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• 21. Eyjafjallajokull_SK_20101214_1

  ) Discussions between the forecasters of IMO and London VAAC about the situation. Next steps to improve monitoring of ash plumes ICAO has agreed to invest in and deploy portable high frequency dual polarization Doppler radar for accurate plume height measurements and potential assessment of the mass transport; timescale 7-8 months. PM10 ash sensor network being investigated. Lidar for airborne ash /media/vedurstofan/myndasafn/Eyjafjallajokull_SK_20101214_1.pdf

• 22. A FUTUREVOLC exercise

  and running models to determine information such as the mass eruption rate. All of this was done in real time. To evaluate downstream dissemination of information, the exercise included the London Volcanic Ash Advisory Centre (VAAC) and representatives from the international media and civil protection. The recently released FutureVolc datahub and Catalogue of Icelandic Volcanoes were also tested /about-imo/news/nr/3277

• 23. Web-pages related to the Grímsvötn eruption 2011

  Of interest - Bárðarbunga Reduction 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 /earthquakes-and-volcanism/articles/nr/2220

• 24. Ash cloud extending to Europe

  aviation authorities consider the ash cloud to be an hazard to aviation, are advised to examine the homepage of the Volcano Advisory Centre in London. Click on the link "Issued graphics" above the map, and choose the most recent map. For more news, click 2010. News 2023 /about-imo/news/nr/1873

• 25. 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

• 26. Ash cloud extending to Europe

  aviation authorities consider the ash cloud to be an hazard to aviation, are advised to examine the homepage of the Volcano Advisory Centre in London. Click on the link "Issued graphics" above the map, and choose the most recent map. For more news, click 2010. News 2023 /about-imo/news/2010/nr/1873

• 27. Ash cloud extending to Europe

  aloft are forecast for the weekend. Those who want to follow the areas, within which aviation authorities consider the ash cloud to be an hazard to aviation, are advised to examine the homepage of the Volcano Advisory Centre in London. Click on the link "Issued graphics" above the map, and choose the most recent map. For more news, click 2010 /about-imo/news/nr/1873/

• 28. Ash cloud extending to Europe

  aloft are forecast for the weekend. Those who want to follow the areas, within which aviation authorities consider the ash cloud to be an hazard to aviation, are advised to examine the homepage of the Volcano Advisory Centre in London. Click on the link "Issued graphics" above the map, and choose the most recent map. For more news, click 2010 /about-imo/news/2010/nr/1873/

• 29. VI_2016_006_rs

  of 100–140 m a.s.l. Several debris flows are recorded in Búðará since the beginning of the 20th century. It is not clear whether the upper or lower area is the main source for these debris flows. The return time for sizeable debris flows in Búðará is around 20 years. It appears that the land- slide activity has been more frequent in the last 30 years than earlier in the 20th century. 4.5 Areas 7 /media/vedurstofan-utgafa-2016/VI_2016_006_rs.pdf

• 30. 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