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• 11. Factsheet_Bardarbunga_20141017

  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 Monday 20 October. The National Commissioner of the Icelandic Police, Department of Civil /media/jar/Factsheet_Bardarbunga_20141017.pdf

• 12. Factsheet_Bardarbunga_20141020

  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 (Monday), gas pollution can be expected in the east and later southeast of Iceland /media/jar/Factsheet_Bardarbunga_20141020.pdf

• 13. Bárðarbunga 2014 - October events

  2014 with the Icelandic Coast Guard. Cloud boundary with haze or dust contaminated clouds below. Photo: Elín Björk Jónasdóttir. 17 October 2014 10:00 - from geoscientist on duty About 100 earthquakes have been observed in Iceland during the past 24 hours, of which 84 were close to the Bárðarbunga area. Few quakes were located in the intrusion but over 40 in the Tungnafellsjökull area /earthquakes-and-volcanism/articles/nr/3011

• 14. Bardarbunga-2014_October-events

  previously been observed for several M>5 events and can not be interpreted as a decrease of the overall activity. The subsidence rate of the caldera had shortly increased around one hour after the M5.3 and is now again back to normal rates, see graph, which also is a frequent observation associated with M>5 earthquakes in Bárðarbunga. Around 20 events have been detected in the northern part /media/jar/Bardarbunga-2014_October-events.pdf

• 15. Bárðarbunga 2014 - October events

  2014 with the Icelandic Coast Guard. Cloud boundary with haze or dust contaminated clouds below. Photo: Elín Björk Jónasdóttir. 17 October 2014 10:00 - from geoscientist on duty About 100 earthquakes have been observed in Iceland during the past 24 hours, of which 84 were close to the Bárðarbunga area. Few quakes were located in the intrusion but over 40 in the Tungnafellsjökull area /earthquakes-and-volcanism/articles/nr/3011/

• 16. Bárðarbunga 2014 - December events

  (pdf 0.4 Mb). The Scientific Advisory Board of the Icelandic Civil Protection has held 80 meetings since the seismic activity started on the 16th of August. The Scientific Advisory Boards wishes all its' dedicated readers a Merry Christmas. 22 December 2014 10:00 - from geoscientist on duty Bárðarbunga: The largest earthquake measured the last 24 hours was M4.5 and occurred at 16:12 yesterday /earthquakes-and-volcanism/articles/nr/3055

• 17. Bárðarbunga 2014 - December events

  (pdf 0.4 Mb). The Scientific Advisory Board of the Icelandic Civil Protection has held 80 meetings since the seismic activity started on the 16th of August. The Scientific Advisory Boards wishes all its' dedicated readers a Merry Christmas. 22 December 2014 10:00 - from geoscientist on duty Bárðarbunga: The largest earthquake measured the last 24 hours was M4.5 and occurred at 16:12 yesterday /earthquakes-and-volcanism/articles/nr/3055/

• 18. Bardarbunga-2014_December-events

  the crater. Lava is also running to the north. Notes from the meeting of the Scientific Advisory Board (pdf 0.4 Mb). The Scientific Advisory Board of the Icelandic Civil Protection has held 80 meetings since the seismic activity started on the 16th of August. The Scientific Advisory Boards wishes all its' dedicated readers a Merry Christmas. 22 December 2014 10:00 - from geoscientist /media/jar/Bardarbunga-2014_December-events.pdf

• 19. Hare-2011-ParticipatoryModelling

  are labelled according to the geographical area of application. Examples such as Zürich and Hase II have already been reviewed and categorized in Hare et al. (2003) and Bots and van Daalen (2008), respectively. The entire Iskar process, of which Iskar (Phase I) is a part, has been categorized by Barreteau et al. (2010). All are included in this review to provide alternative analytical perspectives /media/loftslag/Hare-2011-ParticipatoryModelling.pdf

• 20. Kriauciuniene_Jurate_CES_2010

  9 8 0 2 0 0 0 -45 -30 -15 0 15 30 45 60 1 9 2 0 1 9 4 0 1 9 6 0 1 9 8 0 2 0 0 0 -45 -30 -15 0 15 30 45 60 1 9 2 0 1 9 6 0 2 0 0 0 -45 -30 -15 0 15 30 45 60 1 9 2 0 1 9 4 0 1 9 6 0 1 9 8 0 2 0 0 0 Annual -15 -10 -5 0 5 10 15 20 -0.4 -0.2 0.0 0.2 0.4 0.6 0.8 1.0T, C Q, % Q (1991-2007) Q1(1931-1960) Winter -40 -20 0 20 40 60 80 -0.2 0.0 0.2 0.4 0.6 0.8T, C Q, % Q (1991-2007) Q1(1931-1960) Spring -20 /media/ces/Kriauciuniene_Jurate_CES_2010.pdf