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Results:

• 31. CES_D2.4_task2_CMIP3_winds

  in the average wind speed between the baseline (or control) period 1971-2000 and the scenario period 2046-2065. These periods were chosen based on the availability of model output at daily time resolution. We have analyzed the surface geostrophic wind (hereafter Vg) rather than the actual simulated surface winds, because the latter are sensitive to the details of the boundary layer /media/ces/CES_D2.4_task2_CMIP3_winds.pdf

• 32. Wind Energy

  Technical University, August 2007. Journal of Physics Conference Series, Vol. 75. 8 pp. Pryor, S. C., Schoof, J. T., Clausen, N.-E. & Drews, M. (2010). Changes in extreme wind and intense wind speeds in Northern Europe. European wind energy conference, Warsaw, April 2010. National Barthelmie, R.J. & Pryor, S. C. (2007). Wind speed trends over the contiguous USA. 30th Annual Applied Geography /ces/publications/nr/1944

• 33. Instructions on using meteograms

  side-by-side. Note that when a meteogram is requested via the search option, it is added to other meteograms that are on the page already. By using the search option it is possible to review meteograms from any weather station. The URL of the page changes with each addition. By bookmarking the URL, or saving it in another way, the same batch of meteograms can be retrieved on later visits. Links /weather/articles/nr/1217

• 34. Risk Assessment

  in a changing climate was carried out through the following steps: Review of risk and uncertainty management approaches used in the energy sector; and Integration of risk and uncertainty in decision support tools. A risk management framework, developed by VTT of Finland, according to the emphasis of the industrial partners, has since been tested and applied in various energy sectors (e.g. hydro /ces/project/risk/

• 35. VI_2009_013

  to locate earthquakes in Iceland but the SIL-crustal model has no Moho boundary. Using this model in the routine, daily analysis, the majority of the earthquakes in Eyjafjallajökull form a 3-km-wide chimney between 1 and 10 km depth beneath the northern flank of the volcano. A smaller cloud is also visible between 19 and 25 km depth, about 1.5 km west of the main activity/cluster. 13 Figure 3 /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_013.pdf

• 36. 2010_017

  m J M5 [C°] -3 obs. [C°] -4 nce 1 re 5. Comp 26); an int temperatu this system y gridded v picion abo -Jökulsá w similar dif han observ h elevation ces the effe months No ly only on high the tem n band wi refore be s onthly tem an Feb Ma .2 -3.1 -3. .3 -4.1 -3. .1 1.0 0.6 arison of m erpolation re is shown atic differe alues, see T ut the qual atershed; b ference wa ations for t gradient fo /media/ces/2010_017.pdf

• 37. Increased seismic activity between Krýsuvík and Ölfus

  settlements have spread closer to historically active earthquake faults. It can be expected that large earthquakes on the eastern Reykjanes peninsula will affect surrounding areas (capital region, Grindavík, Þorlákshöfn, Hveragerði and Reykjanesbær). Such earthquakes would be felt by all people in the affected area, many people might be frightened and leave their homes. Heavy furniture could /about-imo/news/nr/3150

• 38. Seismic activity around Mt. Þorbjörn has decreasing

  from the Civil Protection, ISAVIA-ANS and Police Dept of the South-Iceland.In the beginning of April the uplift in Þorbjörn decreased and, in the second part of the month, it stopped. The area around Þorbjörn is now most likely recovering after the large induced stress, and the injected magma is cooling down and contracting. Along with reduced deformation, seismic activity has decreasing /about-imo/news/seismic-activity-around-mt-thorbjorn-has-decreasing-significantly

• 39. Factsheet_Bardarbunga_20160623

  with representatives from the Icelandic Civil Protection. Main points  Activity in the Bardarbunga system since the end of the eruption. Notes Today the Civil Protection Scientific Advisory Board met to review new data on the volcano Bárðarbunga. During a scientific expedition on Vatnajökull June 3rd to 10th echo soundings of the glacier were done to examine whether changes in bedrock /media/jar/Factsheet_Bardarbunga_20160623.pdf

• 40. 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