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• 11. Supporting structures stopped most of an avalanche

  ). The narrow curves show outlines of historical avalances. The health care centre is the large H-shaped building close to the hillside. The rows of supporting structures are shown as black dashed lines. It may be estimated that 5,000-10,000 m³ of snow were stopped in the rows of supporting structures. This is many times the volume of snow in the avalanche tongue below the structures. The snow cover /about-imo/news/nr/2476/

• 12. Supporting structures stopped most of an avalanche

  red curve). The narrow curves show outlines of historical avalances. The health care centre is the large H-shaped building close to the hillside. The rows of supporting structures are shown as black dashed lines. It may be estimated that 5,000-10,000 m³ of snow were stopped in the rows of supporting structures. This is many times the volume of snow in the avalanche tongue below the structures /avalanches/articles/nr/2475/

• 13. NONAM_Perrels_ea_-_From_top-down_to_integrated_economic_assessment

  From top-down to interactive economic assessments – example Finland Adriaan Perrels1, Tony Rosqvist2, Hanna Virta1 1. Finnish Meteorological Institute FMI; 2. Technical Research Centre of Finland VTT email address: adriaan.perrels@fmi.fi Finland started to assess possible economic impacts of climate change as part of the so-called SILMU program1 from 1992 to 1995. In that time it was still /media/loftslag/NONAM_Perrels_ea_-_From_top-down_to_integrated_economic_assessment.pdf

• 14. Avalanche bulletin - Eyjafjörður (experimental)

  { fill: #BDD7EE; } .status1 .s1, .status2 .s2, .status3 .s3, .status4 .s4, .status5 .s5 { fill: #1F4E78; } .status1 .a1, .status2 .a2, .status3 .a3, .status4 .a4, .status5 .a5 { display: block; } /* Elevation */ .elevation { /* width: 255px; height: 197px; */ width: 70px; height: 54px; } .elev-full .mask { clip-path: url(#full); /*clip-path: inset(0 0 0% round 0px /avalanches/forecast/inner_eyjafjordur

• 15. Avalanche bulletin - Tröllaskagi

  { fill: #BDD7EE; } .status1 .s1, .status2 .s2, .status3 .s3, .status4 .s4, .status5 .s5 { fill: #1F4E78; } .status1 .a1, .status2 .a2, .status3 .a3, .status4 .a4, .status5 .a5 { display: block; } /* Elevation */ .elevation { /* width: 255px; height: 197px; */ width: 70px; height: 54px; } .elev-full .mask { clip-path: url(#full); /*clip-path: inset(0 0 0% round 0px /avalanches/forecast/trollaskagi

• 16. Avalanche bulletin - Eyjafjörður (experimental)

  { fill: #BDD7EE; } .status1 .s1, .status2 .s2, .status3 .s3, .status4 .s4, .status5 .s5 { fill: #1F4E78; } .status1 .a1, .status2 .a2, .status3 .a3, .status4 .a4, .status5 .a5 { display: block; } /* Elevation */ .elevation { /* width: 255px; height: 197px; */ width: 70px; height: 54px; } .elev-full .mask { clip-path: url(#full); /*clip-path: inset(0 0 0% round 0px /avalanches/forecast/inner_eyjafjordur/

• 17. Avalanche bulletin - Tröllaskagi

  { fill: #BDD7EE; } .status1 .s1, .status2 .s2, .status3 .s3, .status4 .s4, .status5 .s5 { fill: #1F4E78; } .status1 .a1, .status2 .a2, .status3 .a3, .status4 .a4, .status5 .a5 { display: block; } /* Elevation */ .elevation { /* width: 255px; height: 197px; */ width: 70px; height: 54px; } .elev-full .mask { clip-path: url(#full); /*clip-path: inset(0 0 0% round 0px /avalanches/forecast/trollaskagi/

• 18. A small jökulhlaup in Gígjukvísl

  which does not exceed high river discharge at summer. The road and bridge are safe. A small jökulhlaup The bridge across river Gígjukvísl, 27 March 2014 at 08:00, view to the WNW and the mountain in the background is Lómagnúpur. Photo: Njáll Fannar Reynisson. The river Skeiðará changed its course in 2009 and now runs due west along the margin of Skeiðarárjökull outlet glacier /about-imo/news/nr/2859

• 19. Fractures in Svínafellsheiði and a potential rockslide on Svínafellsjökull

  to 1.3 cm over one year. In the spring of 2018, a new fracture running down the western slope of Svínafellsheiði was discovered. Recent analysis of remote sensing data shows that the area between the fractures and the glacier margin has moved at a rate of 2 to 4 cm per year in the period from late August 2016 to late August 2017. The area in motion is about 0.5–1 km2 in size. A rough estimate /about-imo/news/fractures-in-svinafellsheidi-and-a-potential-rockslide-on-svinafellsjokull

• 20. Vertical displacement in the Bárðarbunga caldera

  September 2014. The gray line represents relative displacement and the blue line the median value for 180 minutes. Earthquakes in the area are shown separately below (same x-axis, same timing). Enlarge. The first two weeks as an example Total subsidence from 12 Sept 2014 until 1 March 2015 The total subsidence of the glacier surface above the Bárðarbunga caldera since the equipment /earthquakes-and-volcanism/gps-measurements/bardarbunga/caldera/