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• 21. A year since the Eyjafjallajökull eruption began

  the conference, where the effects of volcanic events on the travel industry were discussed. The Icelandic Meteorological Office organized an international meeting in Reykjavík with those responsible for the flow of information, i.e. from the scientific community to the civil protection authorities, to the media and to the public. Also in September, an international workshop of geoscientists was held /about-imo/news/2011/nr/2164

• 22. Hock_Regine_CES_2010rs

  Projections Iceland -70% -10% Temperature Precipitation +3% Temperature Precipitation Scandinavia -80% Glacier Volume Projections Iceland -70% -10% Temperature Precipitation +3% Temperature Precipitation Scandinavia Large differences between GCMs GCMs too coarse ? --> Do RCMs do a better job? -80% Volume Projections: Storglaciären -73% 78% M M Volume Projections: Mårmaglaciären -50% -48% M M Volume /media/ces/Hock_Regine_CES_2010rs.pdf

• 23. VI_2009_006_tt

  /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_006_tt.pdf

• 24. Group5-Draft_report

  and the cause of the event when the topic of climate change first tried to squeeze itself into the political agenda. The media in particular played a salient role in establishing conflicting themes centering on these issues, which reflected different interests of the stakeholders. Scientists who took the initiative to propagate climate change issues could not reach an agreement in the first place /media/loftslag/Group5-Draft_report.pdf

• 25. Linnet_Ulfar_CES_2010

  are stationary Changes in flow •Difference between historical series (1950 to 2004) and 2050 series •Direct runoff and spring fed • 5 – 6 % increase •Glacier rivers • 25 - 84 % increase •2050 series are stationary Generation vs. inflow •By the year 2050 inflow has increased by 16 % •At the same time production capacity has only increased by 6 % •Utilization of the runoff decreases from 84 % to 78 % Effect /media/ces/Linnet_Ulfar_CES_2010.pdf

• 26. VI_2020_004

  49 Probabilistic hazard map for a load ≥1000 kg/m2 (Öræfajökull) ............................ 78 Figure 50 Seasonal analysis for 1 kg/m2 (~1mm) tephra ground load (Öræfajökull). ............ 79 Figure 51 Seasonal analysis for 10 kg/m2 (~1 cm) tephra ground load (Öræfajökull). ........... 80 Figure 52 Impact map for roads in case of an eruption like 1362 at Öræfajökull ................... 81 /media/vedurstofan-utgafa-2020/VI_2020_004.pdf

• 27. Traffc-maintenance_expenditures

  602 1985 69 162 268 854 21 519 287 550 - 8 390 17 755 26 574 8 767 - - - 708 572 1 444 484 1984 63 220 239 096 17 569 274 379 - 6 561 17 510 21 630 7 314 - - - 646 775 1 373 444 1983 58 155 225 692 22 930 273 852 - 7 658 15 811 17 982 7 433 - - - 629 513 1 410 203 1982 52 712 189 383 15 822 262 412 - 8 974 15 974 17 509 10 038 - - - 572 824 1 385 993 1981 48 251 172 997 14 874 234 817 - 6 526 20 /media/loftslag/Traffc-maintenance_expenditures.pdf

• 28. NOMEK09_Report

  received by students. The content of media awareness and global warming were included and also a lectures on aviation, avalanches and forecast errors. The course administration was taken care of by Kristín Hermannsdóttir and Sigþrúður Ármannsdóttir, IMO including hotel reservation for all participants and teachers, tickets for sponsored participants and teachers, making budget and maintaining /media/vedurstofan/utgafa/skyrslur/2009/NOMEK09_Report.pdf

• 29. 2010_003rs

  /media/vedurstofan/utgafa/skyrslur/2010/2010_003rs.pdf

• 30. VI_2022_006_extreme

  -year return period, based on the complete ICRA dataset. Timeseries were extracted using the average value of all the grid-points within the catchment. 1M5 value is shown in red. Hálslón 2 years 5 years 10 years 25 years 50 years 100 years 3 hours 8 11 13 15 18 20 6 hours 18 23 27 31 36 39 12 hours 35 43 49 54 62 67 24 hours 60 70 78 85 94 101 48 hours 91 105 115 125 137 147 /media/vedurstofan-utgafa-2022/VI_2022_006_extreme.pdf