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Results:

• 71. ved-eng-2010

  in January, to 47 consecutive snow-free days, the longest snow-free period ever observed during this time of the year. March was warm except the last five days and the first few days were very cold in the inland. A fissure volcanic eruption started at Fimmvörðuháls on the 20th. The temperature in April was close to the average. There was much snow disrupting traffic in the northeast during /media/vedurstofan/utgafa/skylduskil/ved-eng-2010.pdf

• 72. VI_2016_006_rs

  /media/vedurstofan-utgafa-2016/VI_2016_006_rs.pdf

• 73. ces-glacier-scaling-memo2009-01

  of the area and mean elevation for the ice-free and glaciated parts of each elevation band or grid cell. The areas are denoted by ai and gi, and the elevations by zi and yi, for the ice-free and the ice-covered areas, respectively. At the end of each hydrological year, the hydrological model will provide a simulated value for the total mass balance of each glacier group within the watershed, DVa /media/ces/ces-glacier-scaling-memo2009-01.pdf

• 74. Cooperation is a must for adaptation to and

  the long-term background warming. Mild and snow-free conditions in winters will reduce the number of extreme cold events. For summers more heat waves and droughts may be expected as a result of a longer season with high temperatures in combination with relatively small increases, or even regional decreases, in precipitation. Other, more uncertain impacts on the large-scale circulation /about-imo/news/cooperation-is-a-must-for-adaptation-to-and-mitigation-of-climate-change

• 75. The weather in Iceland in 2016

  heavy precipitation for a period in the South and West, the monthly totals were record high at a few stations. The month was totally frost-free in most coastal areas, which is unusual. NovemberThe month was a warm one with heavy precipitation and the weather was favourable but dark and gloomy. DecemberThe warm weather continued until just before Christmas, in the East this was the warmest /about-imo/news/the-weather-in-iceland-in-2016

• 76. Glacial outburst floods

  from ice-dammed marginal lakes. Such lakes often form when an outlet glacier closes off an ice-free side valley. Grænalón is an Icelandic example of such a lake.Jökulhlaups from supraglacial lakes which have formed by accumulation of meltwater in depressions on the surface of the glacier. Such floods are generally small in Iceland but can be of substantial magnitude on the Greenland ice /volcanoes/volcanic-hazards/glacial-outburst/

• 77. Eriksson_2-Acceptability-of-policy

  and the collective • Why doesn’t everybody cooperate? Low response efficacy, “sucker effect”, free riders 3 (1) Environmental policy measures • Structural versus psychological solutions (Vlek, 1996) • Legal policies, economic policies, measures changing the physical context and informational/educational measures (Steg, 2003) • Targeting technological solutions versus curtailment behaviour /media/loftslag/Eriksson_2-Acceptability-of-policy.pdf