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Results:

• 1. programme2---PhD-Workshop-preceding-Adaptation-Research-Conference

  During the conference all of you are requested to act as rapporteur in two or three sessions. A preliminary allocation of rapporteur sessions has been made (see below), while accounting for your expertise in certain areas. Participants can suggest changes in the rapporteur session allocation, on the condition a convincing argumentation is provided as well as a confirmed alternative rapporteur /media/loftslag/programme2---PhD-Workshop-preceding-Adaptation-Research-Conference.pdf

• 2. Bárðarbunga earthquakes - interactive model

  (central mouse scroll), pan (right click), turn over (left click) choose speed 1x, 2x, 10x (available in some browsers (e.g. Chrome but not Firefox) coloured patches on/off (ring icon) choose landscape map (mountain icon) or satellite image (bell icon) for the surface Tryggvi Hjörvar, specialist at the Icelandic Met Office, created this model. An easier presentation - demo In a video /earthquakes-and-volcanism/articles/nr/2971

• 3. Bárðarbunga earthquakes - interactive model

  (central mouse scroll), pan (right click), turn over (left click) choose speed 1x, 2x, 10x (available in some browsers (e.g. Chrome but not Firefox) coloured patches on/off (ring icon) choose landscape map (mountain icon) or satellite image (bell icon) for the surface Tryggvi Hjörvar, specialist at the Icelandic Met Office, created this model. An easier presentation - demo In a video /earthquakes-and-volcanism/articles/nr/2971/

• 4. Kok_and_Veldkamp_editorial_ES-2011-4160

  agreement on use of terminology. Third, all scoping papers stress that there is no silver bullet solution, with a different view on both scale and governance being appropriate depending on the specific case. Buizer et al. (2011) are strongest on this view by presenting and discussing a framework. Termeer et al. (2010) confirm that there is no best governance approach, drawing an analogue /media/loftslag/Kok_and_Veldkamp_editorial_ES-2011-4160.pdf

• 5. Daniell_etal-2010

  and evaluating impacts (see also Swallow et al. 2001, van Ast and Boot 2003). METHODS AND DATA This article is based on empirical data that originated from the analysis of the participatory exercise in the Dhuenn basin. The strong involvement of researchers from two research projects (NeWater[1] and ACER[2]) linked by a joint case study led to the variety of sources available for exploration, including /media/loftslag/Daniell_etal-2010.pdf

• 6. Pollution

  closer to Reykjavík, eight years before that. As elsewhere in Europe sulphur concentration is lower now than when measurements began. Average value of sulphur is about 0.5 mg/l in precipitation, about 0.1 μg/m3 in aerosol and about 0.07 μg/m3 in air. Stórhöfði - a seashore background station Stórhöfði is at the south end of island Heimaey which is the largest of the Westman islands /pollution-and-radiation/pollution/

• 7. Early work and an overview of measurements

  Reykjavík, 209 s. Ogilvie, A. E. J. 1991. Climatic changes in Iceland A. D. c. 865 to 1598. Í: The Norse of the North Atlantic (Presented by G. F. Bigelow). Acta Archaeologica 61(1990), 233-251. Ogilvie, A. E. J. 1992. Documentary evidence for changes in the climate of Iceland, A. D. 1500 to 1800. Í R.S. Bradley and P. D. Jones. Climate Since A.D. 1500. Routledge. London and New York, 92-117 /climatology/articles/nr/1138

• 8. Early work and an overview of measurements

  Reykjavík, 209 s. Ogilvie, A. E. J. 1991. Climatic changes in Iceland A. D. c. 865 to 1598. Í: The Norse of the North Atlantic (Presented by G. F. Bigelow). Acta Archaeologica 61(1990), 233-251. Ogilvie, A. E. J. 1992. Documentary evidence for changes in the climate of Iceland, A. D. 1500 to 1800. Í R.S. Bradley and P. D. Jones. Climate Since A.D. 1500. Routledge. London and New York, 92-117 /climatology/articles/nr/1138/

• 9. IMO at the Arctic Circle Assembly 2017

  the USA, the European Space Agency (ESA) and China.Ingvar Kristinsson, managing director at IMO, participated in a session on the potential effects of volcanic ash clouds from Icelandic volcanoes on aviation in the Arctic airspace. In a special session on issues related to Arctic Freshwater, Halldór Björnsson and Þorsteinn Þorsteinsson contributed to a discussion on freshwater fluxes /about-imo/news/imo-at-the-arctic-circle-assembly-2017

• 10. The segmented dyke intrusion explained

  to time of occurrence and the colour code is shown at the top of the map. The earthquake locations delineate the track of the dyke intrusion from Bárðarbunga volcano to the eruption site at Holuhraun. Vertical cross sections through the crust are also shown; looking from the south (below) and east (to the right). Triangles mark the locations of seismic stations in and around the glacier. Data /about-imo/news/nr/3038