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  • 11. “The small eruption” in

    This was very important as the eruption has attracted many people since the beginning. During the first weeks over 6000 people visited the eruptions site daily and during summer, when tourists could access Iceland again, it continued to be busy. “It has been challenging to guarantee a safe access to the area, given the frequent change in eruptive styles and consequent type of volcanic hazards /about-imo/news/the-small-eruption-in-fagradalsfjall-celebrates-six-months/
  • 12. NOMEK09_Report

    received by students. The content of media awareness and global warming were included and also a lectures on aviation, avalanches and forecast errors. The course administration was taken care of by Kristín Hermannsdóttir and Sigþrúður Ármannsdóttir, IMO including hotel reservation for all participants and teachers, tickets for sponsored participants and teachers, making budget and maintaining /media/vedurstofan/utgafa/skyrslur/2009/NOMEK09_Report.pdf
  • 13. Bárðarbunga 2015 - February events

    The eruption eruption was clearly visible in web cameras. 3 February 2015 - photos from a surveillance flight In a separate article, photos from a surveillance flight 3 February 2015 show both the gasplume, gas fumaroles from the center of the lava field far away from the craters, and photos of the eruptive site. 3 February 2015 12:00 - from the Scientific Advisory Board Hardly any changes /earthquakes-and-volcanism/articles/nr/3087
  • 14. Bárðarbunga 2015 - February events

    The eruption eruption was clearly visible in web cameras. 3 February 2015 - photos from a surveillance flight In a separate article, photos from a surveillance flight 3 February 2015 show both the gasplume, gas fumaroles from the center of the lava field far away from the craters, and photos of the eruptive site. 3 February 2015 12:00 - from the Scientific Advisory Board Hardly any changes /earthquakes-and-volcanism/articles/nr/3087/
  • 15. Bardarbunga-2015_February_events

     The area continues to be closely monitored.  Gas contamination is still detected around the eruption site.  No changes have been made to the restricted area north of Vatnajökull.  The Civil Protection still operates in alert phase.  Aviation Colour Code for Bárðarbunga has been downgraded from orange to yellow. 27 February 2015 15:15 - no glow seen in flight In a helicopter flight /media/jar/Bardarbunga-2015_February_events.pdf
  • 16. VI_2009_012

    Mw(v) plotted against log distance. The coefficient of correlation between Mw(v) and log distance is 0.24. High correlation coefficients have been shown to affect parameter estimates in one step regression methods (see Fukushima and Tanaka, 1990). The Ci values were also calculated from the derived PGA values. Instead of constructing another magnitude scale based on acceleration it was decided /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_012.pdf
  • 17. Water_resources_man_Veijalainen_etal

    range 90% 93.1593.29 93.2793.36 75.43–75.56 94.5994.71 2040–2069 range 90% 93.0993.31 93.2893.40 75.41–75.56 94.7294.83 2070–2099 range 90% 93.0293.32 93.2493.43 75.38–75.61 94.7994.91 Lowest water level (in the 30 year period) (m) Reference period 92.86 92.72 75.20 94.27 2010–2039 range 90% 92.6292.91 92.9693.13 75.24–75.33 94.4794.59 2040–2069 range 90% 92.5592.82 92.8893.12 75.19 /media/ces/Water_resources_man_Veijalainen_etal.pdf
  • 18. VI_2009_013

    to locate earthquakes in Iceland but the SIL-crustal model has no Moho boundary. Using this model in the routine, daily analysis, the majority of the earthquakes in Eyjafjallajökull form a 3-km-wide chimney between 1 and 10 km depth beneath the northern flank of the volcano. A smaller cloud is also visible between 19 and 25 km depth, about 1.5 km west of the main activity/cluster. 13 Figure 3 /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_013.pdf
  • 19. 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
  • 20. ces-glacier-scaling-memo2009-01

    difference between the band and the maximum altitude of the glaciers ymax Dgi = ri gi ; ri = DSa2 (ymax yi) nj=1(ymax y j)g j : (12) The second step is carried out after the lowest glaciated elevation bands have been altered by the reduction in the glaciated area at the lowest altitudes. This procedure to distribute the reduction in glaciated area with altitude is clearly quite crude /media/ces/ces-glacier-scaling-memo2009-01.pdf

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