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• 51. Factsheet_Bardarbunga_20141126

  Almannavarnir www.avd.is/en Twitter: @almannavarnir /media/jar/Factsheet_Bardarbunga_20141126.pdf

• 52. Factsheet_Bardarbunga_20140923

  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_20140923.pdf

• 53. 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

• 54. Factsheet_Bardarbunga_20140930

  will be held Wednesday 1 October. 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_20140930.pdf

• 55. Kok_JGEC658_2009

  to be simple and therefore has important drawbacks. Future improvements should be made in the light of applications within a larger toolbox of scenario methods.  2008 Elsevier Ltd. All rights reserved. * Tel.: +31 317 482422; fax: +31 317 419000. E-mail address: kasper.kok@wur.nl. Contents lists available at ScienceDirect Global Environmental Change journa l homepage: www.e lsev ier .com/ locate /media/loftslag/Kok_JGEC658_2009.pdf

• 56. Vertical displacement in the Bárðarbunga caldera

  September 2014. The gray line represents relative displacement and the blue line the median value for 180 minutes. Earthquakes in the area are shown separately below (same x-axis, same timing). Enlarge. The first two weeks as an example Total subsidence from 12 Sept 2014 until 1 March 2015 The total subsidence of the glacier surface above the Bárðarbunga caldera since the equipment /earthquakes-and-volcanism/gps-measurements/bardarbunga/caldera/

• 57. Vertical displacement in the Bárðarbunga caldera

  September 2014. The gray line represents relative displacement and the blue line the median value for 180 minutes. Earthquakes in the area are shown separately below (same x-axis, same timing). Enlarge. The first two weeks as an example Total subsidence from 12 Sept 2014 until 1 March 2015 The total subsidence of the glacier surface above the Bárðarbunga caldera since the equipment /earthquakes-and-volcanism/gps-measurements/bardarbunga/caldera

• 58. ice-chart_colour-code-standard

  less than 10/10 9+ 10/10 10 Undetermined or unknown x Concentration (C) C – Total concentration of ice in the area, reported in tenths (see symbols in table 3.1). Note: Ranges of concentration may be reported. Ca Cb Cc – Partial concentrations of thickest (Ca), second thickest (Cb) and third thickest (Cc) ice, in tenths. Note: Less than 1/10 is not reported. 10/10 of one stage of development /media/hafis/frodleikur/ice-chart_colour-code-standard.pdf

• 59. Ash measurements

  the quality of the data. Therefore, a mobile X-band weather radar was purchased, but while this custom made radar was being assembled and tested, another was obtained on loan from the Italian Civil Protection Agency. The mobile radar is now situated near the town of Kirkjubæjarklaustur, 80 km from the eruption site in Grímsvötn. IMO staff members monitor the progress of the eruption using /about-imo/news/nr/2183/

• 60. Eyjaf_status_2010-05-04_IES_IMO

  of the lava stream. Radar images from ICG-flight today show tunnels in Gígjökull increasing in size and continuing the build up of the cone at the crater. The size of the eruptive crater is 280 x 190 m. Lava splashes are thrown at least a few hundred meters into the air. Seismic tremor: Tremor levels decreased last night (3 May) and have decreased even further this morning at around 11:00 GMT /media/jar/Eyjaf_status_2010-05-04_IES_IMO.pdf