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21. Kok_et_al._TFSC_published_2011

]. There is ample experience with backcasting, and consequently much has been said about the underlying principles (e.g. [20]), the methodological 838 K. Kok et al. / Technological Forecasting & Social Change 78 (2011) 835–851 Author's personal copy framework (e.g. [8,30–32]), and practical applications (e.g. [33–35]). Also the combination between backcasting and other types of scenarios has been /media/loftslag/Kok_et_al._TFSC_published_2011.pdf

22. Bardarbunga_kafli20140825

have not been located it is not clear whether eruptions on the central part of the system belong to a central volcano or the ice covered fissure swarm. Both cases will generate jökulhlaups from rapidly melting ice. All explosive eruptions originating below ice are therefore described together. 4 4.1 Bárðarbunga central volcano and adjacent ice covered fissure swarm 1. Phreatomagmatic /media/jar/Bardarbunga_kafli20140825.pdf

23. 2011_005

in Appendix III. 4.2 Preferred layout of the network The Iceland CGPS network has been installed mostly through research grants of different projects with various collaborators. As a result the network coverage is uneven around the country. Areas outside of the active plate boundary have hardly any GPS stations and the network coverage is lacking for large part of the plate boundary, many /media/vedurstofan/utgafa/skyrslur/2011/2011_005.pdf

24. Forecast for volcanic ashfall 2010

the Volcanic Ash Advisory Centre in London. Nine Volcanic Ash Advisory Centres around the world are responsible for advising international aviation of the location and movement of clouds of volcanic ash. UK Met Office Zoomed Ash Concentration Charts: These charts supplement the official London VAAC graphics and advisories and are to be used with caution. Flight permission or restriction is shown as red /earthquakes-and-volcanism/articles/nr/1885

25. News

26. Radiation

27. Update on activity in Eyjafjallajökull 2010

not exceeded since 16 April 2010. Meltwater draining beneath the old Markarfljót bridge, ~18 km downstream from Gígjökull, had a temperature of over 11°C. The above is based on status report issued collectively by IMO and the Institute of Earth Sciences. The ash cloud will be analysed - 28 April 2010 17:45 Tomorrow and Friday, scientists from the German Aerospace Center (DLR) will do a measurement /earthquakes-and-volcanism/articles/nr/1884

28. A new banner on our web-site

A new banner on our web-site 2.10.2009 For easy promotion of projects, conferences and lectures, a new banner will appear intermittently on our web-site, at the top of each page. The banner is a link which takes the reader directly to relevant information /about-imo/news/nr/1724

29. How do you view volcanoes?

? 28.2.2017 The Icelandic Met Office and King's College London are carrying out a survey on views toward volcanoes. It has two aims: to investigate Icelanders' and tourists' views about the 2014–15 eruptions at Holuhraun, and to assess the role of volcanoes /about-imo/news/how-do-you-view-volcanoes

30. 2013_001_Nawri_et_al

and a pressure of 1013.25 hPa. In the case of Iceland, the climate deviates significantly from these standard atmospheric conditions. Additionally, terrain elevation varies considerably across the island. Therefore, seasonal and annual differences in air density from the standard value, as well as spatial variability, need to be taken into account. Approximate air density can be calculated by assuming /media/vedurstofan/utgafa/skyrslur/2013/2013_001_Nawri_et_al.pdf

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