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• 41. VI_2022_006_extreme

  77 91 109 Hraunaveita 132 116 136 159 117 140 169 Kvíslaveita 48 42 49 58 42 51 61 Sultartangi 66 57 68 80 58 69 84 Þingvallavatn 96 84 99 117 85 102 123 Þórisvatn 47 41 49 57 42 50 60 Tungnaá 76 67 79 92 67 80 98 Ufsarlón 104 92 108 126 93 112 134 36 Figure 19 – 1M5 maps for catchment Hálslón based on the ICRA dataset without projection (top left), with RCP 2.6 and 10th percentile /media/vedurstofan-utgafa-2022/VI_2022_006_extreme.pdf

• 42. VI_Arsskyrsla_2018_vef

  - politan area to raise the awareness of climate change impacts on local scale. Agreements regarding long-term high-quality operations of weather stations have been made. Tailored services as input into the daily decision making and operations of local governments are also being discussed. IMO is undertaking broad evaluation and gap analysis of the different networks used in monitoring /media/vedurstofan/utgafa/arsskyrslur/VI_Arsskyrsla_2018_vef.pdf

• 43. Journal_of_Hydrology_Veijalainen_etal

  A second, but usually smaller, increase in runoff oc- curs in the autumn. In northern Finland more than 95% of annual maximum floods are caused by spring snowmelt (cf. Fig. 7a). Also the small upstream lakes in the northern part of the lake area and the northernmost of the coastal rivers fall mainly into this cat- egory. In most coastal rivers the major floods can be caused by either snowmelt /media/ces/Journal_of_Hydrology_Veijalainen_etal.pdf

• 44. VI_2020_004

  vedur@vedur.is Veðurstofa Íslands Bústaðavegur 7–9 108 Reykjavík Sara Barsotti, Veðurstofa Íslands Sigrún Karlsdóttir, Veðursstofa Íslands Anna María Ágústsdóttir, Landgræðslan Björn Oddsson, Almannavarnadeild Ríkislögreglustjóra Íris Marelsdóttir, Embætti landlæknis Þorvaldur Þórðarson, Jarðvísindastofnun H áskólans Þórólfur Guðnason, Embætti landlæknis Bogi B. Björnsson, Veðurstofa Íslands /media/vedurstofan-utgafa-2020/VI_2020_004.pdf

• 45. 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 /

• 46. 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/

• 47. Staff members

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

• 48. 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/

• 49. 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

• 50. 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