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  • 61. VI_2020_004

    Preliminary tephra fallout hazard assessment for selected eruptive scenarios in Iceland Sara Barsotti Sigrún Karlsdóttir Anna María Ágústsdóttir Björn Oddsson Íris Marelsdóttir Þorvaldur Þórðarson Þórólfur Guðnason Bogi B. Björnsson VÍ 2020-004 Skýrsla Preliminary tephra fallout hazard assessment for selected eruptive scenarios in Iceland VÍ 2020-004 ISSN 1670-8261 Skýrsla +354 522 60 00 /media/vedurstofan-utgafa-2020/VI_2020_004.pdf
  • 62. AnneFleig_May2010_CES

    E l b e i n D r e s d e n , A p r i l 2 0 0 7 CES conference, Oslo, Norway, 31 May - 2 June 2010 Typical features • develop slowly, • become severe when they cover a large region and persist for an extended period. E l b e i n D r e s d e n , A p r i l 2 0 0 7 ( s p i e g e l . d e ) Anne K. Fleig et al. “Regional hydrological droughts and weather types in north /media/ces/AnneFleig_May2010_CES.pdf
  • 63. VI_2020_005

    . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 9 2 Background . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 11 2.1 Factors affecting sea level . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 12 2.1.1 Main factors affecting sea level in Scandinavia, the UK and Iceland . . . . 13 2.2 Sea level data /media/vedurstofan-utgafa-2020/VI_2020_005.pdf
  • 64. Kok_and_Veldkamp_editorial_ES-2011-4160

    ? Methodological reflections on scalar structuration. Progress in Human Geography 25:591-614. Bryan, B. A., N. D. Crossman, D. King, W. S. Meyer. 2011. Landscape futures analysis: assessing the impacts of environmental targets under alternative spatial policy options and future scenarios. Environmental Modelling and Software 26(1):83-91. Buizer, M., B. Arts, and K. Kok. 2011. Governance, scale /media/loftslag/Kok_and_Veldkamp_editorial_ES-2011-4160.pdf
  • 65. Hock_Regine_CES_2010rs

    ERA-40 and six GCMs ERA4 0 GC M Seasonal temperature cycles averaged over 1961-2001 ERA-40 and six GCMs ERA4 0 GC M ’local scaling’ Method Step 1: Calibrating an elevation dependent mass balance model to 44 glaciers b(h)= - M(h) + C(h) + R(h) hmin hmax ELA Woodward et al., 1997 Melt Snow accumulation Refreezing Results Global volume projections for 21th century (11%) (28 /media/ces/Hock_Regine_CES_2010rs.pdf
  • 66. Johannesson_Thomas_CES_2010

    of Time- Variable Gravity Show Mass Loss in Antarctica. Science, 311, 5768, 1754 – 1756. DOI: 10.1126/science.1123785. Wouters, B., D., Chambers and E. J. O. Schrama. 2008. GRACE observes small-scale mass loss in Greenland. Geophys. Res. Lett., 35, L20501, doi:10.1029/2008GL034816. Meier, F. M., and others. 2007. Glaciers Dominate Eustatic Sea-Level Rise in the 21st Century. Science, 317, 1064–1067 /media/ces/Johannesson_Thomas_CES_2010.pdf
  • 67. Eriksson_Garvill_Nordlund_2006

    were collected through a mail survey in Sweden, Acceptability of travel demand managemen of problem awareness, persona Louise Erikssona,b,, Jo¨rgen Garvil aDepartment of Psychology bTransportation Research Unit Available onlin Abstract y 26 (2006) 15–26 t measures: The importance norm, freedom, and fairness la,b, Annika M. Nordlunda,b a˚ University, Sweden Umea˚ University, Sweden 14 July 2006 /media/loftslag/Eriksson_Garvill_Nordlund_2006.pdf
  • 68. VI_2016_006_rs

    Overview of landslide hazard and possible mitigation measures in the settlement southeast of Fjarðará River in Seyðisfjörður Daniel Illmer Jón Kristinn Helgason Tómas Jóhannesson Eiríkur Gíslason Sigurjón Hauksson VÍ 2016-006 Report Cover photo: Jón Kristinn Helgason, 11 September 2015 Overview of landslide hazard and possible mitigation measures in the settlement southeast of Fjarðará River /media/vedurstofan-utgafa-2016/VI_2016_006_rs.pdf
  • 69. “The small eruption” in

    swarm in December 2019 until the beginning of the eruption (Graph: Skjálfta-Lísa from the Icelandic Meteorological Office (IMO)). Satellite and GPS signals showed that a magmatic dyke extended southwest from Keilir to Fagradaslfjall (Figure 2 A&B) and was getting shallower day by day. Uncertainty remained whether the intrusion would result in an eruption. “For the deformation team the period /about-imo/news/the-small-eruption-in-fagradalsfjall-celebrates-six-months
  • 70. “The small eruption” in

    swarm in December 2019 until the beginning of the eruption (Graph: Skjálfta-Lísa from the Icelandic Meteorological Office (IMO)). Satellite and GPS signals showed that a magmatic dyke extended southwest from Keilir to Fagradaslfjall (Figure 2 A&B) and was getting shallower day by day. Uncertainty remained whether the intrusion would result in an eruption. “For the deformation team the period /about-imo/news/the-small-eruption-in-fagradalsfjall-celebrates-six-months/

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