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• 41. Bárðarbunga earthquakes - interactive model

  (central mouse scroll), pan (right click), turn over (left click) choose speed 1x, 2x, 10x (available in some browsers (e.g. Chrome but not Firefox) coloured patches on/off (ring icon) choose landscape map (mountain icon) or satellite image (bell icon) for the surface Tryggvi Hjörvar, specialist at the Icelandic Met Office, created this model. An easier presentation - demo In a video /earthquakes-and-volcanism/articles/nr/2971/

• 42. Bardarbunga_kafli20140825

  volcanic system has been highly active in the Holocene with at least 26 eruptions in the last 11 centuries. The last eruption took place in 1910 CE. The Bárðarbunga system lies on the Eastern Volcanic Zone and is about 190 km long and up to 25 km wide, consisting of a central volcano rising to 2009 m a.s.l. and a fissure swarm partly covered by the Vatnajökull ice cap. The central volcano has /media/jar/Bardarbunga_kafli20140825.pdf

• 43. 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

• 44. 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

• 45. Paper-Olafur-Rognvaldsson_92

  for Meteorological Research, Reykjavík, Iceland 5Bergen School of Meteorology, Geophysical Insitute, University of Bergen, Norway †Corresponding author: or@belgingur.is, Orkugarður, Grensásvegur 9, 108 Reykjavík ABSTRACT Atmospheric flow over Iceland has been simulated for the period Jan- uary 1961 to July 2006, using the mesoscale MM5 model driven by initial and boundary data from the ECMWF. Firstly /media/ces/Paper-Olafur-Rognvaldsson_92.pdf

• 46. Traffc-maintenance_expenditures

  229 1 587 160 1970 18 591 42 413 2 166 86 101 - 892 5 131 2 310 201 - - - 157 805 1 652 904 1969 17 559 38 840 2 313 93 776 - 922 4 562 1 571 - - - - 159 543 1 832 354 1968 13 474 36 376 3 074 104 519 - 1 080 4 131 1 156 - - - - 163 811 1 964 368 1967 11 139 34 495 5 940 95 857 - 419 3 032 1 087 - - - - 151 968 1 936 249 1966 9 835 32 581 8 349 94 777 - 587 4 205 1 743 - - - - 152 077 2 032 936 /media/loftslag/Traffc-maintenance_expenditures.pdf

• 47. 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

• 48. vanRoosmalen_etal-2009-WRR_2007WR006760

  and Irrigationa Scenario Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec Current 101 85 59 13
  6
  4
  1 6 39 79 84 97 A2 145 132 73 10
  10
  7
  6
  8 4 75 92 123 B2 137 119 75 16
  6
  6
  6
  5 21 74 110 141 aValues are in millimeters. 10 of 18 W00A15 VAN ROOSMALEN ET AL.: CLIMATE AND LAND USE CHANGE W00A15 time and larger area where groundwater levels rise above the drain levels. Table 6 shows the mean discharges /media/loftslag/vanRoosmalen_etal-2009-WRR_2007WR006760.pdf

• 49. Bárðarbunga 2014 - December events

  and Herðubreiðartögl. A few small ones were also detected in the dyke intrusion. 30 December 2014 - now confirmed 82.8 km² Two days ago, difficulties in approaching the lava led to doubts about the newest estimate of its size. The Institute of Earth Sciences has now confirmed that the lava is almost 83 km², see map (enlarge). 30 December 2014 10:30 - from the Scientific Advisory Board /earthquakes-and-volcanism/articles/nr/3055

• 50. Bárðarbunga 2014 - December events

  and Herðubreiðartögl. A few small ones were also detected in the dyke intrusion. 30 December 2014 - now confirmed 82.8 km² Two days ago, difficulties in approaching the lava led to doubts about the newest estimate of its size. The Institute of Earth Sciences has now confirmed that the lava is almost 83 km², see map (enlarge). 30 December 2014 10:30 - from the Scientific Advisory Board /earthquakes-and-volcanism/articles/nr/3055/