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Results:

• 51. Refsgaard_etal-2007-Uncertainty-EMS

  and possibly the stake- holders at different phases of the modelling project. Many QA guidelines exist such as Middlemis (2000) and Van Waveren et al. (1999). The HarmoniQuA project (Schol- ten et al., 2007; Refsgaard et al., 2005a) has developed a com- prehensive set of QA guidelines for multiple modelling domains combined with a supporting software tool, MoST (downloadable via http /media/loftslag/Refsgaard_etal-2007-Uncertainty-EMS.pdf

• 52. VI_2014_001

  /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_001.pdf

• 53. “The small eruption” in

  to make an SO2 flux measurement by walking along the edge of the lava field (Photo: Elísabet Pálmadóttir).The gas released from the eruption has been spreading over Iceland in the past 6 months. The area most impacted is northwest of the eruption. Short-lived peaks in SO2 ground concentration over 1000 microgram/m3 have been measured in a few instances in Njarðvík (Figure 9) and Vogar for example /about-imo/news/the-small-eruption-in-fagradalsfjall-celebrates-six-months

• 54. “The small eruption” in

  to make an SO2 flux measurement by walking along the edge of the lava field (Photo: Elísabet Pálmadóttir).The gas released from the eruption has been spreading over Iceland in the past 6 months. The area most impacted is northwest of the eruption. Short-lived peaks in SO2 ground concentration over 1000 microgram/m3 have been measured in a few instances in Njarðvík (Figure 9) and Vogar for example /about-imo/news/the-small-eruption-in-fagradalsfjall-celebrates-six-months/

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

  out, adding to the results and making them more precise. Below are photographs, maps and graphs that show the main results of measurements and analyses that are available, now two weeks after the event. Width of fracture line: 800 m Vertical drop: 350 m Runout length beyond the lake shore: ~1000 m Volume: ~30–50 million m³ Estimated duration of the slide: 20 seconds according to seismographs /avalanches/articles/nr/2929

• 56. vanRoosmalen_etal-2009-WRR_2007WR006760

  with 20% and 2% for the HIRHAM experiments using HadAM3H and with 30% and 7% for the ECHAM- driven experiments for Middle Europe and Scandinavia, respectively. [18] RCM output is not available for the entire period 1961–2100 because transient RCM simulations are com- putationally very demanding. Instead two 30-year time slices are available; one representative for the climate in the period 1961–1990 /media/loftslag/vanRoosmalen_etal-2009-WRR_2007WR006760.pdf

• 57. VI_2014_006

  the com- plexity of the hydrological processes through modelling, but its application is usually limited to the short-range. Although the results demonstrated a great potential for this method, its success- ful application in real-time will strongly depend on the quality and availability of streamflow observations, which can be poor or simply missing during periods of variable durations, e.g /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_006.pdf

• 58. A minor eruption underway

  earthquakes were detected. Three were larger than magnitude 3, the largest M3.3 at 2:37AM located around 1km N of Nátthagi valley. Today at 13:00GMT the Scientific Advisory Board of the Icelandic Civil Protection will meet to evaluate the latest monitoring data. Findings of the meeting are expected shortly after 15:00GMT.Updated 15.03 at 11:00 Since midnight over 1000 earthquakes have been detected /about-imo/news/earthquake-swarm-in-reykjanes-peninsula

• 59. Information and help

  a truck; destroy a small building or break a few trees. 1000 tonn 4 Could bury and destroy a railway car, large truck, several buildings or a piece of forest. 10.000 tonn 5 Could gouge the landscape; disastrous damage potential. 100.000 tonn It is not always easy or obvious how to classify the size of an avalanche, however, the destructive potential is the predominant /avalanches/forecast/help

• 60. GA_2009_91A_4_Andreassen

  the principalmethods have not changed much over the years, theamount of field work has varied. In the first 15 yearsthe monitoring programme at Storbreen was com-prehensive, often three or more snow density pits were dug, snow depth was measured at about 600points and ablation was measured on 30 stakes evenly distri uted on the glacier (Liestøl 1967).Based on experience of the snow pattern, the ob- servations /media/ces/GA_2009_91A_4_Andreassen.pdf