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  • 71. Factsheet_Bardarbunga-140909

    Bárðarbunga: 09.09.2014, 11:45 UTC Scientists from the Icelandic Met Office and the Institute of Earth Sciences and representatives of the Civil Protection in Iceland attend the meetings of the Scientific Advisory Board of the Icelandic Civil Protection. Representative from The Environment Agency of Iceland and the Chief Epidemiologist and the Directorate of Health, were also present /media/jar/Factsheet_Bardarbunga-140909.pdf
  • 72. Factsheet_Bardarbunga_140908

    rðárbungá: 08.09.2014, 13:20 UTC Scientists from the Icelandic Met Office and the Institute of Earth Sciences and representatives of the Civil Protection in Iceland attend the meetings of the Scientific Advisory Board of the Icelandic Civil Protection. Also, representatives from The Environment Agency of Iceland and the Chief Epidemiologist from the Directorate of Health, were present /media/jar/Factsheet_Bardarbunga_140908.pdf
  • 73. Further information regarding gas pollution

    rather than towards you.In calm/light wind (<5 m/s) gas can accumulate in the valleys, then circulation is controlled by the landscape and gas can exceed danger levels far up the slopes, all around the eruption site. In such cases, spectators need to move up to higher ground levels such as mountains and ridges and not stay on the slopes just above the eruption. Choose a walking route according /volcanoes/fagradalsfjall-eruption/volcanic-gases/
  • 74. Eyjafjallajokull_status_2010-05-08_IES_IMO

    the lava edge. A small lava tunnel was observed with an infrared camera near to the crater. Seismic tremor: Low, similar to yesterday and similar amplitude on all frequency bands. Earthquakes: Less earthquake activity, two events, Ml 1.2, detected at 9 and 12 km depth at around 11:00h and two of similar magnitude around 14:00. GPS deformation: No significant changes were observed /media/jar/Eyjafjallajokull_status_2010-05-08_IES_IMO.pdf
  • 75. Adalgeirsdottir-etal-tc-5-961-2011

    Korona et al., 2009) and 2010 (airborne LiDAR in autumn). The Cryosphere, 5, 961975, 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
  • 76. Factsheet_Bardarbunga-140911

    o 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 jökulhlaup. Other scenarios cannot be excluded. From the Icelandic Met Office: The Aviation Colour Code for Bárðarbunga remains at ‘orange’ but the code for Askja has been changed to ‘green’. /media/jar/Factsheet_Bardarbunga-140911.pdf
  • 77. Factsheet_Bardarbunga-140912

    develop in another location under the glacier. o 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 jökulhlaup, accompanied by ashfall. Other scenarios cannot be excluded. From the Icelandic Met Office: The Aviation Colour Code for Bárðarbunga remains at ‘orange’ and the code /media/jar/Factsheet_Bardarbunga-140912.pdf
  • 78. Factsheet-Bardarbunga-20140913

    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 jökulhlaup, accompanied by ashfall. Other scenarios cannot be excluded. From the Icelandic Met Office: The Aviation Colour Code for Bárðarbunga remains at ‘orange’. /media/jar/myndsafn/Factsheet-Bardarbunga-20140913.pdf
  • 79. VI_2014_005

    lines). Additionally, the aver- age profiles for offshore distances to the coast of up to 30 km are shown by the black lines. For temperature, the dashed lines indicate linear projection from the two lowest model levels to 2 m above ground. A comparison of monthly averages of simulated 2-m temperature with station measurements, both for SURFEX and projected values, is shown in Figure 8. On average /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_005.pdf
  • 80. Latest news on the eruption at Reykjanes peninsula

    the area and to follow instructions and advice as given by the local Police and Civil Protection authorities.Updated 8.8. at 13:00Gas pollution at the eruption site can at any time exceed danger levels. The eruptive plume follows the wind direction, and it is therefore safer to watch the eruption with the wind direction behind you, rather than towards you.In calm/light wind (<5 m/s) gas can /about-imo/news/a-new-eruption-has-started-at-fagradalsfjall

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