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Results:

• 51. Eriksson_Garvill_Nordlund_2006

  indicated an improved model (RMSEA ¼ 0.063 (PCLOSE ¼ 0.116), CFI ¼ 0.968). The modified model was then tested on sub-sample 2, and results showed that all proposed relations were significant and goodness-of-fit was adequate (RMSEA ¼ 0.070 (PCLOSE ¼ 0.035), CFI ¼ 0.967). Explained variance in acceptability was 51% in the first sub-sample and 49% in the second sub-sample (see Fig. 2). 3.3.2. Information /media/loftslag/Eriksson_Garvill_Nordlund_2006.pdf

• 52. News

  News © Veðurstofa Íslands An example from the weather app. Two screenshots side by side /about-imo/news/bigimg/3224

• 53. ces-oslo2010_proceedings

  anomalies of the WTs during the periods leading up to the five most severe droughts as compared to the average frequency of a given WT for the same period of the year over the entire data record. A period equal to dreg preceding the drought plus the 20 first days of the drought was used. All WTs with a net positive frequency anomaly over the five events were considered to be associated /media/ces/ces-oslo2010_proceedings.pdf

• 54. Bárðarbunga 2014 - October events

  activity. The subsidence rate of the caldera had shortly increased around one hour after the M5.3 and is now again back to normal rates, see graph, which also is a frequent observation associated with M>5 earthquakes in Bárðarbunga. Around 20 events have been detected in the northern part of the dyke intrusion; the strongest was 2.1 at 11:51 yesterday. Activity has been low around /earthquakes-and-volcanism/articles/nr/3011

• 55. Bardarbunga-2014_October-events

  of the dyke intrusion; the strongest was 2.1 at 11:51 yesterday. Activity has been low around Tungnafellsjökull, Herðubreið and Askja during the last 24 hours. The eruption ongoing, but rarely visible so far today. 25 October 2014 12:00 - from geoscientist on duty Seismic activity on the Bárðarbunga caldera rim continues at comparably high rates as in recent days. Activity in the dyke intrusion /media/jar/Bardarbunga-2014_October-events.pdf

• 56. Bárðarbunga 2014 - October events

  activity. The subsidence rate of the caldera had shortly increased around one hour after the M5.3 and is now again back to normal rates, see graph, which also is a frequent observation associated with M>5 earthquakes in Bárðarbunga. Around 20 events have been detected in the northern part of the dyke intrusion; the strongest was 2.1 at 11:51 yesterday. Activity has been low around /earthquakes-and-volcanism/articles/nr/3011/

• 57. A minor eruption underway

  of Fagradalsfjall, M4,4 at 12:06, M4,0 at 12:24, M4,1 at 13:51 og M4,2 at 15:10. All those are in a similar location as the M5,7 earthquake. Our interpretation is that these are triggered earthquakes caused by the intense activity and deformation that has occurred in the area. The swarm is still ongoing and roughly 5000 earthquakes have been detected with the automatic system since the beginning /about-imo/news/earthquake-swarm-in-reykjanes-peninsula

• 58. BIGR_windrose_2005-2014

  11 8 12 11 12 1 2 4 9 11 16 16 20 13 28 51 Wind rose BIGR November 2005−2014 90 80 70 60 50 40 30 2010360350340 330 320 310 300 290 280 270 260 250 240 230 220 210 200 190 180 170 160 150 140 130 120 110 100 1 2 3 4 5 6 Frequency of wind direction (%) Aerodrome Total observations: 876 Calm: 0.91% Variable winds: 0.23% Average wind speed for wind direction Wind direction (°) Wind speed (knots /media/vedur/BIGR_windrose_2005-2014.pdf

• 59. Paper-Olafur-Rognvaldsson_91

  balance data from all the ice caps. REFERENCES Björnsson, H., Pálsson F., Guðmundsson M. T. and Haraldsson H. 1998. Mass balance of western and northern Vatnajökull, Iceland, 1991–1995, Jökull, 45, 35–58. Björnsson, H., Pálsson F. and Haraldsson H. 2002. Mass balance of Vatnajökull (1991–2001) and Langjökull (1996–2001), Iceland. Jökull, 51, 75–78. Bromwich, D. H., Bai L. and Bjarnason G. G. 2005 /media/ces/Paper-Olafur-Rognvaldsson_91.pdf

• 60. Bárðarbunga 2014 - September events

  part of the caldera, at 22:51 M3.5, at 02:04 M3.4 and at 04:44 M4.1. All in all, 16 earthquakes have been detected in Bárðarbunga from midnight, the majority at the northern caldera rim. Only 5 earthquakes have been detected under Dyngjujökull, the largest about M2 in size. According to web cameras the intensity of the eruption is unchanged. The extent of the lava field The extent /earthquakes-and-volcanism/articles/nr/3001