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• 11. Iceland a member of ECMWF

  day of the second month following the deposit of its instrument of accession. Svandís Svavarsdóttir: “It is an honour for me to sign the accession agreement with the European Centre for Medium-Range Weather Forecasts, one of the world’s leading centres in numerical weather prediction. This is a major milestone for Iceland in establishing closer links to European centres of excellence /about-imo/news/2011/nr/2142

• 12. Iceland a member of ECMWF

  day of the second month following the deposit of its instrument of accession. Svandís Svavarsdóttir: “It is an honour for me to sign the accession agreement with the European Centre for Medium-Range Weather Forecasts, one of the world’s leading centres in numerical weather prediction. This is a major milestone for Iceland in establishing closer links to European centres of excellence /about-imo/news/nr/2142/

• 13. Iceland a member of ECMWF

  day of the second month following the deposit of its instrument of accession. Svandís Svavarsdóttir: “It is an honour for me to sign the accession agreement with the European Centre for Medium-Range Weather Forecasts, one of the world’s leading centres in numerical weather prediction. This is a major milestone for Iceland in establishing closer links to European centres of excellence /about-imo/news/2011/nr/2142/

• 14. 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

• 15. 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/

• 16. FAQ

  meters-size (bombs and ballistics) can land up to few km from the vent and can represent a serious hazard in the proximity of a volcano. Those particles that decouple quickly from the volcanic plume due to their size and weight fall close to the volcano and constitute the proximal deposit. Smaller particles can reach higher altitudes and persist in the atmosphere for days and weeks /volcanoes/grimsvotn-activity/faq/

• 17. 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/

• 18. 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

• 19. 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/

• 20. 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