Science Plan for COAT: Climate-Ecological Observatory for Arctic Tundra

Total Page:16

File Type:pdf, Size:1020Kb

Science Plan for COAT: Climate-Ecological Observatory for Arctic Tundra Science Plan for COAT: Climate-Ecological Observatory for Arctic Tundra 78º N 70º N FRAM – High North Research Centre for Climate and the Environment Fram Centre Report Series No. 1 Science Plan for COAT: Climate-Ecological Observatory for Arctic Tundra Editors: Rolf A. Ims, Jane U. Jepsen, Audun Stien & Nigel G. Yoccoz Science plan for COAT: Climate-ecological Observatory for Arctic Tundra Editors: Rolf A. Ims, Jane U. Jepsen, Audun Stien & Nigel G. Yoccoz Publisher: Fram Centre by the University of Tromsø Year of publication: 2013 Number of pages: 177 Cover photo: Geir Vie Cover layout: Ingrid Jensvoll and Jane U. Jepsen Typesetting: Jane U. Jepsen Printing: Troms Produkt, Tromsø, Norway ISBN: 978-82-999253-0-3 The publication should be cited as follows: Ims, R.A., Jepsen, J.U., Stien, A. & Yoccoz, N.G. 2013. Science plan for COAT: Climate-ecological Observatory for Arctic Tundra. Fram Centre Report Series 1, Fram Centre, Norway, 177 pages. Notes: The Fram Centre is the short name for FRAM– High North Research Centre for Climate and the Environment. The Fram Centre is based in Tromsø and consists of 21 institutions involved in interdisciplinary research in the field of natural science, technology and social sciences. The following Fram Centre institutions are involved in COAT: University of Tromsø, Norwegian Institute for Nature Research, Norwegian Polar Institute, University Centre in Svalbard and Norwegian Meteorological Institute. The science plan is coordinated by the University of Tromsø, and financienced with contributions from: The Ministry of Education and Research The University of Tromsø Norwegian Polar Institute Norwegian Institute for Nature Research The Fram Centre TABLE OF CONTENTS FOREWORD 5 EXECUTIVE SUMMARY 7 1. BACKGROUND AND RATIONALE 9 1.1. Arctic tundra ecosystem 9 1.2. Long-term research and monitoring 23 2. COAT MODULES 29 2.1. Monitoring targets and conceptual climate impact path models 29 2.2 Tundra-forest ecotone module (Varanger) 31 2.3 Tall shrub (Varanger) 41 2.4 Small rodent module (Varanger) 51 2.5 Ungulate module (Varanger and Svalbard) 65 2.6 Ptarmigan module (Varanger and Svalbard) 77 2.7 Goose module (Svalbard) 89 2.8 Arctic fox module (Varanger and Svalbard) 97 2.9. Monitoring design and methods 111 2.10. Data management and analysis 137 3. ORGANIZATION 141 4. INTERNATIONAL COLLABORATION 143 4.1. Pan-arctic perspectives 143 4.2. Links to other established ecosystem-based observatories 144 4.3. COAT Russia 144 5. SOCIETY INVOLVEMENTS, EDUCATION AND OUTREACH 147 5.1. Management issues and stakeholder fora 147 5.2. Education 148 5.3. Outreach 151 Literature cited 153 FOREWORD In connection with the opening of Fram – High ranger Peninsula were informed about the project North Centre for Climate and the Environment in in a meeting in the Ministry of Environment in fall 2010, the centre was tasked to initiate a plan- February 2011. ning project for a Climate ecological Observatory A draft of the science plan for COAT was submit- for Arctic Tundra (COAT). The planning project ted for review by an expert panel administrated by was funded by the Ministry of Science and the the Division for Energy, Resources and the Envi- University of Tromsø and Professor Rolf A. Ims ronment of The Research Council of Norway in was appointed as the leader. A task force was es- June 2012. Their consensus review report was tablished in January 2011 with members from ready in November 2012. The review provided full Department of Arctic and Marine Biology at the support for the COAT science plan and conclud- University of Tromsø, (Kari Anne Bråthen, John- ed that “the original approach will make a world- André Henden, Dorothee Ehrich, Vera H. Haus- class contribution”, “making this well-conceived ner, Rolf A. Ims, Ingrid Jensvoll, Siw Killengreen, and major initiative operational will simply rely on Virve Ravolainen, Nigel G. Yoccoz), Department resources as all the necessary components, particu- of Arctic Ecology of the Norwegian Institute of lary concepts and experience, are present” and that Nature Research (Martin Biuw, Per Fauchald, it was their opinion “that the project should be Jane U. Jepsen, Audun Stien, Ingunn Tombre, funded appropriately and encouraged into the long Torkild Tveraa), Norwegian Polar Institute (Eva -term […] with all due haste”. The 10-page review Fuglei, Jack Kohler, Åshild Ø. Pedersen), Universi- report provided also a set of contructive sugges- ty Centre of Svalbard (Steve Coulson, Pernille B. tions about additional scientific issues to be in- Eidesen, Eike Müller). Ole Einar Tveito cluded in the plan as to make COAT even more (Norwegian Meteorological Institute), Elisabeth comprehensive and, moreover, good advices on Cooper (AMB, UoT) and Jesper Madsen organizational issues that could make COAT (University of Aarhus) later joined the task force. more robust. The present version of the science The scientific scope and overall approach for plan, which is published as the first issue of the COAT was agreed on during the course of a series Fram Centre’s report series, represents a revision of internal meetings during the spring of 2011. of the draft plan submitted for review. It should, During these meetings the main responsibility for however, not be considered as a final product. writing the module chapters was allocated to the According to COAT’s paradigm of adaptive long- different specialist members of the task force. It term science, its plan should also be an “adaptive was also agreed that all the main modules of the entity” frequently subjected to revisions and im- COAT science plan should be thoroughly pre- provements. sented and discussed in workshops in which ex- ternal referees were invited. Eight workshops were held during May – December 2011. The fol- Tromsø June 25th, 2013 lowing colleagues kindly acted as referees during these workshops: Anders Angerbjörn, Tom Ed- wards, Heikki Henttonen, Greg Henry, Annika Hofgaard, Jesper Madsen, Jim Nichols, Carl Mitch- ell, Erling Solberg and Rene van der Wal. The overall approach of COAT was also presented and On behalf of the COAT team discussed at the AMINOR workshops in Tromsø and at the Terrestrial Monitoring Expert Group (TMEG) of the Circumpolar Biodiversity Moni- toring Program (CBMP) in Denmark in Novem- ber 2011 Finally, two meetings have been held with members of reindeer herding districts on Varanger Peninsula in May and November 2011 and the mayors of the municipalities at the Va- Science plan for COAT 5 6 EXECUTIVE SUMMARY The arctic tundra comprises of the terrestrial eco- ment of “sister observatories” in arctic Russia. systems north of the continuous boreal forest The goal of COAT is to become the world’s most and is one of the earth’s largest terrestrial bi- comprehensive and management relevant long- omes. Owing to its remoteness, the arctic tundra term research and monitoring enterprise for arc- still harbors vast stretches of pristine wilderness tic terrestrial ecosystems. with intact ecosystem functions and endemic COAT aims to be a fully ecosystem-based system biodiversity of great fundamental and societal for long-term adaptive monitoring based on a significance. Yet the arctic tundra is predicted to food web approach. A food web approach in become more challenged by climate change than context of adaptive monitoring confers several any other terrestrial biome. Global circulation advantages. First, the food web concept is strong- models (GCMs) project an average temperature ly embedded in fundamental ecological theory. increase in the Arctic as large as 10 ºC by the This allows the formulation of conceptual climate turn of the century. Given such an extensive and impact prediction models for tractable modules rapid change, the impacts on the ecosystems will (compartments) of the food web which will act as be large and have pervasive implications locally a guide for defining adequate monitoring targets and globally. The rapid shift to new climate re- and state variables. Second, the comprehensive gimes is likely to give rise to new ecosystems with food web approach taken by COAT, with 7 mod- unknown properties, making science unable to ules and derived prediction models, accommo- accurately predict the associated outcomes and date the anticipated climate change impact on long-term consequences. The large internal un- tundra ecosystems. Anticipated impacts include certainties of the GCMs added to the limitations (1) “Arctic greening” due to encroachment of of ecological projection models, will hinder soci- forest and tall shrubs and its resultant feedback ety from responding to the changes by means of to the ecosystem and climate system, (2) disrupt- appropriate adaptive and mitigating actions. It ed dynamics and changed abundance levels of therefore becomes crucial to establish scientifi- arctic key-stone herbivores and the resultant cally robust observation systems to enable real trophic cascades likely to compromise main eco- time detection, documentation and understand- system functions and endemic arctic diversity, ing of climate impacts on arctic tundra ecosys- and (3) emergence of pest species outbreaks, zo- tems. In the light of this background it is para- onoses and invasive southern species and assess- doxical that our observing capacity of the arctic ment of the consequent impacts. Third, the tundra is very low. In context of the vastness of adopted food web approach of COAT should be the circumpolar biome and its large internal vari- sufficiently comprehensive to also accommodate ability there are very few sites devoted to long- early detection of unforeseen events (surprises) term research and monitoring and in particular that follow the development of new climates and which adopt an adequate ecosystem-based ap- ecosystems. COAT has a special focus on targets proach that accommodate the range of impacts that provide important provisioning and cultural and consequences that can be anticipated. ecosystem services locally (e.g. game), as well as In response to these concerns, the Fram Centre supporting services (e.g.
Recommended publications
  • Spitsbergen in Depth
    SPITSBERGEN IN DEPTH Big Island, Big Adventure Contents 1 Overview 2 Itinerary 4 Arrival and Departure Details 6 Your Ship 8 Included Activities 9 Adventure Options 10 Dates & Rates 11 Inclusions & Exclusions 13 Your Expedition Team 13 Extend Your Trip 14 Meals on Board 15 Possible Excursions 18 Packing Checklist Overview Spitsbergen in Depth: Big Island, Big Adventure This 14-day journey offers the most extensive exploration of Spitsbergen in the Norwegian archipelago of Svalbard, including the opportunity to witness iconic Arctic wildlife like walrus, reindeer and polar bears, a glimpse into 16th-century EXPEDITION IN BRIEF maritime culture at secluded landing sites, and the rare chance to appreciate breathtaking views at the birdwatching utopias 14th of July Glacier and Alkefjellet. Encounter iconic Arctic wildlife, such as polar bears, walrus and reindeer If conditions allow, we will also attempt a full circumnavigation of the Arctic during this memorable voyage, including a visit to the remote, uninhabited Arctic desert View numerous Arctic bird species, like puffins, Arctic terns and purple of Nordaustlandet. sandpipers The wildlife-viewing opportunities on this trip will leave you with plenty of Take advantage of continuous daylight memories—and photos: the walrus with its long tusks and distinctive whiskers; Explore glaciers, fjords, icebergs and Arctic birds in the thousands—in all their varied majesty; small herds of reindeer more with included Zodiac cruising loping across the tundra; and that most iconic of Arctic creatures, the polar bear, Immerse yourself in the icy realm especially as it prowls the edges of the pack ice on the perpetual hunt for food.
    [Show full text]
  • Our Arctic Nation a U.S
    Connecting the United States to the Arctic OUR ARCTIC NATION A U.S. Arctic Council Chairmanship Initiative Cover Photo: Cover Photo: Hosting Arctic Council meetings during the U.S. Chairmanship gave the United States an opportunity to share the beauty of America’s Arctic state, Alaska—including this glacier ice cave near Juneau—with thousands of international visitors. Photo: David Lienemann, www. davidlienemann.com OUR ARCTIC NATION Connecting the United States to the Arctic A U.S. Arctic Council Chairmanship Initiative TABLE OF CONTENTS 01 Alabama . .2 14 Illinois . 32 02 Alaska . .4 15 Indiana . 34 03 Arizona. 10 16 Iowa . 36 04 Arkansas . 12 17 Kansas . 38 05 California. 14 18 Kentucky . 40 06 Colorado . 16 19 Louisiana. 42 07 Connecticut. 18 20 Maine . 44 08 Delaware . 20 21 Maryland. 46 09 District of Columbia . 22 22 Massachusetts . 48 10 Florida . 24 23 Michigan . 50 11 Georgia. 26 24 Minnesota . 52 12 Hawai‘i. 28 25 Mississippi . 54 Glacier Bay National Park, Alaska. Photo: iStock.com 13 Idaho . 30 26 Missouri . 56 27 Montana . 58 40 Rhode Island . 84 28 Nebraska . 60 41 South Carolina . 86 29 Nevada. 62 42 South Dakota . 88 30 New Hampshire . 64 43 Tennessee . 90 31 New Jersey . 66 44 Texas. 92 32 New Mexico . 68 45 Utah . 94 33 New York . 70 46 Vermont . 96 34 North Carolina . 72 47 Virginia . 98 35 North Dakota . 74 48 Washington. .100 36 Ohio . 76 49 West Virginia . .102 37 Oklahoma . 78 50 Wisconsin . .104 38 Oregon. 80 51 Wyoming. .106 39 Pennsylvania . 82 WHAT DOES IT MEAN TO BE AN ARCTIC NATION? oday, the Arctic region commands the world’s attention as never before.
    [Show full text]
  • Bird Report for the Varanger Peninsula 7-13 March 2013
    Bird report for the Varanger Peninsula, Norway, 7-13 March 2013 Authors: Gitte Kruse Allan Kruse Aoi Bringsøe Henrik Bringsøe – DOF Køge (Danish Ornithological Society, Køge regional group) Photos: Henrik Bringsøe Introduction We had three main reasons for going to the Varanger Peninsula in the far north-east of Norway in March 2013. We wished to see the: King Eider Steller’s Eider Northern lights (or aurora borealis) The two ducks and several other species will winter at Varanger which is always ice-free because of the warm water moves of the Gulf Stream. The ice-free conditions attract ducks from Siberia and other north-eastern areas to spend the winter there. For our journey we chose a period of the very early phase of the new moon (7%). The moon was only visible at daytime which meant that the nights were as dark as possible. As it was close to the equinox, the days were not too short (sunrise at 5:50, sunset at 16:35). Other bird groups were also given high priority, i.e. gulls, eagles and tits. Had we made our journey in April it would not have been possible to see King Eider although there would be less snow in April and it would be easier to get around. Gitte and Allan were responsible for the overall travel plans as they had visited Varanger in June 2010 and gained valuable experience. They booked accommodation at Mr. Øyvind Artnzen in Vadsø in September 2012 and bought flight tickets to Kirkenes. For their homeward journey they chose the coastal service Hurtigruten from Kirkenes to Tromsø and then a flight to Copenhagen.
    [Show full text]
  • ARCTIC ECOLOGY Total Phosphorus, and Ions of Calcium, Increase in the Spatial Distribution of Lakes in Peril Chloride, Magnesium, and Sodium) Warmer Temperatures
    research highlights ARCTIC ECOLOGY total phosphorus, and ions of calcium, increase in the spatial distribution of Lakes in peril chloride, magnesium, and sodium) warmer temperatures. Glob. Change Biol. http://doi.org/xhk (2014) increased in shrinking lakes over the These findings highlight that extreme 25-year study period, but changed little in Northern Hemisphere anomalies are stable or expanding lakes. These changes the most variable on decadal timescales were most likely the result of shifts in the and could be used as indicators of global evaporation-to-inflow ratio and indicate temperature variability. BW that shrinking lakes may suffer from high- nutrient or saline conditions. AB ECONOMICS Climate-trade policy nexus TEMPERATURE TRENDS Appl. Econ. Persp. Pol. http://doi.org/xhg (2014) Warming hemispheres Geophys. Res. Lett. http://doi.org/xhh (2014) Surface temperature is typically reported as a global average when considering climate change. The use of a global average allows us to see the overall trend in temperature change, but results in the loss of important MINT IMAGES LIMITED / ALAMY MINT IMAGES spatial information. To investigate trends in warm and Reductions in lake area in some regions of cold temperature anomalies and their the Arctic and subarctic have occurred in spatial pattern, Scott Robeson of Indiana recent years. These changes raise concerns University, USA, and co-workers apply a about the fate of stored carbon and could spatial percentile approach to a gridded also have serious consequences for the temperature dataset on a monthly basis. health of the lake ecosystems themselves. Anomalies are calculated by comparison GEDULDIG / ALAMY BILDAGENTUR The mechanisms of lake reduction are with the 1961 to 1990 period and thought to relate primarily to increased analysis was performed individually on Climate change and international trade evaporation and decreased inflow, and lake both hemispheres.
    [Show full text]
  • Arctic Climate Impact Assessment
    PUBLISHED BY THE PRESS SYNDICATE OF THE UNIVERSITY OF CAMBRIDGE The Pitt Building, Trumpington Street, Cambridge, United Kingdom CAMBRIDGE UNIVERSITY PRESS The Edinburgh Building, Cambridge, CB2 2RU, UK AMAP Secretariat 40 West 20th Street, New York, NY 10011-4211, USA P.O. Box 8100 Dep. 10 Stamford Road, Oakleigh, VIC 3166, Australia N-0032 Oslo, Norway Ruiz de Alarcón 13, 28014 Madrid, Spain Tel: +47 23 24 16 30 Dock House, The Waterfront, Cape Town 8001, South Africa Fax: +47 22 67 67 06 http://www.amap.no http://www.cambridge.org First published 2004 CAFF International Printed in Canada Secretariat Hafnarstraeti 97 ISBN 0 521 61778 2 paperback 600 Akureyri, Iceland Tel: +354 461-3352 ©Arctic Climate Impact Assessment, 2004 Fax: +354 462-3390 http://www.caff.is Author Susan Joy Hassol IASC Secretariat Project Production and Graphic Design Middelthuns gate 29 Paul Grabhorn, Joshua Weybright, Clifford Grabhorn (Cartography) P.O. Box 5156 Majorstua N-0302 Oslo, Norway Photography Tel: +47 2295 9900 Bryan and Cherry Alexander, and others: credits on page 139 Fax: +47 2295 9901 Technical editing http://www.iasc.no Carolyn Symon Contributors Assessment Integration Team ACIA Secretariat Robert Corell, Chair American Meteorological Society, USA Gunter Weller, Executive Director Pål Prestrud, Vice Chair Centre for Climate Research in Oslo, Norway Patricia A. Anderson, Deputy Executive Director Gunter Weller University of Alaska Fairbanks, USA Barb Hameister, Sherry Lynch Patricia A. Anderson University of Alaska Fairbanks, USA International Arctic Research Center Snorri Baldursson Liaison for the Arctic Council, Iceland University of Alaska Fairbanks Elizabeth Bush Environment Canada, Canada Fairbanks, AK 99775-7740, USA Terry V.
    [Show full text]
  • The Concept of Cryo-Conditioning in Landscape Evolution
    Quaternary Research 75 (2011) 378–384 Contents lists available at ScienceDirect Quaternary Research journal homepage: www.elsevier.com/locate/yqres The concept of cryo-conditioning in landscape evolution Ivar Berthling a,⁎, Bernd Etzelmüller b a Department of Geography, Norwegian University of Science and Technology, Norway b Department of Geosciences, University of Oslo, Norway article info abstract Article history: Recent accounts suggest that periglacial processes are unimportant for large-scale landscape evolution and Received 15 December 2010 that true large-scale periglacial landscapes are rare or non-existent. The lack of a large-scale topographical Available online 17 January 2011 fingerprint due to periglacial processes may be considered of little relevance, as linear process–landscape development relationships rarely can be substantiated. Instead, periglacial landscapes may be classified in Keywords: terms of specific landform associations. We propose “cryo-conditioning”,defined as the interaction of cryotic Periglacial surface and subsurface thermal regimes and geomorphic processes, as an overarching concept linking landform Periglacial geomorphology Landscape and landscape evolution in cold regions. By focusing on the controls on processes, this concept circumvents Landscape evolution scaling problems in interpreting long-term landscape evolution derived from short-term processes. It also Cryo-conditioning contributes to an unambiguous conceptualization of periglacial geomorphology. We propose that the Scale development of several key elements in the Norwegian geomorphic landscape can be explained in terms of Cryo-geomorphology cryo-conditioning. © 2010 University of Washington. Published by Elsevier Inc. All rights reserved. Introduction individual landforms that make up the landscape are or must be of the same scale as the landscape itself.
    [Show full text]
  • Arctic Policy &
    Arctic Policy & Law References to Selected Documents Edited by Wolfgang E. Burhenne Prepared by Jennifer Kelleher and Aaron Laur Published by the International Council of Environmental Law – toward sustainable development – (ICEL) for the Arctic Task Force of the IUCN Commission on Environmental Law (IUCN-CEL) Arctic Policy & Law References to Selected Documents Edited by Wolfgang E. Burhenne Prepared by Jennifer Kelleher and Aaron Laur Published by The International Council of Environmental Law – toward sustainable development – (ICEL) for the Arctic Task Force of the IUCN Commission on Environmental Law The designation of geographical entities in this book, and the presentation of material, do not imply the expression of any opinion whatsoever on the part of ICEL or the Arctic Task Force of the IUCN Commission on Environmental Law concerning the legal status of any country, territory, or area, or of its authorities, or concerning the delimitation of its frontiers and boundaries. The views expressed in this publication do not necessarily reflect those of ICEL or the Arctic Task Force. The preparation of Arctic Policy & Law: References to Selected Documents was a project of ICEL with the support of the Elizabeth Haub Foundations (Germany, USA, Canada). Published by: International Council of Environmental Law (ICEL), Bonn, Germany Copyright: © 2011 International Council of Environmental Law (ICEL) Reproduction of this publication for educational or other non- commercial purposes is authorized without prior permission from the copyright holder provided the source is fully acknowledged. Reproduction for resale or other commercial purposes is prohibited without the prior written permission of the copyright holder. Citation: International Council of Environmental Law (ICEL) (2011).
    [Show full text]
  • Is Arctic Greening Consistent with the Ecology of Tundra? Lessons from an Ecologically Informed Mass Balance Model
    Environmental Research Letters LETTER • OPEN ACCESS Is arctic greening consistent with the ecology of tundra? Lessons from an ecologically informed mass balance model To cite this article: A V Rocha et al 2018 Environ. Res. Lett. 13 125007 View the article online for updates and enhancements. This content was downloaded from IP address 129.74.231.133 on 02/01/2019 at 15:50 Environ. Res. Lett. 13 (2018) 125007 https://doi.org/10.1088/1748-9326/aaeb50 LETTER Is arctic greening consistent with the ecology of tundra? Lessons OPEN ACCESS from an ecologically informed mass balance model RECEIVED 9 August 2018 A V Rocha1 , B Blakely1, Y Jiang2, K S Wright1 and S R Curasi1 REVISED 1 University of Notre Dame, Department of Biological Sciences & the Environmental Change Initiative, Notre Dame, IN, 46556, United 23 October 2018 States of America ACCEPTED FOR PUBLICATION 2 Oregon State University, Forest Ecosystems and Society, Corvallis, Oregon, 97331, United States of America 25 October 2018 PUBLISHED E-mail: [email protected] 7 December 2018 Keywords: NDVI, arctic greening/browning, disturbance, arctic ecology and biogeochemistry Original content from this work may be used under the terms of the Creative Abstract Commons Attribution 3.0 licence. Climate change has been implicated in the widespread ‘greening’ of the arctic in recent decades. Any further distribution of However, differences in arctic greening patterns among satellite platforms and recent reports of this work must maintain attribution to the decreased rate of greening or of browning have made attributing arctic greening trends to a warming author(s) and the title of climate challenging.
    [Show full text]
  • The Expert Mechanism on the Rights of Indigenous Peoples (EMRIP)
    The Expert Mechanism on the Rights of Indigenous Peoples (EMRIP) Your ref Our ref Date 18/2098-13 27 February 2019 The Expert Mechanism on the Rights of Indigenous Peoples (EMRIP) – Norway's contribution to the report focusing on recognition, reparation and reconciliation With reference to the letter of 20th November 2018 from the Office of the United Nations High Commissioner for Human Rights where we were invited to contribute to the report of the Expert Mechanism on recognition, reparation and reconciliation initiatives in the last 10 years. Development of the Norwegian Sami policy For centuries, the goal of Norwegian Sami policy was to assimilate the Sami into the Norwegian population. For instance Sami language was banned in schools. In 1997 the King, on behalf of the Norwegian Government, gave an official apology to the Sami people for the unjust treatment and assimilation policies. The Sami policy in Norway today is based on the recognition that the state of Norway was established on the territory of two peoples – the Norwegians and the Sami – and that both these peoples have the same right to develop their culture and language. Legislation and programmes have been established to strengthen Sami languages, culture, industries and society. As examples we will highlight the establishment of the Sámediggi (the Sami parliament in Norway) in 1989, the Procedures for Consultations between the State Authorities and Sámediggi of 11 May 2005 and the Sami Act. More information about these policies can be found in Norway's reports on the implementation of the ILO Convention No. 169 and relevant UN Conventions.
    [Show full text]
  • Climate Change Impacts in the Russian Arctic Download
    Climate Change Impacts in the Russian Arctic Searching for Ways for Adaptation Сompillation of basic recommendations prepared by WWF-Russia Moscow • 2009 Climate Change Impacts in the Russian Arctic, Searching for Ways for Adaptation. Сompillation of basic recommendations prepared by WWF-Russia. WWF-Russia, Moscow, 2009. - 64 pp. The study addresses climate change impacts on Russian Arctic. It formulates recommendations on ecosystem resilience, including: 1) enhanced system of protected areas; 2) conservation of unique biodiversity; and 3) monitoring and early warning systems, timely update of prognoses and planned measures. The study could be used for planning and subsequent implementation of resilience building and adaptation strategies and plans in Russian Arctic, including activities of wide range of stakeholders: officials, business, ecological organizations and public at national and local levels. Compiled by Dr. Olga Krever Editors: Dr. Victoria Elias, Dr. Alexey Kokorin Translated by: Vadim Vinichenko Design and Production: Alexander Filippov Photo on the cover: © Wim van Passel / WWF-Canon Circulation: 200 November 2009, WWF-Russia, Moscow, Russia Any reproduction in full or in part of this publication must mention WWF. Use of photographs from this publication is prohibited without written permission of WWF-Russia. © text 2009 WWF-Russia. All rights reserved. For free distribution Table of Contents Introduction 3 Chapter I. Observed climate changes 7 1. Surface air temperature 7 2. Precipitation 8 3. Snow cover 8 4. Permafrost 8 5. Sea ice in the Arctic basin 9 Chapter II. Projected climate changes 10 1. Climate models 10 2. Surface air temperature 12 3. Snow cover 12 4. Permafrost 12 5.
    [Show full text]
  • Diagenesis and Weathering of Quartzite at the Palaeic Surface on the Varanger Peninsula, Northern Norway
    NORWEGIAN JOURNAL OF GEOLOGY Diagenesis and weathering of quartzite at the Paleic surface 239 Diagenesis and weathering of quartzite at the palaeic surface on the Varanger Peninsula, northern Norway Jakob Fjellanger & Johan Petter Nystuen Fjellanger, J. & Nystuen, J. P. Weathering of quartzite at the palaeic surface on the Varanger Peninsula, northern Norway. Norwegian Journal of Geology, Vol. 87, pp. 133-145.Trondheim 2007. ISSN 029-196X. Weathered zones in quartzitic bedrock on the Hak alancˇearru Mountain on the Varanger Peninsula, northern Norway, have been examined, as has the timing of their development. The weathered zones are mainly associated with fractures formed by tectonic shear. SEM, microprobe and thin section studies reveal features belonging to the diagenesis and weathering history of the rock. Flakes of phyllosilicate minerals were originally depo- sited together with the quartz sand and became attached as coatings to the surface of individual quartz grains as well as forming an intergranular fill. Some of the detrital clay minerals turned into kaolinite during an early stage of the burial diagenesis. Kaolinite was later partly transformed to dickite. Quartz dissolution with concomitant quartz cementation and illite formation took place during later burial diagenesis. The kaolinite occurs in intergranular voids where it was partly transformed to pyrophyllite at a peak temperature of about 300 ˚C. As the overlying rocks were eroded the previously formed tectonic joints and small faults enhanced the circulation of ground water. This facilitated chemical weathering along joints and nearby grain contacts where slight dissolution of quartz significantly weakened inter-granular bonds. The resulting increase in permeability facilita- ted recent disintegration of the quartzite by mechanical processes.
    [Show full text]
  • LAG OG FORENINGER Pr 30.05.2017 Lag/Forening Leder
    LAG OG FORENINGER pr 30.05.2017 Lag/forening Leder Adresse Postnr. Telefonnr E-postadresse Idrettslag Austertana IL Sigmund Nerby Austertana 9845 Tana 9006 7334 [email protected] Båteng IL Ottar Wigelius Hillagurra 9845 Tana 9517 3882 [email protected] Deanu Searat v/Olaf Trosten Holmesund 9845 Tana 9427 6407 [email protected] IL Forsøk Vidar Johansen Luftjok 9845 Tana 94833978 [email protected] Levajok rideklubb Beate W. Søvsø Lyngbakken 5 9800 Vadsø 97965680 [email protected] Tana motorklubb Morten Blien 9845 Tana 9589 1092 [email protected] Sirbmá - Sirma IL Monica Balto Luohkka 56 9826 Sirma 41264148 [email protected] http://www.sirbma.no Tana ballklubb Anne Smeland Postboks 120 9845 Tana 47486768 [email protected] ostboks 120 Tana IF Benn Larsen Boftsa 9845 Tana 97598378 [email protected] Bryteklubben Tana Ulf Børre Hansen Diddigeaidnu 9845 Tana 97091002 [email protected] Tana Hestesportsklubb Mette Lillebostad 9845 Tana 91856350 [email protected] http://tanakjoreogrideklubb.blogspo t.no/ Tana skiskytterlag Otto Daniloff Lyngveien 13 9845 Tana 9174 6578 [email protected] Tana svømmeklubb Antti Lukkari Bjørkelia 9845 Tana 47901237 Tana idrettsråd Ole Henrik Somby 9845 Tana 41456161 [email protected] Tana fjellsportlag Andreas Valbekmo Luftjok 9845 Tana 9110 7358 [email protected] Tanafjord og omegn Arnt Pettersen Leirpollskogen 9845 Tana 98609449 [email protected] travlag Skytterlag Tana skytterlag Hans Ole Mudenia 9845 Tana 91783669 [email protected] Tana og Nesseby Roger Persson Bergeby 9840 [email protected] pistolklubb Varangerbotn Friluftsorg. Tana jeger og Yvonne 9845 Tana 91530790 http://www.njff.no/portal/page/port fiskeforening Johannessen al/finnmark/lokallag/tana [email protected] Deatnu/Tana Harald Persen Holmesund 9845 Tana 48138047 [email protected] elgjegerforening Barneorg.
    [Show full text]