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• 31. Bárðarbunga - decay of seismic activity

  the cumulative seismic moment release per week (blue dots), i.e. the sum of the moment of all earthquakes in the respective week, in the left panel for the caldera and in the right panel for the dyke intrusion. The red line marks the onset of the eruption and the zero point is the beginning of the earthquake swarm on 16 August 2014. The last data point shows the current week (might still rise). Note /earthquakes-and-volcanism/articles/nr/3083

• 32. Huntjens_etal-2010-Climate-change-adaptation-Reg_Env_Change

  to determine a global figure for economic impact (From: EM-DAT 2008). 4 Based on baseline assessments of the case-studies in the NeWater- project (http://www.newater.info). 264 P. Huntjens et al. 123 these case-studies, more specifically in their level of AIWM.5 Therefore, this paper intends to identify differ- ences and similarities in AIWM, to detect general patterns, and to compare measures being /media/loftslag/Huntjens_etal-2010-Climate-change-adaptation-Reg_Env_Change.pdf

• 33. “The small eruption” in

  and deformation may precede many eruptions this is not always the case and depends on how much stress has already been released and the strength of the upper crust”, says Michelle.Figure 2. A) GPS data from the station KRI in Krísuvík. The blue line indicates the beginning of the eartquake swarm (24.02) and the red line shows the beginning of the eruption (19.03). A rapid deformation was detected /about-imo/news/the-small-eruption-in-fagradalsfjall-celebrates-six-months

• 34. “The small eruption” in

  and deformation may precede many eruptions this is not always the case and depends on how much stress has already been released and the strength of the upper crust”, says Michelle.Figure 2. A) GPS data from the station KRI in Krísuvík. The blue line indicates the beginning of the eartquake swarm (24.02) and the red line shows the beginning of the eruption (19.03). A rapid deformation was detected /about-imo/news/the-small-eruption-in-fagradalsfjall-celebrates-six-months/

• 35. VI_2016_006_rs

  in Seyðisfjörður VÍ 2016-006 ISSN 1670-8261 Report +354 522 60 00 vedur@vedur.is Veðurstofa Íslands Bústaðavegur 7–9 108 Reykjavík Daniel Illmer, Ingenieurbüro Illmer Daniel e.U. Jón Kristinn Helgason, Icelandic Met Office Tómas Jóhannesson, Icelandic Met Office Eiríkur Gíslason, Icelandic Met Office Sigurjón Hauksson, Efla Consulting Engineers 5 Abstract Evaluation and interpretation /media/vedurstofan-utgafa-2016/VI_2016_006_rs.pdf

• 36. 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

• 37. Past temperature conditions in Iceland

  Figure 5. Spring temperature (April and May) in Stykkishólmur. The red line corresponds to a linear trend of about 0.7°C per century. The temperature variations in the spring (April and May) are similar in timing to the winter. The 1840s had the warmest spring temperatures in the 19th century corresponding to a minimum extent of sea ice at that time. This was followed by a very /climatology/articles/nr/1213

• 38. Past temperature conditions in Iceland

  Figure 5. Spring temperature (April and May) in Stykkishólmur. The red line corresponds to a linear trend of about 0.7°C per century. The temperature variations in the spring (April and May) are similar in timing to the winter. The 1840s had the warmest spring temperatures in the 19th century corresponding to a minimum extent of sea ice at that time. This was followed by a very /climatology/articles/nr/1213/

• 39. Reykholt-abstracts

  and Gareth Rees Scott Polar Research Institute (SPRI), University of Cambridge, UK Calculation of glacier velocity from repeat lidar survey Lidar measurements of the cryosphere Reykholt, Iceland, June 20–21, 2013 5 Tómas Jóhannesson Icelandic Meteorological Office, Iceland Flow paths of subglacial water detected by lidar measurements of changes in the ice surface elevation of glaciers /media/vatnafar/joklar/Reykholt-abstracts.pdf

• 40. Jökulhlaup from Grímsvötn subsides

  that previously flowed into the Skeiðará river breached this sediment bank in 2009, leading to the start of meltwater flow along the margin and into Gígjukvísl. Photo: Þorsteinn Þorsteinsson. Figure 5 shows the location where the greatest amount of upwelling of water was observed and Figure 6 shows a scientist measuring the water temperature at this site. Earlier data from the subglacial lake /about-imo/news/2010/nr/2042