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• 11. Low level flight conditions over Iceland

  -13 FL180: 270/25-45KT, but 26015KT by the NE-coast, -29 Overview of weather systems: 1000 km S of Cape Farewell is an extensive 980 mb low. Over Greenland is a 1038 mb high. Near surface winds: N-ly or variable wind, 05-25 KT. Cloud heights/visibility/weather: BKN/OVC at 1000-2500 FT in the N-part and occasional snowshowers with poor visibility. Widely FEW/SCT and good /weather/aviation/llf-iceland/

• 12. Öræfajökull – frequent questions & answers

  in Iceland and the second largest in Europe after the Vesuvius 79 AD. Question: What are the possible hazards related to an eruption in Öræfajökull?Answer: Tephrafallout, ash cloud, lightning, pyroclastic flows, jökulhlaup /glacial outburst floods, ballistics, lava flows, gas pollution. They will occur over different time frames, with probably the flood to be the first sub-aerial evidence /volcanoes/about-volcanoes/oraefajokull/q-a/

• 13. Iceland a member of ECMWF

  such as ECMWF. I would like to express my appreciation of the ECMWF Council voting unanimously in favour of Iceland’s accession to the ECMWF Convention on 24 February 2011." Árni Snorrason: “Since Iceland became a Co-operating State in December 1980, the Icelandic Meteorological Office has been able to make good use of ECMWF’s products, in particular to improve our forecasts. Above all, the Centre’s /about-imo/news/nr/2142

• 14. Iceland a member of ECMWF

  such as ECMWF. I would like to express my appreciation of the ECMWF Council voting unanimously in favour of Iceland’s accession to the ECMWF Convention on 24 February 2011." Árni Snorrason: “Since Iceland became a Co-operating State in December 1980, the Icelandic Meteorological Office has been able to make good use of ECMWF’s products, in particular to improve our forecasts. Above all, the Centre’s /about-imo/news/2011/nr/2142

• 15. Iceland a member of ECMWF

  such as ECMWF. I would like to express my appreciation of the ECMWF Council voting unanimously in favour of Iceland’s accession to the ECMWF Convention on 24 February 2011." Árni Snorrason: “Since Iceland became a Co-operating State in December 1980, the Icelandic Meteorological Office has been able to make good use of ECMWF’s products, in particular to improve our forecasts. Above all, the Centre’s /about-imo/news/nr/2142/

• 16. Iceland a member of ECMWF

  such as ECMWF. I would like to express my appreciation of the ECMWF Council voting unanimously in favour of Iceland’s accession to the ECMWF Convention on 24 February 2011." Árni Snorrason: “Since Iceland became a Co-operating State in December 1980, the Icelandic Meteorological Office has been able to make good use of ECMWF’s products, in particular to improve our forecasts. Above all, the Centre’s /about-imo/news/2011/nr/2142/

• 17. FAQ

  and grazing animals. Instructions for preparedness before, after and during ashfall can be found on the webpage of the Icelandic Civil Protections.Volcanic ash impact on the aviationA volcanic cloud can reach the altitudes of air traffic routes and threaten the safety of aircrafts. If an airplane flies through a volcanic cloud, the volcanic ash can reduce significantly the visibility and damage /volcanoes/grimsvotn-activity/faq/

• 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. Ash plume and lightnings

  active volcano. It last erupted in 2004 and the current eruption is in a similar location. Flash floods south of the volcano often occur associated with eruptions, but can also happen in between eruptions. The latest such flood occurred in October 2010, so a big flood currently appears unlikely. The MODIS satellite picture taken around 5 o'clock this morning shows the plume; at sunrise the plume /about-imo/news/nr/2177

• 20. norsem_bryndis

  Crustal accretion along the divergent plate boundary in Iceland is governed by rifting episodes and dyking. Over a period of two weeks in August-September 2014, magma propagated laterally from the subglacial Bárðarbunga central volcano, Iceland, about 50 km along the divergent plate boundary to the NNE where it erupted continuously for six months. The dyke propagation was associated with more /media/norsem/norsem_bryndis.pdf