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Results:

• 21. 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

• 22. 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

• 23. 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

• 24. 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

• 25. 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

• 26. 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/

• 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/2010/nr/1873/

• 28. Moellenkampetal_etal-2010

  Acteurs et Usages (UMR G-EAU), Cemagref, 4University of Architecture, Civil Engineering and Geodesy, 5Hornsby Shire Council, 6Lisode, 7UN-Water Decade Programme on Capacity Development (UNW-DPC), United Nations University, 8School of Natural and Rural Systems Management, University of Queensland, 9College of Asia and the Pacific, The Australian National University, 10Marine and Atmospheric Research /media/loftslag/Moellenkampetal_etal-2010.pdf

• 29. Adalgeirsdottir-etal-tc-5-961-2011

  Korona et al., 2009) and 2010 (airborne LiDAR in autumn). The Cryosphere, 5, 961–975, 2011 www.the-cryosphere.net/5/961/2011/ G. Aðalgeirsdóttir et al.: 20th and 21st century evolution of Hoffellsjökull glacier 963 Fig. 2. (A) Measured bedrock topography of Hoffellsjökull (2001). Blue colours indicate elevation below sea level. (B–E) Surface to- pography at different times, showing retreat /media/ces/Adalgeirsdottir-etal-tc-5-961-2011.pdf

• 30. 2012-Refsgaard_etal-uncertainty_climate-change-adaptation-MITI343

  e in relatio n to climat echang eadapt ation .X ,X X ,XX X is a ge n era lguid eo n th e relativ e imp ortanc e leve lo fth e sourc es , alth oug h it mus tb e em phasise d tha tth e imp ortanc e o fth e indi vidua lsou rce s o fun certaint y is co n tex tspe cifi c St ep si n cl im at e ch an ge ad ap tat io n an al ys es (ch ain in u n ce rta in ty ca sc ad e, Fi g. 2) So ur ce s o fu n ce rta /media/loftslag/2012-Refsgaard_etal-uncertainty_climate-change-adaptation-MITI343.pdf