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Results:

• 11. 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

• 12. Ash carried southward and east

  is about 16,000 feet, periodically up to 24,000 feet. Winds from the north carry the ash southward, where westely winds in the upper atmosphere carry it towards the east. The wind directions are not expected to change much during the next few days. Check London VAAC for further information. Click on the link "Issued graphics" above the map, and choose the most recent map. Glacial floods /about-imo/news/nr/1879

• 13. 47th Nordic Seismology Seminar

  and then click on "Registration" on top of that page (see screenshot). Conference costs are 30.000 ISK (~220€), to be paid upon registration. See details on cancellation policies on the registration page. Rooms at Grand Hotel Reykjavík can be booked during the registration process. Participants are free to book other potentially cheaper hotels in the vicinity.Conference costs include coffee /norsem/norsem2016/registration/

• 14. PhD summer school

  Center for International Climate and Environmental Research - Oslo (CICERO), Norway Finnish Environment Institute (SYKE), Finland Government Institute for Economic Research (VATT), Finland Aalto University School of Science and Technology /nonam/events/nr/1928

• 15. Hare-2011-ParticipatoryModelling

  are labelled according to the geographical area of application. Examples such as Zürich and Hase II have already been reviewed and categorized in Hare et al. (2003) and Bots and van Daalen (2008), respectively. The entire Iskar process, of which Iskar (Phase I) is a part, has been categorized by Barreteau et al. (2010). All are included in this review to provide alternative analytical perspectives /media/loftslag/Hare-2011-ParticipatoryModelling.pdf

• 16. Notes on the 2010 eruptions

  the crater, supported by lower plume (2-4 km) according to radar. MODIS satellite image shows both ash from the volcanic site and loose ash blown from the surface of Mýrdalsjökull ice cap. Comments on sound blasts, viscosity, deflation and tremors. Link to satellite image RADARSAT-2 (from the Canadian Space Agency), link to a briefing issued by WMO of frequently asked questions. 25.04.2010 – 28.05.2010 /earthquakes-and-volcanism/articles/nr/2467

• 17. Significant ground

  commenced in December 2019. The unrest is ongoing and the occurrence of additional future earthquakes is considered likely. Click here for a larger image. Here is also a useful link on how to interpret an interferogram from our colleagues at USGS. News 2023 2022 /about-imo/news/satellite-images-show-significant-ground-deformation-associated-with-earthquake

• 18. Accessibility on this web site

  To improve access to the web site, the following options, among others, are available: For blind and partially sighted users, local forecasts, weather observations and seismic information can be viewed in screen readers. All the web site's text can be viewed in a screen reader. Text can be enlarged and reduced. The background colour can be changed for partially sighted or dyslexic users /about-imo/the-web/accessibility/

• 19. Information about the conference

  for abstract submissions has been extended to 14 September. The deadline for extended abstracts is 30 October - the same day as the conference. Details about abstract submission are available via the abstract submission link. The registration fee for the conference is 5,000 ISK (30 EUR). Students can participate in the conference at the subsidised rate of 2,500 ISK (15 EUR). The registration fee /earthquakes-and-volcanism/conferences/jsr-2009/info/

• 20. Ice subsidence above eastern Skaftá cauldron

  the subsidence did not disrupt the line-of-sight for the radio link. Ice surface lowering above eastern Skaftá cauldron 2015. This graph was updated every five minutes. These measurements are funded by FutureVolc and the research funds of the National Power Company of Iceland and of the Icelandic Road and Coastal Administration. The project is run by the Icelandic Met Office with support from /hydrology/research/skafta-cauldron/