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• 51. VI_2013_006

  Office Guðrún Nína Petersen, Icelandic Met Office Halldór Björnsson, Icelandic Met Office   4 5 Table of contents Introduction ............................................................................................................................ 6 Lightning location data /media/vedurstofan/utgafa/skyrslur/2013/VI_2013_006.pdf

• 52. ces-oslo2010_proceedings

  5 6 Welcome to the conference “ Future Climate and Renewable Energy: Impacts, Risks and Adaptation” We welcome you to the international conference Future Climate and Renewable Energy: Impacts, Risks and Adaptation. The conference is convened by the Nordic-Baltic project Climate and Energy Systems which is funded by Nordic Energy Research, the Nordic Energy sector /media/ces/ces-oslo2010_proceedings.pdf

• 53. IMO at the Arctic Circle Assembly 2017

  at IMO, participated off-venue in a workshop on "Energy in the Arctic".Aldís Elfarsdóttir, currently working as an intern at IMO, worked with the Arctic Circle management team during the assembly, writing statements for the Arctic Circle´s social media accounts on Twitter and Facebook.More pictures from the conference and IMO sessions are online, by OZZO Photography /about-imo/news/imo-at-the-arctic-circle-assembly-2017

• 54. Update on volcanic activity in Grímsvötn

  ) of the Institute of the Earth Sciences and of the Icelandic Meteorological office was published at 16:00. After 2:20 UTC the plume has not been detectable on radar, except for a steam plume at 3:30 which reached 5 km. Eyewitnesses have reported small steam bursts from the crater today. Widespread ash in cloud layers has been detectable 5-7 km west of the volcano. Yesterday evening there was still /earthquakes-and-volcanism/articles/nr/2180

• 55. Paper-Olafur-Rognvaldsson_91

  equal to 372, and the greatest skill on Brúarjökull (ρ= 0.83; 0.0002) where the RMS er- ror is equal to 171. The correlation for Dyngjujökull is 0.61 with a significance value of 0.06 and the RMS error is equal to 286. The simulated precipitation is within estimated observational error-margins for 10 out of 12 winters for Dyn- gjujökull, 13 out of 14 for Brúarjökull and 5 out of 10 for Langjökull ice /media/ces/Paper-Olafur-Rognvaldsson_91.pdf

• 56. An

  at 23:36 yesterday evening with a magnitude (M) of 5. Two other events greater than M4 occurred early this morning at 05:46 (M4.6) and 06:23 (M4.3), respectively. In addition, 22 earthquakes greater than M3 have occurred since midnight. Felt earthquakes have been reported by local residents as far Akranes in the west and Vík in the east. The seismic swarm is still ongoing with similar /about-imo/news/an-earthquake-swarm-in-fagradalsfjall

• 57. VONA message

  .hazard_yellow { background-color: #ffff00; color: #222;} .vol_code .hazard_orange { background-color: #ffa500; color: #222;} .vol_code .hazard_red { background-color: #ff0000; color: #fff} VONA message Askja Time: 03. Sep 2021, 18:10 GMT Color code: green Volcano id: 373060 Activity summary:Unfortunately the previous VONA went out /earthquakes-and-volcanism/volcanoes/vona-notifications/

• 58. ces_wind_flyer-hq

  while the two emission scenarios A2 and B2 are quite similar. Fig. 3 The 50-year wind in 100 m height. Results from HIRHAM5 with ECHAM5 boundary condi- tions. Left graph for the middle of the century and right at the end of the century. Fig. 4 Changes in U50 in %. Left graph for the middle of the century and right at the end of the century. Partners The work in the Wind Energy group is carried out /media/ces/ces_wind_flyer-hq.pdf

• 59. Eyjafjallajokull_status_2010-05-07_IES_IMO

  recorded at 5-13 km depth, but fewer than yesterday. GPS deformation: Measurements from around Eyjafjallajökull indicate no major net discplaceaments, suggesting a stabilization of the surface deformation since yesterday. Other remarks: Grainsize analysis of samples taken of ash that fell on May 3rd at 64 km distance from the eruption site shows that about 5 % of the ash is smaller /media/jar/Eyjafjallajokull_status_2010-05-07_IES_IMO.pdf

• 60. Grimsvotn_status_2011-05-22_IES_IMO

  to 10 kilometers. Heading: Most of the ash cloud heads to the south. Lower and scattered clouds head southwest and travel over the eastern part of the South Iceland Lowlands. The plume forms a 60 km long circular cloud around the eruption site with its lower boundary at a height of about 5 km. Out from this cloud, a scattered cloud lies to the north reaching about 450 km north /media/jar/Grimsvotn_status_2011-05-22_IES_IMO.pdf