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• 21. Terms and conditions

  no authorisation is given to change data or any other information available from this web-site, unless the source and modification is stated clearly. (i.e., a description of data sourced from IMO and the subsequent changes made by others.) The Icelandic Met Office's website does not collect personally identifiable data about users. Web traffic on en.vedur.is is measured by Google Analytics, Siteimprove /about-imo/the-web/conditions

• 22. Funded MS student opportunity. Dust and ash re-suspension sources

  Formulating source term for dust and ash re-suspension for the NAME model. The MS student will work on the implementation of an emission scheme particularly apt for Icelandic land coverage and climate, and to validate the code using a past event. The MS student will:Formulate code; working on selected test cases.Do backward numerical runs for quantifying the temporal changes of areal source /about-imo/news/funded-ms-student-opportunity-dust-and-ash-re-suspension-sources-in-emission-models

• 23. Terms and conditions

  no authorisation is given to change data or any other information available from this web-site, unless the source and modification is stated clearly. (i.e., a description of data sourced from IMO and the subsequent changes made by others.) The Icelandic Met Office's website does not collect personally identifiable data about users. Web traffic on en.vedur.is is measured by Google Analytics, Siteimprove /about-imo/the-web/conditions/

• 24. 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

• 25. 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

• 26. A small jökulhlaup in Gígjukvísl

  which does not exceed high river discharge at summer. The road and bridge are safe. A small jökulhlaup The bridge across river Gígjukvísl, 27 March 2014 at 08:00, view to the WNW and the mountain in the background is Lómagnúpur. Photo: Njáll Fannar Reynisson. The river Skeiðará changed its course in 2009 and now runs due west along the margin of Skeiðarárjökull outlet glacier /about-imo/news/nr/2859

• 27. Ash plume and lightnings

  active volcano. It last erupted in 2004 and the current eruption is in a similar location. Flash floods south of the volcano often occur associated with eruptions, but can also happen in between eruptions. The latest such flood occurred in October 2010, so a big flood currently appears unlikely. The MODIS satellite picture taken around 5 o'clock this morning shows the plume; at sunrise the plume /about-imo/news/nr/2177

• 28. norsem_bryndis

  Crustal accretion along the divergent plate boundary in Iceland is governed by rifting episodes and dyking. Over a period of two weeks in August-September 2014, magma propagated laterally from the subglacial Bárðarbunga central volcano, Iceland, about 50 km along the divergent plate boundary to the NNE where it erupted continuously for six months. The dyke propagation was associated with more /media/norsem/norsem_bryndis.pdf

• 29. 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

• 30. Dyrrdal_Anita_CES_2010

  parameters – In the light of climate change Norwegian Meteorological Institute met.no Observed changes in Norway between 1961-90 and 1979-08 • Winter precipitation has increased by 5-25 % • Winter temperature has increased by 0.91–1.34 ºC (Hanssen-Bauer et al., 2009) What about snow conditions? Introduction Data & Methods Results Norwegian Meteorological Institute met.no Snow parameters Start End /media/ces/Dyrrdal_Anita_CES_2010.pdf