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  • 21. Sea ice maps from the Danish Meteorological Institute

    Institute (DMI) presents ice maps. The maps are either based on satellite images or reconnaissance flights from Greenland. Various DMI ice-maps are available on their web (see dates as links below the main map). Their latest maps are also accessible through our web: Newest map (in black and white) (pdf 0,7 Mb) Newest map (in colour) (pdf 0,7 Mb) Ice chart colour code standard (WMO 2004 JCOMM /sea-ice/sea-ice-maps/dmi/
  • 22. 47th Nordic Seismology Seminar

    September 23:59 UTC.Abstracts shall be sent in email as plain text to: ingibjorg@vedur.is For the subject line, please adhere to: "NordSem 2016 Abstract [name of main author]"Please provide the following information:TitleNames of all authors (indicate who is presenting if not first author)Affiliations of all authorsAbstract text (we do not have a restriction on the maximum number of words /norsem/norsem2016/abstract-submission/
  • 23. Sea ice in November 2009

    northwest of the Westfjords, and the one closest to shore was 89 nm NW of Barði. No main ice edge was seen in the Icelandic waters. The seaice moved southwards in the month, i.e. south by the Blosseville cost of East Greenland. IMO issued a satellite image November 23rd where the sea ice edge could be seen clearly. It was observed to be approximately 100 nm WNW of Straumnes. Easterly /sea-ice/monthly/2009/nr/2333
  • 24. News

    as white dots, 20-26 October as red dots and 23-25 October as green dots. The M5.6 event is marked as a black star. The blue circle shows the area of the cluster that was detected 23-25 October further east of the main cluster. Tectonic faults are shown as black lines. News 2023 /about-imo/news/bigimg/2561
  • 25. Horsens_breakout_12August

    1 Horsens caseBreak out groups Jens Christian Refsgaard and Hans Jørgen Henriksen, GEUS The Horsens case deals with climate change adaptation of water issues in the Horsens area. The aim of the group work is to work actively with the four topics covered during lecturing (scenario building, stakeholder involvement; risk perception/acceptability and uncertainty) in a specific case /media/loftslag/Horsens_breakout_12August.pdf
  • 26. 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
  • 27. ICEWIND

    in the Nordic countries. In Iceland the main focus has been on establishment of atlases for wind and icing as well as integration of wind power with other energy sources. A wind atlas for Iceland created under the project can now be found on IMO's Icelandic web-site (English legend). Ísvindar Alongside the cooperative Nordic project, an ongoing Icelandic project ÍSVINDAR is run, where /about-imo/arctic/icewind/
  • 28. Earthquake sequence east of Grímsey

    been manually revised so far are shown as red dots. The M5.5 mainshock is located on a north-south striking left lateral strike-slip fault, see black lines in the map. The M4.7 event around 9 am was located on a normal fault to the north-west. This cluster at about 7.5 km distance to the main cluster was most likely activated due to static stress changes induced by the M5.5 earthquake /about-imo/news/nr/2681
  • 29. Travel information

    or early afternoon leaving ample time to catch the workshop bus that departs from the main bus terminal in Reykavík at 18:00 on Wednesday 19 June arriving at Reykholt hótel, see map below, around 19:30. Those who want to rent their own car can check e.g. Avis or Europcar car rentals, or check their favourite car rental search engines. There will be a bus from Reykholt to Reykjavík on Friday /lidar/lidar-2013/travel-info/
  • 30. VONA message

    At this stage it is hard to anticipate how the activity will evolve as this might be a temporary halt in the eruption caused by changes in the feeding system/conduit. A scientific meeting will be held on Thursday next week and a new assessment will be done. IMO keeps monitoring the area carefully. Because of the lack of ash and the minor tephra emission in the atmosphere /earthquakes-and-volcanism/volcanoes/vona-notifications/

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