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Results:

• 31. 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

• 32. vanRoosmalen_etal-2009-WRR_2007WR006760

  /media/loftslag/vanRoosmalen_etal-2009-WRR_2007WR006760.pdf

• 33. 2010_003rs

  ...................................................................................................................... 63 x 5 Conclusions .................................................................................................................... 67 References ........................................................................................................................... 69 APPENDIX A –List of fault parameters /media/vedurstofan/utgafa/skyrslur/2010/2010_003rs.pdf

• 34. 2010_005_

  /media/ces/2010_005_.pdf

• 35. VI_2020_011_en

  in this report ........................................... …69 Figures Figure 1: Map of Iceland featuring the main central volcanoes, fissure swarms, main volcanic belts and populated areas that could be particularly vulnerable to effusive eruption products .. 11 Figure 2: Bathymetry and topography of the Vestmannaeyjar volcanic system ..................... 15 Figure 3: Map of Heimaey /media/vedurstofan-utgafa-2020/VI_2020_011_en.pdf

• 36. ces-oslo2010_proceedings

  /media/ces/ces-oslo2010_proceedings.pdf

• 37. 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

• 38. VI_2016_006_rs

  horizontal displacement of the most active part of Þófi since the start of the measurements is mostly in the range 10–35 cm (maximum 69 cm), whereas the movement in Neðri-Botnar is slower, with the more active points having total displacement mostly in the range 5–10 cm (maximum 46 cm). The maximum measured velocity of the horizontal movement in the Þófi area was 92 cm/a over a two-month period in late /media/vedurstofan-utgafa-2016/VI_2016_006_rs.pdf

• 39. 2010_012rs

  /media/vedurstofan/utgafa/skyrslur/2010/2010_012rs.pdf

• 40. VI_2020_005

  /media/vedurstofan-utgafa-2020/VI_2020_005.pdf