Monitoring Ocean Acidification in Norwegian Seas in 2017

Total Page:16

File Type:pdf, Size:1020Kb

Monitoring Ocean Acidification in Norwegian Seas in 2017 Monitoring Report M-1072 | 2018 Monitoring ocean acidification in Norwegian seas in 2017 MADE BY: Institute of Marine Research, Uni Research, Norwegian Institute for Water Research COLOPHON Executive institutions (the institutions are responsible for the content in the report) Institute of Marine Research, Uni Research, Norwegian Institute for Water Research Project manager for the contractor Contact person in the Norwegian Environment Agency Melissa Chierici Gunnar Skotte M-number Year Pages Contract number M-1072 2018 106 17078007 Publisher The project is funded by Norwegian Environment Agency Norwegian Environment Agency Author(s) Jones, E., M. Chierici, I. Skjelvan, M. Norli, K.Y. Børsheim, H.H. Lødemel, T. Kutti, K. Sørensen, A.L. King, K. Jackson, T. de Lange Title – English and Norwegian Monitoring ocean acidification in Norwegian seas in 2017/ Havforsuringsovervåking i norske farvann i 2017 Summary – Sammendrag This is the annual report from 2017 based on the program: ‘Monitoring ocean acidification in Norwegian waters’ funded by the Norwegian Environment Agency. The measurements are performed by the Institute of Marine Research (IMR), Norwegian Institute for Water Research (NIVA), and Uni Research (UNI), and the measurements cover the area from Skagerrak/North Sea in the south, through the Norwegian Sea, and the seasonally sea-ice covered northern Barents Sea. IMR conducted water column measurements along repeated transects, mainly during winter in the North Sea (Torungen–Hirtshals section), in the Norwegian Sea (Svinøy-NW and Gimsøy-NW sections), in the Barents Sea (Fugløya-Bjørnøya section and stations in the NE Barents Sea), and at Skrova and Arendal coastal stations. UNI conducted water column measurements at Station M, continuous surface measurements at the same site, and water column measurements at two coastal stations in Hardanger. NIVA performed surface water measurements on two sections; Oslo-Kiel (North Sea/Skagerrak) and Tromsø-Longyearbyen (Barents Sea opening) during all of 2017. This report shows and discusses some time series and trends for the period 2011-2017. Denne rapporten gjelder undersøkelser av havforsuring i 2017 utført av Havforskningsinstituttet (IMR), Norsk institutt for vannforskning (NIVA) og Uni Research (UNI) på oppdrag fra Miljødirektoratet. Måleområdet i rapporten går fra Skagerrak/Nordsjøen, gjennom hele Norskehavet og til nordlige deler av Barentshavet. IMR har gjort vannsøylemålinger, i hovedsak vinterstid, langs faste snitt i Nordsjøen (Torungen–Hirtshals), Norskehavet (Svinøy- NV og Gimsøy-NV), i Barentshavet (Fugløya-Bjørnøya og stasjoner i det nordøstlige Barentshavet), og ved Arendal og Skrova kyststasjon. UNI har gjort vannsøylemålinger gjennom store deler av året på Stasjon M i Norskehavet, kontinuerlige overflatemålinger på Stasjon M, og vannsøylemålinger på to kyststasjoner i Hardanger. NIVA har gjort overflatemålinger store deler av året på strekningen Oslo-Kiel og Tromsø-Longyearbyen. I denne rapporten presenteres og diskuteres tidsserier fra perioden 2011-2017. 4 Keywords 4 Emneord Carbonate system, interannual and seasonal Karbonmålinger, mellomårlig-og sesongs- variability, biogeochemical processes variasjon, biogeokjemiske prosesser Cover photo Photo: Kim Abel Tromsø, mai 2018 Authors: Elizabeth Jones*, Melissa Chierici*, Ingunn Skjelvan**, Marit Norli***, Knut Yngve Børsheim*, Helene Hodal Lødemel*, Tina Kutti*, Kai Sørensen***, Andrew Luke King***, Kristin. Jackson**, Tor de Lange** *Havforskningsinstituttet (IMR), **Uni Research (UNI), ***Norsk institutt for vannforskning (NIVA) This report should be cited: Jones, E., Chierici, M., I. Skjelvan, M. Norli, K.Y. Børsheim, H.H. Lødemel, T. Kutti, K. Sørensen, A.L. King, K. Jackson og T. de Lange. 2018. Monitoring of ocean acidification in Norwegian seas in 2017, Rapport, Miljødirektoratet, M-XXX|2018 Monitoring ocean acidification in Norwegian seas in 2017 | M-1072|2018 Content Content .......................................................................................................... 4 Summary ..................................................................................................... 5 Extended Norwegian Summary ........................................................................... 8 1. Introduction ............................................................................................... 11 2. Methods and Data......................................................................................... 13 2.1 Sampling and Variables ............................................................................ 16 2.2 Measurements of Total Alkalinity and Total Inorganic Carbon ............................. 17 2.3 pH Measurements................................................................................... 17 2.4 pCO2 Measurements ................................................................................ 18 2.5 Calculation of pH and Saturation State of Calcite and Aragonite ......................... 18 3. Results ...................................................................................................... 19 3.1 North Sea and Skagerrak .......................................................................... 19 3.1.1 Spatial variability along Torungen-Hirtshals section ................................. 19 3.1.2 Seasonal variability at Arendal station ................................................. 22 3.1.3 Seasonal variability in surface water ................................................... 24 3.1.4 Trend analysis at selected stations ..................................................... 28 3.2 Norwegian Sea ...................................................................................... 31 3.2.1 Spatial variability along the Svinøy-NW section ...................................... 31 3.2.2 Spatial variability along the Gimsøy-NW section ..................................... 34 3.2.3 Seasonal variability in open ocean ...................................................... 36 3.2.4 Seasonal variability in coastal water .................................................... 41 3.2.5 Trend analysis at selected stations ..................................................... 45 3.3 Barents Sea .......................................................................................... 52 3.3.1 Spatial variability along the Fugløya-Bjørnøya section .............................. 52 3.3.2 Spatial variability along the northeastern Barents Sea section .................... 55 3.3.3 Seasonal variability in surface water ................................................... 56 3.3.4 Trend analysis at selected stations ..................................................... 60 3.4 Norwegian Coast .................................................................................... 66 3.5 Cold Water Coral Reefs ............................................................................ 67 4. Summary and Recommendations ...................................................................... 69 5. References ................................................................................................. 71 6. Attachments ............................................................................................... 74 6.1 Plots .................................................................................................. 74 6.2 Data Tables .......................................................................................... 81 6.3 Definitions .......................................................................................... 104 4 Monitoring ocean acidification in Norwegian seas in 2017 | M-1072|2018 Summary This is the annual report from 2017 based on the program: ‘Monitoring ocean acidification in Norwegian waters’, which began in 2013 and is funded by the Norwegian Environment Agency. The report is based on measurements of AT, CT, pCO2 and pH made by the Institute of Marine Research (IMR), Norwegian Institute for Water Research (NIVA) and Uni Research (UNI) with updated data from 2017. IMR conducted water column measurements along repeated transects during winter and spring 2017 in the North Sea (Torungen–Hirtshals), at two sections in the Norwegian Sea (Svinøy-NW and Gimsøy-NW), and at two sections in the Barents Sea (Fugløya-Bjørnøya in February and April 2017, and in the northeastern Barents Sea in September 2017). The Norwegian Sea water column was also investigated by UNI which performed seasonal studies at Station M. Moreover, UNI also contributed with continuous surface pCO2 data at Station M. NIVA performed seasonal cruises (winter, spring, summer and autumn) for surface water measurements on two sections; Oslo-Kiel (North Sea) and Tromsø- Longyearbyen (Barents Sea opening) during 2017, and present data on both seasonal and interannual basis. In addition, the report includes data from monthly measurements at a coastal site in Skrova in Lofoten and Arendal in Skagerrak (IMR) and from two coastal sites in Hardanger (UNI). All sampling positions are shown in Figure 1. This report includes carbonate chemistry data and ancillary variables such as salinity, temperature, and inorganic nutrient concentrations to provide baseline observations of variability attributed to oceanographic and anthropogenic processes such as the influence of mixing of water masses, freshwater/meltwater inputs, CO2 emissions and oceanic uptake, and biological processes including production and respiration. For water column data, this is measured each year and the observed seasonal and interannual
Recommended publications
  • 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.
    [Show full text]
  • A Persistent Norwegian Atlantic Current Through the Pleistocene Glacials
    A persistent Norwegian Atlantic Current through the Pleistocene glacials Newton, A. M. W., Huuse, M., & Brocklehurst, S. H. (2018). A persistent Norwegian Atlantic Current through the Pleistocene glacials. Geophysical Research Letters. https://doi.org/10.1029/2018GL077819 Published in: Geophysical Research Letters Document Version: Publisher's PDF, also known as Version of record Queen's University Belfast - Research Portal: Link to publication record in Queen's University Belfast Research Portal Publisher rights Copyright 2018 the authors. This is an open access article published under a Creative Commons Attribution License (https://creativecommons.org/licenses/by/4.0/), which permits unrestricted use, distribution and reproduction in any medium, provided the author and source are cited. General rights Copyright for the publications made accessible via the Queen's University Belfast Research Portal is retained by the author(s) and / or other copyright owners and it is a condition of accessing these publications that users recognise and abide by the legal requirements associated with these rights. Take down policy The Research Portal is Queen's institutional repository that provides access to Queen's research output. Every effort has been made to ensure that content in the Research Portal does not infringe any person's rights, or applicable UK laws. If you discover content in the Research Portal that you believe breaches copyright or violates any law, please contact [email protected]. Download date:01. Oct. 2021 Geophysical Research Letters RESEARCH LETTER A Persistent Norwegian Atlantic Current Through 10.1029/2018GL077819 the Pleistocene Glacials Key Points: A. M. W. Newton1,2,3 , M. Huuse1,2 , and S.
    [Show full text]
  • The Place of the Oceans in Norway's Foreign and Development Policy
    Norwegian Ministry of Foreign Affairs Published by: Meld. St. 22 (2016–2017) Report to the Storting (white paper) Norwegian Ministry of Foreign Affairs Public institutions may order additional copies from: Norwegian Government Security and Service Organisation The place of the oceans E-mail: [email protected] Internet: www.publikasjoner.dep.no KET T ER RY Telephone: + 47 222 40 000 M K Ø K J E L R in Norway's foreign and I I Photo: Peter Prokosch / Grid Arendal M 0 Print: 07 PrintMedia AS 7 9 7 P 3 R 0 I 1 N 4 08/2017 – Impression 500 TM 0 EDIA – 2 development policy 2016–2017 Meld. St. 22 (2016–2017) Report to the Storting (white paper) 1 The place of the oceans in Norway’s foreign and development policy Meld. St. 22 (2016–2017) Report to the Storting (white paper) The place of the oceans in Norway’s foreign and development policy Translation from Norwegian. For information only. Contents 1 Introduction................................... 5 Part III Priority areas for Norway ......... 41 2 Summary ....................................... 8 5 Sustainable use and value creation ......................................... 43 Part I Ocean interests ............................ 13 5.1 Oil and gas sector .......................... 43 5.1.1 International cooperation in the 3 Norwegian ocean interests in oil and gas sector ........................... 44 an international context ............ 15 5.2 Maritime industry .......................... 45 3.1 The potential of the oceans ........... 15 5.2.1 International cooperation in 3.2 Forces shaping international shipping .......................................... 45 ocean policy .................................... 16 5.2.2 Shipping in the north ..................... 47 3.3 Need for knowledge ....................... 17 5.3 Seafood industry ...........................
    [Show full text]
  • Chapter 7 Arctic Oceanography; the Path of North Atlantic Deep Water
    Chapter 7 Arctic oceanography; the path of North Atlantic Deep Water The importance of the Southern Ocean for the formation of the water masses of the world ocean poses the question whether similar conditions are found in the Arctic. We therefore postpone the discussion of the temperate and tropical oceans again and have a look at the oceanography of the Arctic Seas. It does not take much to realize that the impact of the Arctic region on the circulation and water masses of the World Ocean differs substantially from that of the Southern Ocean. The major reason is found in the topography. The Arctic Seas belong to a class of ocean basins known as mediterranean seas (Dietrich et al., 1980). A mediterranean sea is defined as a part of the world ocean which has only limited communication with the major ocean basins (these being the Pacific, Atlantic, and Indian Oceans) and where the circulation is dominated by thermohaline forcing. What this means is that, in contrast to the dynamics of the major ocean basins where most currents are driven by the wind and modified by thermohaline effects, currents in mediterranean seas are driven by temperature and salinity differences (the salinity effect usually dominates) and modified by wind action. The reason for the dominance of thermohaline forcing is the topography: Mediterranean Seas are separated from the major ocean basins by sills, which limit the exchange of deeper waters. Fig. 7.1. Schematic illustration of the circulation in mediterranean seas; (a) with negative precipitation - evaporation balance, (b) with positive precipitation - evaporation balance.
    [Show full text]
  • MARITIME ACTIVITY in the HIGH NORTH – CURRENT and ESTIMATED LEVEL up to 2025 MARPART Project Report 1
    MARITIME ACTIVITY IN THE HIGH NORTH – CURRENT AND ESTIMATED LEVEL UP TO 2025 MARPART Project Report 1 Authors: Odd Jarl Borch, Natalia Andreassen, Nataly Marchenko, Valur Ingimundarson, Halla Gunnarsdóttir, Iurii Iudin, Sergey Petrov, Uffe Jacobsen and Birita í Dali List of authors Odd Jarl Borch Project Leader, Nord University, Norway Natalia Andreassen Nord University, Norway Nataly Marchenko The University Centre in Svalbard, Norway Valur Ingimundarson University of Iceland Halla Gunnarsdóttir University of Iceland Iurii Iudin Murmansk State Technical University, Russia Sergey Petrov Murmansk State Technical University, Russia Uffe Jakobsen University of Copenhagen, Denmark Birita í Dali University of Greenland 1 Partners MARPART Work Package 1 “Maritime Activity and Risk” 2 THE MARPART RESEARCH CONSORTIUM The management, organization and governance of cross-border collaboration within maritime safety and security operations in the High North The key purpose of this research consortium is to assess the risk of the increased maritime activity in the High North and the challenges this increase may represent for the preparedness institutions in this region. We focus on cross-institutional and cross-country partnerships between preparedness institutions and companies. We elaborate on the operational crisis management of joint emergency operations including several parts of the preparedness system and resources from several countries. The project goals are: • To increase understanding of the future demands for preparedness systems in the High North including both search and rescue, oil spill recovery, fire fighting and salvage, as well as capacities fighting terror or other forms of destructive action. • To study partnerships and coordination challenges related to cross-border, multi-task emergency cooperation • To contribute with organizational tools for crisis management Project characteristics: Financial support: -Norwegian Ministry of Foreign Affairs, -the Nordland county Administration -University partners.
    [Show full text]
  • Cop13 Inf. 66 (English Only / Únicamente En Inglés / Seulement En Anglais)
    CoP13 Inf. 66 (English only / únicamente en inglés / seulement en anglais) Written Statement by Japan on the naming of Sea of Japan In response to the written statement distributed by the RoK Delegation, Japan would like to present the pamphlet and related information on the appellation of the Sea of Japan, which show that the Sea of Japan is the standard appellation of the regional sea, and that all the UN publications shall exclusively use this specific appellation. Naming of the Sea of Japan The purpose of the United Nations Group of Experts on Geographical Names (UNGEGN) is to consider the technical problems of standardization of geographical names with a view to furthering it at both the national and international levels thereby preventing confusion in the use of names of geographical features. The delegation of Japan therefore believes that as a matter of principle it is not appropriate to discuss the issue of the naming of any particular geographical feature such as the Sea of Japan at this meeting. The views of the Government of Japan on this matter were clearly expressed at the previous sessions of the UNGEGN and the United Nations Conference on the Standardization of Geographical Names (UNCSGN), including its last session in Berlin in 2002, and have been duly recorded. It should be reiterated here that the name “Sea of Japan” is geographically and historically established and is used at present all over the world, except the ROK and the DPRK that claim the name should be replaced or at least co-named the “East Sea.” The following are the major points Japan wishes to make in response to these unfounded and politically motivated assertions.
    [Show full text]
  • Arctic Report Card 2017
    Arctic Report Card 2017 Arctic Report Card 2017 Arctic shows no sign of returning to reliably frozen region of recent past decades 2017 Headlines 2017 Headlines Video Executive Summary Contacts Arctic shows no sign of returning to reliably frozen Vital Signs region of recent past decades Surface Air Temperature Despite relatively cool summer temperatures, Terrestrial Snow Cover observations in 2017 continue to indicate that the Greenland Ice Sheet Arctic environmental system has reached a 'new Sea Ice normal', characterized by long-term losses in the Sea Surface Temperature extent and thickness of the sea ice cover, the extent Arctic Ocean Primary Productivity and duration of the winter snow cover and the mass of ice in the Greenland Ice Sheet and Arctic glaciers, Tundra Greenness and warming sea surface and permafrost Other Indicators temperatures. Terrestrial Permafrost Groundfish Fisheries in the Highlights Eastern Bering Sea Wildland Fire in High Latitudes • The average surface air temperature for the year ending September 2017 is the 2nd warmest since 1900; however, cooler spring and summer temperatures contributed to a rebound in snow cover in the Eurasian Arctic, slower summer sea ice loss, Frostbites and below-average melt extent for the Greenland ice sheet. Paleoceanographic Perspectives • The sea ice cover continues to be relatively young and thin with older, thicker ice comprising only 21% of the ice cover in on Arctic Ocean Change 2017 compared to 45% in 1985. Collecting Environmental • In August 2017, sea surface temperatures in the Barents and Chukchi seas were up to 4° C warmer than average, Intelligence in the New Arctic contributing to a delay in the autumn freeze-up in these regions.
    [Show full text]
  • Norway in Respect of Areas in the Arctic Ocean, the Barents Sea and the Norwegian Sea Executive Summary
    Continental Shelf Submission of Norway in respect of areas in the Arctic Ocean, the Barents Sea and the Norwegian Sea Executive Summary 50˚00’ 85˚00’ 45˚00’ 40˚00’ 35˚00’ Continental shelf 30˚00’ 30˚00’ 200 nautical mile limit of Norway beyond 200 nautical 85˚00’ 25˚00’ 25˚00’ 20˚00’ 20˚00’ miles 15˚00’ 15˚00’ 200 nautical mile limits of other states 10˚00’5˚00’ 0˚00’ 5˚00’10˚00’ Bilateral maritime boundaries between Water depth Norway and other states 0 meter Computed median line between 500 meter Norway and the Russian Federation 1000 meter Western 80˚00’ Nansen Basin Preliminary line connecting continental 1500 meter shelf outer limit points of Norway and the Russian Federation 2000 meter Outer limit of the continental shelf 2500 meter beyond 200 nautical miles 3000 meter 2500 meter isobath 3500 meter 80˚00’ Yermak BARENTS Land boundaries between states 4000 meter Plateau Boundary between 200 nautical mile 4500 meter SEA 75˚00’ zones of Mainland Norway and around Svalbard 5000 meter 5500 meter Land Svalbard Continental shelf outer limit points Norwegian territory 60 nautical mile distance criterion Sediment thickness criterion Land, undifferentiated Knipovich Ridge Loop Greenland Hole Point of the Russian Federation 75˚00’ 70˚00’ GREENLAND SEA Bjørnøya 65˚00’ 70˚00’ Mohns Ridge Jan Mayen 60˚00’ NORWEGIAN 50˚00’ Lofoten Jan Mayen Fracture Zone SEA Basin Iceland SEAVøring Spur Jan Mayen Micro Continent Banana Hole Plateau Banana Hole 65˚00’ 45˚00’ Vøring Russian Federation Norway Plateau Basin 40˚00’ Iceland Finland 35˚00’ 60˚00’ 30˚00’
    [Show full text]
  • Grade 6 Social Studies
    Grade 6 SEPTEMBER OCTOBER NOVEMBER 5 Themes of Geography – Europe Europe st (1 week or 2) E.1 E.1 A. absolute and relative On a map of the world, locate On a map of the world, locate locations, B. climate, C. the continent of Europe. On a the continent of Europe. On a major physical characteristics, map of Europe, locate the map of Europe, locate the D. major natural resources, Atlantic Ocean, Arctic Ocean, Atlantic Ocean, Arctic Ocean, E. population size Norwegian Sea, and Barents Norwegian Sea, and Barents Sea. Locate the Volga, Sea. Locate the Volga, Europe Danube, Ural, Rhine, Elbe, Danube, Ural, Rhine, Elbe, E.1 Seine, Po, and Thames Seine, Po, and Thames On a map of the world, locate Rivers. Locate the Alps, Rivers. Locate the Alps, the continent of Europe. On a Pyrenees, and Balkan Pyrenees, and Balkan map of Europe, locate the Mountains. Locate the Mountains. Locate the Atlantic Ocean, Arctic Ocean, countries in the northern, countries in the northern, Norwegian Sea, and Barents southern, central, eastern, and southern, central, eastern, and Sea. Locate the Volga, western regions of Europe. western regions of Europe. Danube, Ural, Rhine, Elbe, E.2 E.2 Seine, Po, and Thames Use a map key to locate Use a map key to locate Rivers. Locate the Alps, countries and major cities in countries and major cities in Pyrenees, and Balkan Europe. (G) Europe. (G) Mountains. Locate the E.3 E.3 countries in the northern, Explain how the following five Explain how the following five southern, central, eastern, and factors have influenced factors have influenced western regions of Europe.
    [Show full text]
  • SESSION I : Geographical Names and Sea Names
    The 14th International Seminar on Sea Names Geography, Sea Names, and Undersea Feature Names Types of the International Standardization of Sea Names: Some Clues for the Name East Sea* Sungjae Choo (Associate Professor, Department of Geography, Kyung-Hee University Seoul 130-701, KOREA E-mail: [email protected]) Abstract : This study aims to categorize and analyze internationally standardized sea names based on their origins. Especially noting the cases of sea names using country names and dual naming of seas, it draws some implications for complementing logics for the name East Sea. Of the 110 names for 98 bodies of water listed in the book titled Limits of Oceans and Seas, the most prevalent cases are named after adjacent geographical features; followed by commemorative names after persons, directions, and characteristics of seas. These international practices of naming seas are contrary to Japan's argument for the principle of using the name of archipelago or peninsula. There are several cases of using a single name of country in naming a sea bordering more than two countries, with no serious disputes. This implies that a specific focus should be given to peculiar situation that the name East Sea contains, rather than the negative side of using single country name. In order to strengthen the logic for justifying dual naming, it is suggested, an appropriate reference should be made to the three newly adopted cases of dual names, in the respects of the history of the surrounding region and the names, people's perception, power structure of the relevant countries, and the process of the standardization of dual names.
    [Show full text]
  • Maintaining Arctic Cooperation with Russia Planning for Regional Change in the Far North
    Maintaining Arctic Cooperation with Russia Planning for Regional Change in the Far North Stephanie Pezard, Abbie Tingstad, Kristin Van Abel, Scott Stephenson C O R P O R A T I O N For more information on this publication, visit www.rand.org/t/RR1731 Library of Congress Cataloging-in-Publication Data is available for this publication. ISBN: 978-0-8330-9745-3 Published by the RAND Corporation, Santa Monica, Calif. © Copyright 2017 RAND Corporation R® is a registered trademark. Cover: NASA/Operation Ice Bridge. Limited Print and Electronic Distribution Rights This document and trademark(s) contained herein are protected by law. This representation of RAND intellectual property is provided for noncommercial use only. Unauthorized posting of this publication online is prohibited. Permission is given to duplicate this document for personal use only, as long as it is unaltered and complete. Permission is required from RAND to reproduce, or reuse in another form, any of its research documents for commercial use. For information on reprint and linking permissions, please visit www.rand.org/pubs/permissions. The RAND Corporation is a research organization that develops solutions to public policy challenges to help make communities throughout the world safer and more secure, healthier and more prosperous. RAND is nonprofit, nonpartisan, and committed to the public interest. RAND’s publications do not necessarily reflect the opinions of its research clients and sponsors. Support RAND Make a tax-deductible charitable contribution at www.rand.org/giving/contribute www.rand.org Preface Despite a period of generally heightened tensions between Russia and the West, cooperation on Arctic affairs—particularly through the Arctic Council—has remained largely intact, with the exception of direct mil- itary-to-military cooperation in the region.
    [Show full text]
  • Carbon and Oxygen Fluxes in the Barents and Norwegian Seas
    Carbon and oxygen fluxes in the Barents and Norwegian Seas: Production, air-sea exchange and budget calculations Caroline Kivimäe Dissertation for the degree philosophiae doctor (PhD) at the University of Bergen August 2007 ISBN 978-82-308-0414-8 Bergen, Norway 2007 Printed by Allkopi Ph: +47 55 54 49 40 ii Abstract This thesis focus on the carbon and oxygen fluxes in the Barents and Norwegian Seas and presents four studies where the main topics are variability of biological production, air-sea exchange and budget calculations. The world ocean is the largest short term reservoir of carbon on Earth, consequently it has the potential to control the atmospheric concentrations of carbon dioxide (CO2) and has already taken up ~50 % of the antropogenically emitted CO2. It is thus important to study carbon related processes in the ocean to understand their changes in the past, present, and future perspectives. The main function of the Arctic Mediterranean, within which the study area lies, in the global carbon cycle is to take up CO2 from the atmosphere and, as part of the northern limb of the global thermohaline circulation, to convey surface water to the ocean interior. A carbon budget is constructed for the Barents Sea to study the carbon fluxes into and out of the area. The budget includes advection, air-sea exchange, river runoff, land sources and sedimentation. The results reviel that ~5.6 Gt C annually is exchanged through the boundaries of the Barents Sea mainly due to advection, and that the carbon sources within the Barents Sea itself are larger than the sinks.
    [Show full text]