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  • 11. arhrifafylki_web

    Impact Matrix of the Icelandic Meteorological Office Minimal or no hazard. No damage likely. Medium or high likelihood of medium impact weather which can have localized affects. This weather could affect travels between different areas of Iceland. The weather is potentially hazardous if precautions are not taken and can cause damages or accidents. Yellow warnings are fairly common /media/frettir/arhrifafylki_web.pdf
  • 12. Publications 2020

    assessment of the Vestmannaeyjar Volcanic System: Impacts of lava flow and tephra deposit on Heimaey Melissa Anne Pfeffer, Sara Barsotti, Esther Hlíðar Jensen, Emmanuel Pierre Pagneux, Bogi Brynjar Björnsson, Guðrún Jóhannesdóttir, Ármann Höskuldsson, Laura Sandri, o.fl. 73 16,0 2020-008 Reassessment of precipitation return levels in Iceland Andréa-Giorgio R. Massad, Guðrún Nína /about-imo/publications/2020/
  • 13. VI_2020_011_en

    An initial volcanic hazard assessment of the Vestmannaeyjar Volcanic System: Impacts of lava flow and tephra deposit on Heimaey Melissa Anne Pfeffer, Sara Barsotti, Esther Hlíðar Jensen, Emmanuel Pierre Pagneux, Bogi Brynjar Björnsson, Guðrún Jóhannesdóttir, Ármann Höskuldsson, Laura Sandri, Jacopo Selva, Simone Tarquini, Mattia de´Michieli Vitturi, Ingibjörg Jónsdóttir, Davið Egilson /media/vedurstofan-utgafa-2020/VI_2020_011_en.pdf
  • 14. Big_landslides_Table_ENG

    Naustavík/Náttfaravíkur by Skjálfandi bay Heavy snowmelt, accumulation of water at the boundary between rock and loose material 1.2 June 1995 Þormóðsstaðir in Sölvadalur in Eyjafjörður Heavy snowmelt, accumulation of water in ancient rockslide deposit 0.6–0.8 March 2007 Morsárjökull Unstable slope by a glacier 4–4.5 April 2007 Stóra-Selfjall in Múladalur/Geithellnadalur in Álftafjörður /media/frettir-myndasafn-2018/Big_landslides_Table_ENG.pdf
  • 15. Öræfajökull – frequent questions & answers

    to melt. The pyroclastic flows and jökulhlaup caused by the 1362 eruption are thought to have resulted in the death of ~300 individuals. The magnitude of the 1362 jökulhlaup was of order 100,000 m3/s, whereas the 1727 flood was about half that size. In 1362 tephra fallout buried houses and villages with a deposit >40cm thick.The Öræfajökull eruption in 1362 has been one of the largest eruption /volcanoes/about-volcanoes/oraefajokull/q-a/
  • 16. Avalanche notices on the web - an improved map

    Photo: Sveinn Brynjólfsson. EAWS avalance size classification Avalanche size. Extent of the avalanche, classified by destructive potential and runout length. Size 1 Sluff Minimal danger of burying (danger of falling) Snow relocation stops typically before the end of a slope Size 2 Small Avalanche Could bury, injure or kill a person Snow avalanche stops typically at the end of a slope Size 3 /about-imo/news/nr/2838
  • 17. Avalanche notices on the web - an improved map

    Photo: Sveinn Brynjólfsson. EAWS avalance size classification Avalanche size. Extent of the avalanche, classified by destructive potential and runout length. Size 1 Sluff Minimal danger of burying (danger of falling) Snow relocation stops typically before the end of a slope Size 2 Small Avalanche Could bury, injure or kill a person Snow avalanche stops typically at the end of a slope Size 3 /about-imo/news/nr/2838/
  • 18. About the implementation

    are in the forefront. Architecture It was decided to use the Eplica content management system. It is as a Java based system so specific dynamic components were written in Java. It was decided to use Servlets and the MVC pattern, with minimal usage of Eplica API. This way the components may be moved and reused with minimal efforts in other Java CMS or converted to Portlets (JSR 168) if and when /about-imo/the-web/implementation/
  • 19. Daniell_etal-2010

    the process was to be set in the real world to avoid the perception of being merely a hypothetical exercise. Before opting for collaboration with researchers and consultants, the Wupperverband faced many uncertainties concerning the future management of the Dhuenn and the organization of a participatory process. The Wupperverband knew about the temperature problem in the Dhuenn and its impact on the fish /media/loftslag/Daniell_etal-2010.pdf
  • 20. A large landslide falls in Hítardalur valley

    displacements and might be an old landslide deposit. The displaced material is a mixture of e.g. rock debris, scree from the lower part of the hillside, swamp soil and sediments from ancient lakes on the valley bottom. A preliminary estimate of the volume of the slide is 10–20 million m3. The area of the debris tongue is ca. 1,5 km2 and the debris is up to 20–30 m thick. The thickness is 5–10 m in many /about-imo/news/a-large-landslide-falls-in-hitardalur-valley

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