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• 31. Bárðarbunga 2014 - September events

  February, March-April-May and the overview article (list of links). Calendar Below is a calendar with a short-cut to each day of this month's events: Sept.:1-2-3-4-5-6-7-8-9-10-11-12-13-14-15-16-17-18-19-20-21-22-23-24-25-26-27-28-29-30 Panoramic view towards the eruptive site in Holuhraun 3rd September 2014. Photo: Richard Yeo. Updated information 30 September 2014 18:50 - from /earthquakes-and-volcanism/articles/nr/3001/

• 32. VI_2020_011_en

  rate [km3/ month]3 Reference Eldfell 23/01/73–28/06/73 5.1 0.27 0.24 9–100 3.7 0.04 A, B, C, D, E Surtsey effusive phase 14 04/04/64–17/05/65 13.5 ? 0.3 max 100 ? >0.02 F, G Surtsey effusive phase 25 19/08/66–05/06/67 9.5 ? 0.1 max 70 ? >0.02 F, G Helgafell 5900 BP 11.5 0.65 0.59 3–50 6.5 <0.06 B, F, H Klif 12900 BP ? 0.01 0.009 ? ? ? B References: A: Jakobsson et al., 1973; B: Mattsson /media/vedurstofan-utgafa-2020/VI_2020_011_en.pdf

• 33. Lorenzoni_Pidgeon_2006

  ) Survey indicated that more than half of the respondents in 13 out of 24 countries worldwide felt that climate change was a serious problem (Brechin, 2003, p. 109). Of these 13 nations, 8 were European (and 5 formed part of the EU15); the USA did not figure in these 13. More than 65% of the surveyed populations in the same 23 out of 24 nations indicated they felt that global warming was a serious /media/loftslag/Lorenzoni_Pidgeon_2006.pdf

• 34. VI_2013_006

  <6h <12h <24h Total Grímsvötn 1998-12-18 09:20 2 h 0 1 20 121 167 183 Hekla 2000-02-26 18:17 41 min 1 4 6 6 6 6 Grímsvötn 2004-11-01 21:50 4 h 0 0 15 59 142 251 Fimmvörðuháls 2010-03-20 23:34 - 0 0 0 0 0 0 Eyjafjallajökull 2010-04-14 01:15 17 h 0 0 0 0 10 790 Grímsvötn 2011-05-21 19:00 15 min 888 3340 6484 11729 16041 16195 9 The monitoring system There are two main parts /media/vedurstofan/utgafa/skyrslur/2013/VI_2013_006.pdf

• 35. 2005EO260001

  lake within the caldera until the surrounding ice is breached. When that happens, water escapes to cause a jökulhlaup in the river Skeidará, after having traveled ~50 km beneath the Skeidarárjökull outlet glacier (Figure 1b). Jökulhlaups occur there every 1–10 years and last from days to weeks, each time releasing 0.4–4 km3 of water [Björnsson, 2002]. Volcanic eruptions in Gríms- vötn often /media/jar/myndsafn/2005EO260001.pdf

• 36. On the Bárðarbunga gradual caldera collapse

  volcano collapsed during the eruption as 1.9 km³ of magma flowed laterally from a magma reservoir under the volcano. About one quarter formed a 48 km long dyke (0.5 km³) while about three quarters were erupted in Holuhraun (1.4 km³) over the six months between 31 August 2014 and 27 February 2015. The subsidence bowl formed in Bárðarbunga was up to 65 m deep and the area where subsidence exceeded 1 m /about-imo/news/on-the-bardarbunga-gradual-caldera-collapse

• 37. On the Bárðarbunga gradual caldera collapse

  volcano collapsed during the eruption as 1.9 km³ of magma flowed laterally from a magma reservoir under the volcano. About one quarter formed a 48 km long dyke (0.5 km³) while about three quarters were erupted in Holuhraun (1.4 km³) over the six months between 31 August 2014 and 27 February 2015. The subsidence bowl formed in Bárðarbunga was up to 65 m deep and the area where subsidence exceeded 1 m /about-imo/news/on-the-bardarbunga-gradual-caldera-collapse/

• 38. BIKF_windrose_2005-2014

  (°) Wind speed (knots ) 0 5 10 15 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 61 1 68 5 71 8 71 3 42 4 28 0 28 0 32 2 28 2 21 2 21 0 28 2 43 3 61 6 65 7 53 4 55 2 50 0 54 2 49 4 39 1 41 3 42 4 44 6 43 3 35 9 29 8 21 6 16 5 22 7 18 4 15 1 18 5 22 3 24 2 40 2 Wind rose BIKF October 2005−2014 90 80 70 60 50 40 30 /media/vedur/BIKF_windrose_2005-2014.pdf

• 39. Reykholt-abstracts

  /media/vatnafar/joklar/Reykholt-abstracts.pdf

• 40. VI_2016_006_rs

  was 0.1–0.2 C and the flow was 40–50 l/s (Árni Hjartarson, 2015). The inner Efri-Botnar area is similar to the outer cirque, but the thickness of the debris appears to be somewhat greater. There are ridges and lateral glacier moraines within the cirque and the thickness of the piles of loose materials near the mouth of the cirque is around 6–8 m. Glacier striations from the end of the last ice age can /media/vedurstofan-utgafa-2016/VI_2016_006_rs.pdf