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• 21. Lorenzoni_Pidgeon_2006

  for people to conceptualise and to relate to their daily activities, arguably because it cannot be easily translated into the language of popular culture (Ungar, 2000; see also mental models of cli- mate change by Bostrom et al., 1994; Kempton, 1997; discussed later). Secondly, the various datasets available detailing public opinions and attitudes on climate PUBLIC VIEWS ON CLIMATE CHANGE: EUROPEAN /media/loftslag/Lorenzoni_Pidgeon_2006.pdf

• 22. VI_2014_001

  flood method for deriving flood quantiles at gauged sites with limited data availability (see for in- stance Blazkova and Beven, 1997; Cameron et al., 1999; Fiorentino et al., 2007; and a review by Boughton and Droop, 2003). A distributed hydrological model calibrated on a gauged catch- ment can be used to continuously simulate discharge series at different sites on that catchment and flood /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_001.pdf

• 23. VI_2020_008

  by the Peak-over-Threshold with MLE applied on daily and 24-hour accumulated precipitation from the ICRA. ............................... 58 8 Glossary 1M5 – Daily or 24-hour precipitation return level with a 5-year return period AMS – Annual Maxima Series CC – Closeness Coefficient CDO – Climate Data Operator EVA – Extreme Value Analysis GP – Generalized Pareto ICRA – Icelandic /media/vedurstofan-utgafa-2020/VI_2020_008.pdf

• 24. VI_2014_006

  to reduce systematic biases in the flow forecasts, if any, a recursive error correction procedure which builds on the algorithm proposed by Boi (2004) is defined, assuming that dis- charge observations are available in real-time and are of good quality. The algorithm establishes a correction to be applied on predicted discharge issued at time t0, based on the error between observed and analyzed /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_006.pdf

• 25. 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 /

• 26. 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/

• 27. Staff members

  Meteorologist Service and Research Division Anton Berg Carrasco Snow avalanche observer /about-imo/employees/

• 28. Mission

  IMO has a long-term advisory role with the Department of Civil Protection and Emergency Management of the National Commissioner of the Icelandic Police and issues public alerts about impending natural hazards. The institute participates in international weather and aviation alert systems, such as London Volcanic Ash Advisory Centre (VAAC), and the Icelandic Aviation Oceanic Area Control /about-imo/mission/

• 29. News

  2008 2007 2006 Search Search string Contact IMO © Veðurstofa Íslands | Bústaðavegi 7- 9 | 105 Reykjavík | Phone 522 6000 | Fax: 522 6001 Recording 902 0600 /about-imo/news

• 30. Fagradalsfjall eruption unusual in many ways compared to other eruptions

  deformation and seismicity preceding the eruption that began 19 March 2021. a) Model of deformation 24 February – 19 March, showing horizontal displacements as arrows and vertical displacements with a colour scale. The red line shows the location of the dyke and the broken black line shows the central axis of the plate boundary b) Hourly earthquake rate (blue) and cumulative number of earthquakes /about-imo/news/fagradalsfjall-eruption-unusual-in-many-ways-compared-to-other-eruptions