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Results:

• 31. ces-oslo2010_proceedings

  change over the North Atlantic and in some simulations also for Iceland. In all areas, including the North Atlantic and Iceland, a clear climate change signal compared to the spread between the simulations is seen. The standard deviation calculated from 17 of the simulations are less than 1°C in all areas apart from Iceland where it reaches between 1 and 2°C and in parts of the Barents Sea where /media/ces/ces-oslo2010_proceedings.pdf

• 32. 2010_005_

  Century control runs, as well as 21st Century forecast runs, submitted by various institutions to the Intergovernmental Panel on Climate Change (IPCC) for their Forth 11 Table 1. General circulation and regional climate models that were considered in this study. Model Version Model Name, Institute BCCR BCM 2.0 Bergen Climate Model, Bjerknes Centre for Climate Research, Bergen, Norway CCCMA CGCM 3.1 /media/ces/2010_005_.pdf

• 33. 2013_001_Nawri_et_al

  and a pressure of 1013.25 hPa. In the case of Iceland, the climate deviates significantly from these standard atmospheric conditions. Additionally, terrain elevation varies considerably across the island. Therefore, seasonal and annual differences in air density from the standard value, as well as spatial variability, need to be taken into account. Approximate air density can be calculated by assuming /media/vedurstofan/utgafa/skyrslur/2013/2013_001_Nawri_et_al.pdf

• 34. IMO at the Arctic Circle Assembly 2017

  the USA, the European Space Agency (ESA) and China.Ingvar Kristinsson, managing director at IMO, participated in a session on the potential effects of volcanic ash clouds from Icelandic volcanoes on aviation in the Arctic airspace. In a special session on issues related to Arctic Freshwater, Halldór Björnsson and Þorsteinn Þorsteinsson contributed to a discussion on freshwater fluxes /about-imo/news/imo-at-the-arctic-circle-assembly-2017

• 35. The segmented dyke intrusion explained

  to time of occurrence and the colour code is shown at the top of the map. The earthquake locations delineate the track of the dyke intrusion from Bárðarbunga volcano to the eruption site at Holuhraun. Vertical cross sections through the crust are also shown; looking from the south (below) and east (to the right). Triangles mark the locations of seismic stations in and around the glacier. Data /about-imo/news/nr/3038

• 36. Case_B___Road_transport_operation_and_infrastructure_planning

  on the Shifts of climatic zones from cooler or wetter to warmer or drier (a) 1971-2000 (b) 2010-39 A1B observational data set (0.25º grid) from Haylock et al. (2008) (b-d) Based on CMIP3 GCM runs for A1B & the delta-change method (c) 2040-69 A1B (d) 2070-99 A1B Jylhä et al. (2010) Uncertainties in climate change schematically Observed climate Future climate Natural /media/loftslag/Case_B___Road_transport_operation_and_infrastructure_planning.pdf

• 37. event_numbers_17022015

  Earthquakes since 16. August 2014 00:00 all intrusion caldera Kistufell Askja HB / HBT TFJ Kverkfj. automatic ~ 35.000 - - - - - - - checked ~ 20.000 ~ 8.000 ~ 9.000 ~ 200 ~ 300 ~ 1.800 ~ 600 ~ 20 M3.0-3.9 1208 99 1089 6 2 4 7 1 M4.0-4.9 655 7 646 1 1 0 0 0 M>5.0 79 0 79 0 0 0 0 0 HB / HBT Herðubreið and Herðubreiðartögl TFJ Tungnafellsjökull Kverkfj. Kverkfjöll Kistufell cluster north /media/jar/myndasafn/frodleikur/event_numbers_17022015.pdf

• 38. BIGJ_windrose_2005-2014

  1 2 1 1 Wind rose BIGJ April 2005−2014 90 80 70 60 50 40 30 2010360350340 330 320 310 300 290 280 270 260 250 240 230 220 210 200 190 180 170 160 150 140 130 120 110 100 2 4 6 8 10 Frequency of wind direction (%) Aerodrome Total observations: 114 Calm: 0.88% Variable winds: 0% Average wind speed for wind direction Wind direction (°) Wind speed (knots ) 0 5 10 15 0 45 90 135 180 225 270 315 /media/vedur/BIGJ_windrose_2005-2014.pdf

• 39. A large landslide falls in Hítardalur valley

  released from the landslide source area at present. People should, therefore, not travel close the landslide area and the police has closed two gravel roads leading up to the slide.The next steps in the study of this landslide will be to process measurements that have been carried out and analyse aerial photographs as well as other photographs from the area, both before and after the slide /about-imo/news/a-large-landslide-falls-in-hitardalur-valley

• 40. A large landslide falls in Hítardalur valley

  released from the landslide source area at present. People should, therefore, not travel close the landslide area and the police has closed two gravel roads leading up to the slide.The next steps in the study of this landslide will be to process measurements that have been carried out and analyse aerial photographs as well as other photographs from the area, both before and after the slide /about-imo/news/a-large-landslide-falls-in-hitardalur-valley/