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Results:

• 1. 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

• 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. 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

• 4. Public-Choice-2012---McGuiness-and-Walker---Foundations-of-the-Ostrom-workshop---institutional-analysis,-polycentricity,-and-self-governance-of-the-commons

  The well-being of any human community is critically dependent on continued access to natural and man-made resources. Decades before sustainability became a popular slogan, the Ostroms began to investigate the conditions under which natural resources can be man- aged in a sustainable manner. The origins of the Workshop approach can be traced back at least as far as “State Administration of Natural /media/loftslag/Public-Choice-2012---McGuiness-and-Walker---Foundations-of-the-Ostrom-workshop---institutional-analysis,-polycentricity,-and-self-governance-of-the-commons.pdf

• 5. ces-oslo2010_proceedings

  change over the North Atlantic and in some simulations also for Iceland. In all areas, including the North Atlantic and Iceland, a clear climate change signal compared to the spread between the simulations is seen. The standard deviation calculated from 17 of the simulations are less than 1°C in all areas apart from Iceland where it reaches between 1 and 2°C and in parts of the Barents Sea where /media/ces/ces-oslo2010_proceedings.pdf

• 6. BIGJ_windrose_2005-2014

  1 2 1 1 Wind rose BIGJ April 2005−2014 90 80 70 60 50 40 30 2010360350340 330 320 310 300 290 280 270 260 250 240 230 220 210 200 190 180 170 160 150 140 130 120 110 100 2 4 6 8 10 Frequency of wind direction (%) Aerodrome Total observations: 114 Calm: 0.88% Variable winds: 0% Average wind speed for wind direction Wind direction (°) Wind speed (knots ) 0 5 10 15 0 45 90 135 180 225 270 315 /media/vedur/BIGJ_windrose_2005-2014.pdf

• 7. Instructions on using wind, precipitation and temperature forecasts

  The colours represent 2°C temperature intervals. The temperature scale on the image changes according to the temperature range of the forecast. Wind forecasts: The map displays wind direction and wind speed (in m/s) based on 10-minute averages. Wind direction is denoted by arrows. The wind-speed scale on the image changes in relation to the forecast speed. The lowest wind /weather/articles/nr/1211

• 8. BIBD_windrose_2005-2014

  8 2 2 4 5 22 5 1 4 2 4 2 4 8 11 9 34 7 3 31 3 2 1 BIBD gusts exceeding 50 knots (2005−2014) 90 80 70 60 50 40 30 2010360350340 330 320 310 300 290 280 270 260 250 240 230 220 210 200 190 180 170 160 150 140 130 120 110 100 5 10 15 20 25 Frequency of wind direction (%) Aerodrome Total observations: 78 Calm: 0% Variable winds: 0% Average wind speed for wind direction Wind /media/vedur/BIBD_windrose_2005-2014.pdf

• 9. BIIS_windrose_2005-2014

  1 1 1 6 1 7 4 9 6 3 7 2 3 5 4 5 2 8 1 1 1 0 3 2 5 1 3 5 Wind rose BIIS August 2005−2014 90 80 70 60 50 40 30 2010360350340 330 320 310 300 290 280 270 260 250 240 230 220 210 200 190 180 170 160 150 140 130 120 110 100 2 4 6 8 10 12 14 Frequency of wind direction (%) Aerodrome Total observations: 3183 Calm: 14% Variable winds: 6.7% Average wind speed for wind /media/vedur/BIIS_windrose_2005-2014.pdf

• 10. Warning due to gale winds and heavy precipitation

  gusts around 30 m/s or more. The strongest wind is expected at the southwest coast and in the western part of the highlands. There, mean wind speed might be 18 to 23 m/s and gusts up to 40 m/s. Travellers are warned that tents and light trailers can become loose in these conditions. Travellers near the coast are also advised to be aware of high tide on Saturday evening. After midnight, winds /about-imo/news/nr/2501