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• 21. Water_resources_man_Veijalainen_etal

  range 90% 93.15–93.29 93.27–93.36 75.43–75.56 94.59–94.71 2040–2069 range 90% 93.09–93.31 93.28–93.40 75.41–75.56 94.72–94.83 2070–2099 range 90% 93.02–93.32 93.24–93.43 75.38–75.61 94.79–94.91 Lowest water level (in the 30 year period) (m) Reference period 92.86 92.72 75.20 94.27 2010–2039 range 90% 92.62–92.91 92.96–93.13 75.24–75.33 94.47–94.59 2040–2069 range 90% 92.55–92.82 92.88–93.12 75.19 /media/ces/Water_resources_man_Veijalainen_etal.pdf

• 22. 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

• 23. 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

• 24. VI_2015_007

  of Iceland, Science Institute, University of Iceland, and National Energy Authority. 2004), a soil map from the Agricultural University of Iceland and a vegetation map from the Icelandic Institute of Natural history were also used in this study. 8 Table 1. Main characteristics of river basins used in this study. Catchment Name Area Mean Mean annual Available period / (km2) elevation precipitation /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_007.pdf

• 25. VI_2020_011_en

  particles formed as the magmatic gases age (most notably, SO4 aerosol is formed from SO2 gas), and from tephra particles (the finest ash can be breathed in, and the acidic coatings on tephra particles can acidify and pollute fresh water). One person died due to CO2 accumulation in a basement during the 1973 Eldfell eruption. During the eruption, rescue 22 workers needed to be aware of escape /media/vedurstofan-utgafa-2020/VI_2020_011_en.pdf

• 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