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Results:

• 31. 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

• 32. 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

• 33. Forecasts - Gufuskálar

  GMT 9° ENE 3 Cloud cover: 100% 21 GMT 8° ENE 4 Cloud cover: 100% Sun 7.05 00 GMT 6° ENE 5 Cloud cover: 100% 06 GMT 5° ENE 6 Cloud cover: 100% 12 GMT 8° ENE 8 Cloud cover: 100% 18 GMT 7° ENE 11 Cloud cover: 100% Mon 8.05 00 GMT 5° ENE 8 Cloud cover: 90% 06 GMT 6° ENE 5 Cloud cover: 100% 12 GMT 9° NE 6 Cloud cover: 100 /m/forecasts/areas

• 34. BIHN_windrose_2005-2014

  9 3 2 2 7 1 6 8 6 12 9 13 2 15 8 Wind rose BIHN March 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 1 2 3 4 5 6 7 8 Frequency of wind direction (%) Aerodrome Total observations: 2200 Calm: 6% Variable winds: 0.73% Average wind speed for wind direction Wind direction (°) Wind speed (knots ) 0 5 /media/vedur/BIHN_windrose_2005-2014.pdf

• 35. BIBD_windrose_2005-2014

  8 2 2 4 5 22 5 1 4 2 4 2 4 8 11 9 34 7 3 31 3 2 1 BIBD gusts exceeding 50 knots (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 5 10 15 20 25 Frequency of wind direction (%) Aerodrome Total observations: 78 Calm: 0% Variable winds: 0% Average wind speed for wind direction Wind /media/vedur/BIBD_windrose_2005-2014.pdf

• 36. VI_2020_005

  and CNES, n.d.; National Center for Atmospheric Research Staff, 2016; Quante and Colijn, 2016). Now, additional altimeters at different orbits perform slightly less accurate measurements up to 82 N and S (Rhein et al., 2013). These records are used to estimate sea surface changes and calculate global mean sea level, a temporal average sea level averaged over the oceans (Church, Clark, et al., 2013 /media/vedurstofan-utgafa-2020/VI_2020_005.pdf

• 37. VI_2015_005

  Franz Josef Land. The western boundary at 71 W excludes Hudson Bay and Foxe Basin, both associated with their own storm climate. Baffin Bay is included in its entirety, since storm activity in that region is closely linked to that over the western North Atlantic (Dacre & Gray, 2009). The eastern boundary at 55 E is chosen to completely include the Barents Sea. This results in an area of 21,625,566 /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_005.pdf

• 38. VI_2014_005

  lines). Additionally, the aver- age profiles for offshore distances to the coast of up to 30 km are shown by the black lines. For temperature, the dashed lines indicate linear projection from the two lowest model levels to 2 m above ground. A comparison of monthly averages of simulated 2-m temperature with station measurements, both for SURFEX and projected values, is shown in Figure 8. On average /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_005.pdf