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• 51. Factsheet_Bardarbunga_20141008

  of the caldera. Such an eruption would melt large quantities of ice, leading to a major jokulhlaup, accompanied by ash fall. Other scenarios cannot be excluded.  From the Icelandic Met Office: The Aviation Colour Code for Bardarbunga remains at ‘orange’.  From today, the Scientific Advisory Board will meet on Mondays, Wednesdays and Fridays. The next meeting will be held on Friday 10 /media/jar/Factsheet_Bardarbunga_20141008.pdf

• 52. Factsheet_Bardarbunga_20141010

  DEPARTMENT OF CIVIL PROTECTION AND EMERGENCY MANAGEMENT Information and any questions on air pollution can be sent to The Environment Agency through the email gos@ust.is. The Environment Agency is especially looking for information from people who have been in contact with high concentrations of gas; where they were, at what time it happened, how the gas cloud looked (colour and thickness /media/jar/Factsheet_Bardarbunga_20141010.pdf

• 53. Factsheet_Bardarbunga_20141022

  of Dyngjujokull leading to the eruption site in Holuhraun.  The GPS station in the centre of Bardarbunga show that the subsidence of the caldera continues with similar rate as before.  GPS measurements show minor movements. No great changes were detected.  No change was detected in water monitoring that cannot be explained by changing weather. Air quality:  Today (Wednesday /media/jar/Factsheet_Bardarbunga_20141022.pdf

• 54. Factsheet_Bardarbunga_20141024

  that the subsidence of the caldera continues with similar rate as it has done over the last few weeks.  GPS measurements in the active area show minor changes.  No change was detected in water monitoring that cannot be explained by changing weather. Air quality:  Today (Friday) gas pollution can be expected in the areas north and east of the eruption. Tomorrow (Saturday) the pollution will move first /media/jar/Factsheet_Bardarbunga_20141024.pdf

• 55. Factsheet_Bardarbunga_20140923

  NATIONAL COMMISSIONER OF THE ICELANDIC POLICE DEPARTMENT OF CIVIL PROTECTION AND EMERGENCY MANAGEMENT THE SCIENTIFIC ADVISORY BOARD OF THE ICELANDIC CIVIL PROTECTION Date: 23.09.2014 Time: 09:30 Location: Bifröst, Borgarfirði. Regarding: Volcanic activity in the Bardarbunga system. Attending: Scientists from Icelandic Met Office and the Institute of Earth Sciences University of Iceland /media/jar/myndsafn/Factsheet_Bardarbunga_20140923.pdf

• 56. Factsheet_Bardarbunga_20140924

  accompanied by ash fall. Other scenarios cannot be excluded. From the Icelandic Met Office: The Aviation Colour Code for Bardarbunga remains at ‘orange’. The National Commissioner of the Icelandic Police, Department of Civil Protection and Emergency Management www.almannavarnir.is www.avd.is Twitter: @almannavarnir /media/jar/myndsafn/Factsheet_Bardarbunga_20140924.pdf

• 57. Factsheet_Bardarbunga_20140930

   Large-scale subsidence of the caldera occurs, causing an eruption at the edge of the caldera. Such an eruption would melt large quantities of ice, leading to a major jokulhlaup, accompanied by ash fall. Other scenarios cannot be excluded.  From the Icelandic Met Office: The Aviation Colour Code for Bardarbunga remains at ‘orange’.  Next meeting of The Scientific Advisory Board /media/jar/myndsafn/Factsheet_Bardarbunga_20140930.pdf

• 58. 2010_012rs

  ) closest stations, respectively. The 40 highest correlating events are then inverted for the best location. For comparison the manual locations, obtained by an analyst are shown in yellow. The final locations of the events are all within an approximately 1 km2 area, even though their original, automatic locations are up to 5 km away. They are also within a few hundred meters from the manual /media/vedurstofan/utgafa/skyrslur/2010/2010_012rs.pdf

• 59. Notes on the 2010 eruptions

  the crater, supported by lower plume (2-4 km) according to radar. MODIS satellite image shows both ash from the volcanic site and loose ash blown from the surface of Mýrdalsjökull ice cap. Comments on sound blasts, viscosity, deflation and tremors. Link to satellite image RADARSAT-2 (from the Canadian Space Agency), link to a briefing issued by WMO of frequently asked questions. 25.04.2010 – 28.05.2010 /earthquakes-and-volcanism/articles/nr/2467

• 60. 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