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• 21. Eyjafjallajökull eruption 2010 - the role of IMO

  in April-May 2010, IMO monitored the volcanic activity through various geophysical sensors (seismic, strain, GPS), river runoff from the glacier and the behaviour of the volcanic eruption cloud (see slide show). The main tool for monitoring the volcanic cloud was a C-band weather radar located at Keflavik international airport, approximately 150 km west of the volcano (see map below). Plume height /earthquakes-and-volcanism/articles/nr/2072

• 22. The Eyjafjallajökull eruption 2010

  on activity in Eyjafjallajökull assessment from 14 April until 9 October 2010 QA on the eruption in Eyjafjallajökull, Iceland - 17 April Forecast for volcanic ash fall in Iceland - updated from 20 April until 23 May Photos from Eyjafjallajökull - 9 May An eruption in South Iceland - 23 MarchPhoto galleriesReconaissance flights with the Icelandic Coast Guard - from 24 March until 22 May Local /volcanoes/about-volcanoes/eyjafjallajokull/the-eyjafjallajokull-eruption-2010/

• 23. Flood from Skaftá

  eastern and western, are located in the western part of Vatnajökull Ice-cap. They form because of geothermal activity that melts the glacier from below and water accumulates beneath them. When the hydro static pressure is high enough for the water to lift the ice above and flow from below the cauldrons it causes a flood. Floods from the eastern-cauldron are usually larger than the floods /about-imo/news/flood-in-estern-skafta

• 24. Flood from Skaftá

  eastern and western, are located in the western part of Vatnajökull Ice-cap. They form because of geothermal activity that melts the glacier from below and water accumulates beneath them. When the hydro static pressure is high enough for the water to lift the ice above and flow from below the cauldrons it causes a flood. Floods from the eastern-cauldron are usually larger than the floods /about-imo/news/flood-in-estern-skafta/

• 25. Mission

  IMO has a long-term advisory role with the Department of Civil Protection and Emergency Management of the National Commissioner of the Icelandic Police and issues public alerts about impending natural hazards. The institute participates in international weather and aviation alert systems, such as London Volcanic Ash Advisory Centre (VAAC), and the Icelandic Aviation Oceanic Area Control /about-imo/mission/

• 26. Web-pages on the Eyjafjallajökull eruption 2010

  of the accesscontrolled area around Holuhraun lava field END OF ERUPTION declaredby the Scientific Board Location map (detailed)around the new lava field Bárðarbunga earthquakes3D interactive model Thickness and volumeestimate from January 1st Comparing historic sizes of lavafields: AD 934 and 1783 Gas dispersion model Preliminary flood risk assessmentfor Jökulsá /earthquakes-and-volcanism/articles/nr/2221

• 27. A year since the Eyjafjallajökull eruption began

  the eruption, it was necessary to hold frequent meetings with aviation authorities, flight companies, communities in the vicinity of the volcano and civil protection authorities. IMO was guided by London VAAC, one of the volcanic ash advisory centres. In September 2010, after the eruption, an Atlantic Conference on Eyjafjallajökull and Aviation was held. The Keilir Aviation Academy organized /about-imo/news/nr/2164

• 28. A year since the Eyjafjallajökull eruption began

  the eruption, it was necessary to hold frequent meetings with aviation authorities, flight companies, communities in the vicinity of the volcano and civil protection authorities. IMO was guided by London VAAC, one of the volcanic ash advisory centres. In September 2010, after the eruption, an Atlantic Conference on Eyjafjallajökull and Aviation was held. The Keilir Aviation Academy organized /about-imo/news/2011/nr/2164

• 29. Jens_Christian_Refsgaard_(GEUS,_Dk)

  Refsgaard JC, van der Sluijs JP, Højberg AL, Vanrolleghem PA (2010) Uncertainty analysis in model–based water management: Better modelling practices. In: Vanrolleghem PA, Modelling Aspects of Water Framework Directive Implementation Volume 1. IWA Publishing, London, UK, 271-331. van der Keur P, Henriksen HJ, Refsgaard JC, Brugnach M, Pahl-Wostl C, DeWulf A, Buiteveld H (2008) Identification /media/loftslag/Jens_Christian_Refsgaard_(GEUS,_Dk).pdf

• 30. VI_2020_004

  vedur@vedur.is Veðurstofa Íslands Bústaðavegur 7–9 108 Reykjavík Sara Barsotti, Veðurstofa Íslands Sigrún Karlsdóttir, Veðursstofa Íslands Anna María Ágústsdóttir, Landgræðslan Björn Oddsson, Almannavarnadeild Ríkislögreglustjóra Íris Marelsdóttir, Embætti landlæknis Þorvaldur Þórðarson, Jarðvísindastofnun H áskólans Þórólfur Guðnason, Embætti landlæknis Bogi B. Björnsson, Veðurstofa Íslands /media/vedurstofan-utgafa-2020/VI_2020_004.pdf