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• 11. Publications 2009

  Skaftá cauldron in the Vatnajökull ice cap, Iceland Bergur Einarsson 90 pp 5,7 Mb 2009-002 A survey of active slope movements in Central-North IcelVI_2009_002rs and from satellite radar interferometry Sigurjón Jónsson 78 pp 9,2 Mb NOMEK2009 Report to the Directors of the Nordic Meteorological Services and EUMETSAT Kristín Hermannsdóttir, Mikael Hellgreen, Birgitte Knudsen, Vibeke /about-imo/publications/2009/

• 12. 16910025

  Flugskýrsla TF-SIF 30. nóvember 2010 Flug nr. 16910.025 Áhöfn: Flugstjóri Benóný Ásgrímsson Flugmaður Hafsteinn Heiðarsson Flugmaður 2 / Þjálfunarfl. Yfirstýrimaður Auðunn F. Kristinsson Stýrimaður Gunnar Örn Arnarson Stýrimaður Stýrimaður Aðrir Flugtími: Flugvöllur Hreyfing Flugtak Flugvöllur Lending Stöðvað Flugtími Blokktími Sjml. BIRK 08:31 08:35 /media/hafis/skyrslur_lhg/16910025.pdf

• 13. 2011_005

  in Appendix III. 4.2 Preferred layout of the network The Iceland CGPS network has been installed mostly through research grants of different projects with various collaborators. As a result the network coverage is uneven around the country. Areas outside of the active plate boundary have hardly any GPS stations and the network coverage is lacking for large part of the plate boundary, many /media/vedurstofan/utgafa/skyrslur/2011/2011_005.pdf

• 14. Statistical Analysis

  and Chemistry of the Earth, Special Issue: COST Action (Accepted for publication). Jónsdóttir, J. F., Uvo, C. B. & Clarke, R. T. (2008). Filling gaps in measured discharge series with model-generated series. Technical Notes. Journal of Hydrological Engineering, 13, 9, 905-909. Jónsdóttir, J. F., Uvo, C. B. & Clarke, R. T. (2008). Trend analysis in Icelandic discharge, temperature and precipitation series /ces/publications/nr/1943

• 15. Kok_and_Veldkamp_editorial_ES-2011-4160

  agreement on use of terminology. Third, all scoping papers stress that there is no silver bullet solution, with a different view on both scale and governance being appropriate depending on the specific case. Buizer et al. (2011) are strongest on this view by presenting and discussing a framework. Termeer et al. (2010) confirm that there is no best governance approach, drawing an analogue /media/loftslag/Kok_and_Veldkamp_editorial_ES-2011-4160.pdf

• 16. Warning due to violent storm

  934 mb when the low approaches the southeast coast soon after midnight and 933 mb in the northeast at 7:00 UTC tomorrow morning. Then the low continues to the north and the weather moderates. Brief forecast for the evening and the night Southeast 8 - 15 m/s or patchy sleet or snow, but mainly dry in the northeastern parts. Temperatures around zero. Rapidly increasing east- and northeast winds /about-imo/news/nr/3255

• 17. Lava flows

  in Heimaey in 1973. Heimaey is in the Vestmannaeyjar Archipelago west of Iceland and it lies within an active volcanic zone. During the eruption of 1973 a part of the town was submerged by the lava and the sailing routes to the harbour was almost closed off because of the lava flow. A world known operation to cool the advancing lava with sea water saved the harbor. Largest flood /volcanoes/volcanic-hazards/lava-flow/

• 18. Bárðarbunga 2014 - October events

  The lowest layers had a cloud ceiling of 2000 feet, the second layer between 6000-9000 and a third layer at flight level around 19000 feet. The clouds slowly dissipated to the south. The flight was directed to the northeast from Reykjavik airport, north towards Hofsjokull and Askja. A large circle was then flown around the Bárðarbunga caldera and Holuhraun. In the later part of the flight the area /earthquakes-and-volcanism/articles/nr/3011

• 19. Bardarbunga-2014_October-events

  previously been observed for several M>5 events and can not be interpreted as a decrease of the overall activity. The subsidence rate of the caldera had shortly increased around one hour after the M5.3 and is now again back to normal rates, see graph, which also is a frequent observation associated with M>5 earthquakes in Bárðarbunga. Around 20 events have been detected in the northern part /media/jar/Bardarbunga-2014_October-events.pdf

• 20. Bárðarbunga 2014 - October events

  The lowest layers had a cloud ceiling of 2000 feet, the second layer between 6000-9000 and a third layer at flight level around 19000 feet. The clouds slowly dissipated to the south. The flight was directed to the northeast from Reykjavik airport, north towards Hofsjokull and Askja. A large circle was then flown around the Bárðarbunga caldera and Holuhraun. In the later part of the flight the area /earthquakes-and-volcanism/articles/nr/3011/