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Results:

• 41. Bárðarbunga 2014 - December events

  of the eruption column reached 3.1 km above Dyngjusandur, while the base of the aerosol-laden lower part of the plume reached ~1.4 km above the sand plain. Photo: Morten S. Riishuus. The lava extent is now just over 75 km², see map. For comparison, outlines based on a satellite image since 25.11. are given and the northern outline based on fieldwork 27.11. Institute of Earth Sciences. 1 /earthquakes-and-volcanism/articles/nr/3055/

• 42. Bardarbunga-2014_December-events

  Board Notes from the meeting of the Scientific Advisory Board (pdf 0.4 Mb) On Dyngjusandur From Dyngjusandur, northeast of the vent, at 14:41 on 27 Nov 2014. The top of the eruption column reached 3.1 km above Dyngjusandur, while the base of the aerosol-laden lower part of the plume reached ~1.4 km above the sand plain. Photo: Morten S. Riishuus. The lava extent is now just over 75 km /media/jar/Bardarbunga-2014_December-events.pdf

• 43. BIAR_windrose_2005-2014

  ) 0 2 4 6 8 10 0 45 90 135 180 225 270 315 360 N E S W N (Number of observations for wind direction) Icelandic Met Office 02. júl. 2015 62 7 29 6 22 9 11 0 4 5 3 0 1 6 2 3 2 9 3 6 5 1 4 6 5 7 8 9 12 9 19 1 22 8 25 9 34 9 30 2 18 0 6 4 5 4 4 0 4 4 3 2 2 5 2 7 1 8 4 5 12 6 26 1 35 1 54 1 75 0 81 3 Wind rose BIAR July 2005−2014 90 80 70 60 50 40 30 2010360350340 330 320 310 /media/vedur/BIAR_windrose_2005-2014.pdf

• 44. BIEG_windrose_2005-2014

  110 100 2 4 6 8 10 Frequency of wind direction (%) Aerodrome Total observations: 7174 Calm: 12% Variable winds: 3.1% Average wind speed for wind direction Wind direction (°) Wind speed (knots ) 0 2 4 6 8 10 0 45 90 135 180 225 270 315 360 N E S W N (Number of observations for wind direction) Icelandic Met Office 02. júl. 2015 53 5 75 5 32 2 15 2 6 0 4 4 3 1 2 2 2 7 2 1 1 4 4 1 2 2 3 9 /media/vedur/BIEG_windrose_2005-2014.pdf

• 45. Moellenkampetal_etal-2010

  /media/loftslag/Moellenkampetal_etal-2010.pdf

• 46. VI2010-006_web

  ). Með því er átt við að áhættan sé svo lítil að ekki sé ástæða til að grípa til neinna aðgerða til þess að auka öryggi. Staðaráhætta sem svarar til þessa gildis getur verið mismunandi vegna breytilegrar gerðar og styrks bygginga og mismunandi dvalartíma fólks í þeim. Að öðru jöfnu er reiknað með að fólk dvelji allt að 75% af tíma sínum á heimilum og allt að 40% í atvinnu- húsnæði. Samkvæmt /media/vedurstofan/utgafa/skyrslur/2010/VI2010-006_web.pdf

• 47. CES_D2.4_task1

  :34:35 300 P 2649 TUDDAL NO +59:44:43 +08:48:36 464 P 2651 HEREFOSS NO +58:31:01 +08:21:12 85 P 2652 MYKLAND NO +58:37:59 +08:16:54 245 P 2653 TOVDAL NO +58:47:35 +08:14:03 227 P 2654 BAKKE NO +58:24:42 +06:39:29 75 P 2655 FEDAFJORDEN II /media/ces/CES_D2.4_task1.pdf

• 48. Eriksson_Garvill_Nordlund_2006

  Method 2.1. Procedure and participants The study was conducted through a mail survey in four municipalities, situated in different parts of Sweden and varying in population size (from 40,000 to 470,000 citizens). A randomly selected sample, 20–75 years of age, of 4000 respondents, received a questionnaire (see below). After two reminders the overall response rate was 31%, varying from 26% to 35 /media/loftslag/Eriksson_Garvill_Nordlund_2006.pdf

• 49. 2010_003rs

  /media/vedurstofan/utgafa/skyrslur/2010/2010_003rs.pdf

• 50. VI_2009_013

  stress and the spectra of seismic shear waves from earthquakes. J. Geophys. Res., 75, no 26, 4997–5009. Brune, J. N. (1971). Correction. J. of Geophys. Res., 76, No. 20, 5002. Dahm, Thorsten, B. Brandsdóttir (1997). Moment tensors of microearthquakes from the Eyjafjallajökull volcano in South Iceland. Geophys. J. Int, 130, 183–192. Einarsson, P., S. Björnsson, G. Foulger, R. Stefánsson and Th /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_013.pdf