Copyright Law of September 9, 1965, in its current version, and permission for use must always be obtained from Springer. Violations are liable to prosecution under the German Copyright Law. The use of general descriptive names, registered names, trademarks, etc. in this publication does not imply, even in the absence of a specific statement, that such names are exempt from the relevant protective laws and regulations and therefore free for general use.