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  • 41. VI_2020_011_en

    / Aðal- og undirtitill: Upplag: 20 An initial volcanic hazard assessment of the Vestmannaeyjar Volcanic System: Impacts of lava flow and tephra deposit on Heimaey Fjöldi síðna: 73 Framkvæmdastjóri sviðs: Jórunn Harðardóttir Höfundar: Melissa Anne Pfeffer, Sara Barsotti, Esther Hlíðar Jensen, Verkefnisstjóri: Emmanuel Pierre Pagneux, Bogi Brynjar Björnsson, Guðrún Jóhannesdóttir, Ármann /media/vedurstofan-utgafa-2020/VI_2020_011_en.pdf
  • 42. IPPC-2007-ar4_syr

    judgment and statistical analysis of a body of evidence (e.g. observations or model results), then the following likelihood ranges are used to express the assessed probability of occurrence: virtually certain >99%; extremely likely >95%; very likely >90%; likely >66%; more likely than not > 50%; about as likely as not 33% to 66%; unlikely <33%; very unlikely <10%; extremely unlikely <5 /media/loftslag/IPPC-2007-ar4_syr.pdf
  • 43. Öræfajökull – frequent questions & answers

    from Öræfajökull can cause complete destruction of man-made structures almost anywhere in sectors at risk of flooding. The potential impact of major floods on the local economy is high. Question: How much time is available at the onset of an eruption for a full evacuation of the floodplain?Answer: Jökulhlaups can be very swift, reaching the lowlands in as little as 20–30 minutes from /volcanoes/about-volcanoes/oraefajokull/q-a/
  • 44. CES_D2.4_task1

    about 20-25% in 2010 to about 50% in 2050. Perhaps surprisingly, a particularly high probability is found in Iceland, most likely as a result of the small 12 interannual variability there. As expected, the probability of very warn years rises even faster than that of warm months – in northern Europe from typically 30-40% in 2010 to about 60- 80% in 2030 and to 85-95% or even more in 2050 /media/ces/CES_D2.4_task1.pdf
  • 45. Bardarbunga_kafli20140825

    an 80 km2 ice-filled caldera. The characteristic activity is explosive basaltic eruptions occurring on central volcano flanks or the fissure swarm. Known eruptions have mostly been VEI 3-4 but occasionally VEI 5-6 (bulk volume of tephra up to 10 km3). The largest eruptions occurred in the early Holocene, effusive basaltic eruptions on the fissure swarm with lava volumes ≥20 km3. Eruption /media/jar/Bardarbunga_kafli20140825.pdf
  • 46. Paper-Olafur-Rognvaldsson_92

  • 47. 2010_017

    an important part of the runoff from many areas. In total, approximately 20% of runoff in Iceland originates from groundwater (Hjartarson, 1994a). In the above mentioned previous simulation of runoff map for Iceland for the period 1961– 1990, groundwater was omitted. Effects of groundwater flowing across watershed boundaries were simulated by scaling the precipitation for each watershed. On watersheds /media/ces/2010_017.pdf
  • 48. 2010_003rs

    ........................................................ 19 2.3.2 Changing the maximum number of events in a group ................................. 20 2.3.3 Rearrange order of input .............................................................................. 22 2.3.4 Relocate only the best events ....................................................................... 22 2.3.5 Other tests /media/vedurstofan/utgafa/skyrslur/2010/2010_003rs.pdf
  • 49. VI_2020_004

    ...................................................................................... 17 2 Selected volcanoes and selected scenarios ......................................................................... 20 2.1 Hekla ......................................................................................................................... 21 2.2 Katla /media/vedurstofan-utgafa-2020/VI_2020_004.pdf
  • 50. CES_BioFuels_Flyer_new

    and how future climate change within the next 20–30 years can impact these resources. In the future, an increase in the utilization of various sources of bioenergy will increase in Nordic countries. This raises a question what is the biomass production potential of forests now and in the future and how sustainable the energy production based on biomass are owing to possible large-scale harvestings /media/ces/CES_BioFuels_Flyer_new.pdf

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