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• 21. VI_2015_006

  intensity is given as the sine of the al- titude angle. Absolute incident solar intensity at the top of the atmosphere is obtained by multiplication with 1360 W m 2. Rise [UTC] Set [UTC] Length [hrs] Noon [UTC] Altitude [deg] Intensity 27 Jul 2012 03:58 22:46 18:48 13:22 44.05 0.70 3 Aug 2012 04:22 22:21 17:59 13:22 42.32 0.67 3 Sep 2012 06:03 20:27 14:24 13:15 32.30 0.53 16 are limited to about 50 W /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_006.pdf

• 22. Bárðarbunga 2014 - December events

  a referral point in the bay, is now immersed. Photo: Ármann Höskuldsson. Míla's webcam and thermal image from a satellite confirm this north- or northwestern progression. According to the thermal image, the current magma flow also appears to be approaching the northeastern margin of the lava field but that progression is far away from the bay mentioned above. 16 December 2014 12:00 - from /earthquakes-and-volcanism/articles/nr/3055

• 23. Bárðarbunga 2014 - December events

  a referral point in the bay, is now immersed. Photo: Ármann Höskuldsson. Míla's webcam and thermal image from a satellite confirm this north- or northwestern progression. According to the thermal image, the current magma flow also appears to be approaching the northeastern margin of the lava field but that progression is far away from the bay mentioned above. 16 December 2014 12:00 - from /earthquakes-and-volcanism/articles/nr/3055/

• 24. VI_2020_004

  mainly by Civil Protection authorities, is: what might happen if this or that volcano will erupt? It is possible to constraint the expected scenario by looking into what happened in the past and learn from the volcano‘s history as an example of its possible behavior in the future. This report summarizes the results we obtained trying to answer the question: “which national level impact might /media/vedurstofan-utgafa-2020/VI_2020_004.pdf

• 25. vanRoosmalen_etal-2009-WRR_2007WR006760

  by groundwater base flow. 2.2. Geology and Hydrogeology [13] The main ice border of the Weichselian glaciation was located at the Jutland Ridge, hence the shallow geology in Western Jutland is dominated by glacial outwash sand and gravel originating from the glaciers’ meltdown. Isolated islands of Saalian sandy till are found between the outwash plains (Figure 2). The thickness of the Quaternary /media/loftslag/vanRoosmalen_etal-2009-WRR_2007WR006760.pdf

• 26. News

  News © Ólafur Freyr Gíslason Rainbow by Elliðaey - one of the Westman islands off the south coast - 14 July 2014 /about-imo/news/bigimg/3082

• 27. News

  with dust peaks in a record of measurements at Storhofdi on Heimaey, Westman Islands, off the south coast of Iceland. News 2023 2022 2021 2020 2019 2018 2017 2016 2015 2014 2013 2012 2011 /about-imo/news/bigimg/1331

• 28. News

  News © Pálmi Freyr Óskarsson Winterview from Stórhöfði, Heimaey, Vestman islands, off the south coast of Iceland /about-imo/news/bigimg/1424

• 29. Glacier change sessions at this year's Arctic Circle

  (Norðurslóðanetið) and the International Arctic Science Committee (IASC). Rapid mass-loss from Arctic glaciers Some of the largest glaciated areas on Earth are located in the Arctic and sub-Arctic regions, including Alaska, Arctic Canada, Svalbard, the Russian Arctic islands and Iceland. The Greenland Ice sheet, which is the second largest ice mass on the planet after Antarctica, is also /about-imo/news/glacier-change-sessions-at-this-year-s-arctic-circle-assembly

• 30. Lidar 2013

  together specialists from major airborne lidar campaigns, such as NASA-IceBridge and the ESA-Cryosat validation programs, regional or national glacier mapping teams using research or commercial systems, and scientists and engineers developing novel laser technologies for airborne and space use, to exchange experience and presenting novel trends in lidar developments. Scientists and engineers /lidar/lidar-2013