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Results:

• 11. The final CES conference, 31 May-2 June 2010

  to exchange views and acquire information about current research of climate changes and energy issues. Altogether 31 oral presentations and 21 posters were presented at the conference, including 5 keynote presentations given by invited speakers from leading research institutes on climate and energy issues. The extended abstract volume of the presentations in PDF-form is available for download /ces/nr/1979

• 12. vonKorff_etal-2010

  played a role in this first phase as the author tables on decision analysis show. In summary, the comparison resulted in the reconstruction of 10 steps on which there appears to be considerable agreement among the five guides. 1. DA 1: Assemble a team for decision analysis as part of the participation design. Its members should belong to the lead agency, e.g., the water board, but can also /media/loftslag/vonKorff_etal-2010.pdf

• 13. A minor eruption underway

  for the aviation.Reykjanesbraut – the main road from the capital region to Reykjanesbær and the international airport at Keflavík is open. However, Suðurstrandarvegur – the road along the south coastline of Reykjanes peninsula is closed between the two coastal towns Grindavík and Þorlákshöfn. Other roads and unpaved tracks in the close vicinity of the eruption site are also closed.Updated 19.03 23:20At around 20:45 UTC today /about-imo/news/earthquake-swarm-in-reykjanes-peninsula

• 14. Climate and Modeling Scenarios

  & Ruosteenoja, K. (2009). Comparing regional risks in producing turnip rape and oilseed rape - Impacts of climate change and breeding. Acta agriculturae Scandinavica 59B:2, 129-138. doi:10.1080/09064710802022895 (http://www.ingentaconnect.com/content/tandf/sagb/2009/00000059/00000002/art00004). Pryor, S.C., Barthelmie, R.J., Clausen, N.E., Drews, M., MacKellar, N. & Kjellström, E. (2010). Analyses /ces/publications/nr/1680

• 15. VI_2021_008

  off an audio alarm. This feature is especially useful when there is an ongoing eruption (i.e. Fagradalsfjall 2021), as the stations around this eruptive area can be muted to enhance signals from other regions in Iceland. • Remove stations: Stations can be removed from the trigger calculations for all bandpass filters. Removed stations will not be accounted for in the tremor catalog /media/vedurstofan-utgafa-2021/VI_2021_008.pdf

• 16. VI_2016_006_rs

  of 100–140 m a.s.l. Several debris flows are recorded in Búðará since the beginning of the 20th century. It is not clear whether the upper or lower area is the main source for these debris flows. The return time for sizeable debris flows in Búðará is around 20 years. It appears that the land- slide activity has been more frequent in the last 30 years than earlier in the 20th century. 4.5 Areas 7 /media/vedurstofan-utgafa-2016/VI_2016_006_rs.pdf

• 17. Refsgaard_etal-2007-Uncertainty-EMS

  The advantage of Monte Carlo analysis is its general appli- cability and that it does not impose many assumptions on prob- ability distributions and correlations and that it can be linked to any model code. The key limitation is the large run times for computationally intensive models and the huge amount of outputs that are not always straightforward to analyse. 4.8. Multiple model simulation Multiple model /media/loftslag/Refsgaard_etal-2007-Uncertainty-EMS.pdf

• 18. VI_2020_005

  and CNES, n.d.; National Center for Atmospheric Research Staff, 2016; Quante and Colijn, 2016). Now, additional altimeters at different orbits perform slightly less accurate measurements up to 82 N and S (Rhein et al., 2013). These records are used to estimate sea surface changes and calculate global mean sea level, a temporal average sea level averaged over the oceans (Church, Clark, et al., 2013 /media/vedurstofan-utgafa-2020/VI_2020_005.pdf

• 19. Home-page - Icelandic Meteorological Office

  been located before. Activity in Reykjanes peninsula was less than previous week and it was quite scattered. Events north of lake Hlíðarvatn are still being located, the largest one M2.7 on April 17th. One earthquake was located in Mt. Hekla and the Hengill area near Húsmúli was more active than previous week. More /

• 20. Contact us

  Contact us You are welcome to contact us through web-form "Enquiry" below or send an email to fyrirspurnir(at)vedur.is or call tel. +354 522 6000. Is your inquiry already answered on the web? Questions regarding the results of our current monitoring and forecasting are not suitable /about-imo/contact/