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• 11. 100 days of gas release at Holuhraun

  rich but not as Laki in the 18th century Sara Barsotti 11.12.2014 The ongoing eruption at Holuhraun, which began in at the end of August 2014, is very rich in gas. We have to go 150 years back to find an event (Trölladyngja) that had a comparable impact on Iceland and its /pollution-and-radiation/volcanic-gas/measurements/nr/3036

• 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. 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

• 14. 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

• 15. 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/

• 16. 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

• 17. Hazard zoning

  takes place on two vents along the fissure, the northernmost part of the rampart and from the central part of the rampart. These two sources merge into one plume. Downwind, dense volcanic gases separate and descend. Further downwind a second plume, rich in water vapour, reaches higher elevation than the first plume /pollution-and-radiation/volcanic-gas/hazard-zoning/bigimg/3042

• 18. 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

• 19. VONA message

  with fountains reaching 100-150 m above the ground. These pulses are very apparent in the seismic tremor from stations in a wide area around the eruption site. Cloud height:The base of the volcanic cloud is discernible from the webcameras and it is assessed to be between 800-900 m asl. Other cloud information:The plume is gas rich and minor ash is observed. Remarks:Some gas /earthquakes-and-volcanism/volcanoes/vona-notifications/

• 20. VONA message

  with fountains reaching 100-150 m above the ground. These pulses are very apparent in the seismic tremor from stations in a wide area around the eruption site. Cloud height:The base of the volcanic cloud is discernible from the webcameras and it is assessed to be between 800-900 m asl. Other cloud information:The plume is gas rich and minor ash is observed. Remarks:Some gas /earthquakes-and-volcanism/volcanoes/vona-notifications/' link '/