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• 11. 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/

• 12. 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/

• 13. 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

• 14. 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

• 15. Horsens_breakout_12August

  are the main knowledge gaps? o How is this knowledge acquired? (new data, modelling studies, stakeholder processes, research, etc.) o What are the expected main climate change effects for this case? 2. Uncertainty o What are the main uncertainties on climate change effects? o Prepare a survey of the main uncertainties, their characteristics and describe how to deal with the different /media/loftslag/Horsens_breakout_12August.pdf

• 16. ICEWIND

  the Risø DTU National Laboratory for Sustainable Energy, the Norwegian Meteorological Institute, the University of Gotland, Statoil and the Technical Research Centre of Finland (VTT) along with many of the Nordic countries major wind energy companies. The ICEWIND's main goal is to share knowledge between the Nordic countries and identify factors that delay or prevent the adopton of wind energy /about-imo/arctic/icewind/

• 17. Earthquake sequence east of Grímsey

  Several hundruds aftershocks have been detected following the mainshock. The source region is located on a fault system that reaching from Öxarfjörður to the north of Grímsey, the so called Grímsey lineament. Another M4.7 earthquake followed this morning at 08:56 and was located about 7.5km northwest of the night's main event. Both mainshocks are shown as black stars in the map, aftershocks that have /about-imo/news/nr/2681

• 18. Travel information

  to several times a day with the the airlines Icelandair, WOW air, and Scandinavian Airlines. Icelandair offers flights to Iceland from several American cities. Prices can be compared at dohop search engine, which may offer additional airlines. There are frequent bus connections to the main bus terminal in Reykjavík, see map. The bus trip takes less than an hour. Most aircraft land in the morning /lidar/lidar-2013/travel-info/

• 19. VONA message

  (03.00 am). Currently the tremor is at very low level and the activity at the vent (as observed for cameras and visual inspections) is absent. Gas is still degassing from the main crater and high values of SO2 are still measured at the eruption site. Thermal detection from satellite images detected clear signs of activity last night when the crater was still active and abundant lava rivers were /earthquakes-and-volcanism/volcanoes/vona-notifications/

• 20. VONA message

  (03.00 am). Currently the tremor is at very low level and the activity at the vent (as observed for cameras and visual inspections) is absent. Gas is still degassing from the main crater and high values of SO2 are still measured at the eruption site. Thermal detection from satellite images detected clear signs of activity last night when the crater was still active and abundant lava rivers were /earthquakes-and-volcanism/volcanoes/vona-notifications/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/