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Results:

• 31. Group3-Road-scenarios

  in asphalt, road maintenace Change: 30% more than BAU Socio-economic scenario Climate scenario Worst case (4.4 C increase; 17 % increase in prec) Best case (1.5 C increase; 2% increase in prec) BAU A B Change +30 % C D Spatial analogues: - regions which today have a similar climate to the expected future one the study region (IPCC TAR, 2001) - limited by possible lack /media/loftslag/Group3-Road-scenarios.pdf

• 32. VI_2015_006

  m 2 or less, compared with losses of 80 W m 2 or more over neigh- bouring cloud-free regions. The conditions around midnight, off the southeast coast on 27 July, and along the north coast on 3 September, clearly show the limited ability (in the model) of even a complete high-level cloud cover to affect the longwave radiation balance at the surface. Mid- level clouds are usually simulated together /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_006.pdf

• 33. 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

• 34. 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/

• 35. askja_minnisblad_ens

  and rescue team saw a white plume rise up above Askja at 23:27. The steam plume was created when the slide exposed shallow geothermal areas in the release area. In addition, a dust cloud created by the rock slide may have contributed to the plume. The release area of the rockslide is approximately 800 m wide and 350 m above the lake surface. It may have been a "rotational slide movement", which /media/ofanflod/myndasafn/frodleikur/askja_minnisblad_ens.pdf

• 36. VI_2014_001

  flood method for deriving flood quantiles at gauged sites with limited data availability (see for in- stance Blazkova and Beven, 1997; Cameron et al., 1999; Fiorentino et al., 2007; and a review by Boughton and Droop, 2003). A distributed hydrological model calibrated on a gauged catch- ment can be used to continuously simulate discharge series at different sites on that catchment and flood /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_001.pdf

• 37. VI_2015_009

  flood models 1–24 (Eqs. 8 and 9 applied with variables 1–12). Ratio between esti- mated and reference index flood (solid black line). The solid blue line corresponds to the reference index flood (Ratio=1), estimated as the arithmetic mean of the observed AMF sample and the dashed blue lines the 95% CI derived from the GEV distribution. Large red symbol indicates overall best model. 18 4.2.2 Flood /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_009.pdf

• 38. “The small eruption” in

  This was very important as the eruption has attracted many people since the beginning. During the first weeks over 6000 people visited the eruptions site daily and during summer, when tourists could access Iceland again, it continued to be busy. “It has been challenging to guarantee a safe access to the area, given the frequent change in eruptive styles and consequent type of volcanic hazards /about-imo/news/the-small-eruption-in-fagradalsfjall-celebrates-six-months

• 39. “The small eruption” in

  This was very important as the eruption has attracted many people since the beginning. During the first weeks over 6000 people visited the eruptions site daily and during summer, when tourists could access Iceland again, it continued to be busy. “It has been challenging to guarantee a safe access to the area, given the frequent change in eruptive styles and consequent type of volcanic hazards /about-imo/news/the-small-eruption-in-fagradalsfjall-celebrates-six-months/

• 40. Rockslide in Askja, July 21 2014 - Preliminary results of observations

  plume rise up above Askja at 23:27. The steam plume was created when the slide exposed shallow geothermal areas in the release area. In addition, a dust cloud created by the rock slide may have contributed to the plume. The release area of the rockslide is approximately 800 m wide and 350 m above the lake surface. It may have been a "rotational slide movement", which means that the failure surface /avalanches/articles/nr/2929