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• 11. Avalanches in Iceland

  and landslides have caused both death and injury and done great damage to infrastructure and property in Iceland. In the twentieth century, 193 persons died, thereof 69 persons after 1974. Financial cost between 1974 and 2000 amounts to 3.3 billion IKR. Catastrophic avalanches in the villages Súðavík (January) and Flateyri (October) 1995, which killed 34 people and caused extensive economic damage /avalanches/avalanches/

• 12. VI_2020_004

  and synthetic scenario .......................................................... 60 6 5.3.2 Probabilistic hazard maps ................................................................................ 62 5.3.3 Towards Impact-based maps ............................................................................ 69 5.4 Öræfajökull /media/vedurstofan-utgafa-2020/VI_2020_004.pdf

• 13. VI_2020_005

  therein and archeological evidence can be used to indirectly infer mean sea levels thousands of years back. Geological evidence of former sea levels can be used to reconstruct the sea level history of the past on geological time scales, thousands to millions of years, through different climate conditions. In the geological record, a clear link can be seen be- tween climate and sea level /media/vedurstofan-utgafa-2020/VI_2020_005.pdf

• 14. IPPC-2007-ar4_syr

  (-33%) during 1970 to 2004 has been smaller than the com- bined effect of global income growth (77%) and global population growth (69%); both drivers of increasing energy-related CO2 emis- sions. The long-term trend of declining CO2 emissions per unit of en- ergy supplied reversed after 2000. {WGIII 1.3, Figure SPM.2, SPM} Differences in per capita income, per capita emissions and energy /media/loftslag/IPPC-2007-ar4_syr.pdf

• 15. Flood from Skaftá

  /about-imo/news/flood-in-estern-skafta

• 16. Flood from Skaftá

  /about-imo/news/flood-in-estern-skafta/

• 17. 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

• 18. VI_2019_009

  To distinguish between rain and snow, the volume is com- pared to the water equivalent but the volume of snow is ten times larger. Figure 1. How PWD22 determines the type of precipitation. Using the information about the changes of the backscatter signal, water equivalent and temper- ature the Vaisala Present Weather Detector can give information about the type of precipitation. It is also used /media/vedurstofan-utgafa-2019/VI_2019_009.pdf

• 19. VI_2009_006_tt

  to theoretical framework. I do also want to thank him for an enjoyable time during this work, both in the office and in the field. This work was carried out as a part of the Skaftá cauldrons research project which was funded and supported by the Icelandic Centre For Research (RANNÍS), Kvískerja- sjóður, the NASA Astrobiology Institute, Landsvirkjun (the National Power Com- pany), the National Energy /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_006_tt.pdf

• 20. CES_D2.4_task2_CMIP3_winds

  in the Nordic area in its western parts (Denmark, west coast of Sweden and western Norway up to 69°N). Along with the simulated warming of the climate, the wind speeds increase in the southern part of northern Europe, the average Vg over the southern Baltic Sea being 9,5-10 m/s in the period 1971-2000 and 10-10,5 m/s in 2046-2065. 3 Fig. 2. 10-GCM mean of the simulated geostrophic wind speeds /media/ces/CES_D2.4_task2_CMIP3_winds.pdf