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Results:

• 11. Eriksson_1-Risk-perception

  with the effects of climate change • Climate change as an environmental stressor – discrete (cataclysmic events) or continuous • Stressors lead to: 1. Threat appraisals (evaluating threat and put in relation to resources) 2. Coping appraisals (evaluations of coping strategies considering for example self-efficacy and response efficacy) 3. Different cognitive, emotional and behavioural /media/loftslag/Eriksson_1-Risk-perception.pdf

• 12. Flood in Grímsvötn

  of earthquakes in the days preceding the eruption. No such earthquakes have been measured now. The last eruption in Grímsvötn was in 2011. There was a flood 6 months prior to that eruption. Since 2011 there have been 6 floods without an eruption in the aftermath. Recent eruptions in Grímsvötn have happened every 5-10 years and, considering measurements and observations, scientists agree /about-imo/news/icesheet-in-grimsvotn-subsiding

• 13. Re-evaluation needed of the size of the hazard area

  the chemical composition of magma/gas, or possibly changes in the volcanic conduit cannot be ruled out. Considering these changes in activity, the size of the hazard area at the eruption site is being re-evaluated. Updated 21.04. at 16:00With the Fagradalsfjall eruption continuing for over a month, it is natural to ask how long the eruption will last. New fissure openings have formed several times /about-imo/news/new-fissure-near-the-eruption-site-in-geldingadalir

• 14. The weather in Iceland in 2016

  very favourable month in the South and West, but wet and gloomy in the Northeast. There was excessive precipitation in places in the East, but below average in the West. AugustThis was a warm and favourable month in most areas, rather dry and warm. SeptemberIt was very wet in the North and East, but in other areas the weather was favourable. The winds were unusually light considering /about-imo/news/the-weather-in-iceland-in-2016

• 15. The weather in Iceland 2008

  with precipitation,considering the whole year, was close to average. There was slightly more snowfall than has typical since 2000, but it barely reached the average falls of the preceding decades. There were 64 days with snow-cover in Reykjavík, nine days more than the average 1961-1990, but just below the average for 1971-2000. Bright sunshine was measured for 1463 hours in Reykjavík, 195 hours more /about-imo/news/2009/nr/1438

• 16. The weather in Iceland 2008

  with precipitation,considering the whole year, was close to average. There was slightly more snowfall than has typical since 2000, but it barely reached the average falls of the preceding decades. There were 64 days with snow-cover in Reykjavík, nine days more than the average 1961-1990, but just below the average for 1971-2000. Bright sunshine was measured for 1463 hours in Reykjavík, 195 hours more /about-imo/news/nr/1438

• 17. The weather in Iceland 2008

  with precipitation,considering the whole year, was close to average. There was slightly more snowfall than has typical since 2000, but it barely reached the average falls of the preceding decades. There were 64 days with snow-cover in Reykjavík, nine days more than the average 1961-1990, but just below the average for 1971-2000. Bright sunshine was measured for 1463 hours in Reykjavík, 195 hours more /about-imo/news/2009/nr/1438/

• 18. The weather in Iceland 2008

  with precipitation,considering the whole year, was close to average. There was slightly more snowfall than has typical since 2000, but it barely reached the average falls of the preceding decades. There were 64 days with snow-cover in Reykjavík, nine days more than the average 1961-1990, but just below the average for 1971-2000. Bright sunshine was measured for 1463 hours in Reykjavík, 195 hours more /about-imo/news/nr/1438/

• 19. ces_SA_group_flyer_new

  Statistical analyses are, therefore, also being undertaken on trends in streamflow and in wind, relative to, for example, the North Atlantic Oscillation (NAO). Other work is considering the relationship between the occurrence of particular weather types and extreme events, such as floods and droughts. For further information, contact: Deborah Lawrence (dela@nve.no) Göran Lindström (Goran.Lindstrom /media/ces/ces_SA_group_flyer_new.pdf

• 20. ved-eng-2008

  was close to average in the North and East, but in the South and West it was a wet year, though not as wet as 2007. The precipitation anomalies were largest in the Northwest. The year began with heavy precipitation, but the first part of the summer was very dry. September was very wet. The number of days with precipitation,considering the whole year, was close to average. There was slightly more /media/vedurstofan/utgafa/skylduskil/ved-eng-2008.pdf