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  • 1. 2010_005_

    that might be the result of the specific beginning and end dates used in these regression analyses, linear SAT trend values were also calculated for 1000 time- series with randomised beginning and end years within a 10-year range centred around the fixed beginning and end years. This analysis was repeated 10 times, and the mean values of each set of randomised trends, as well as their standard /media/ces/2010_005_.pdf
  • 2. VI_2015_005

    but are considered for climatological anal- yses only if their centre depression on the 1000 hPa geopotential height field reaches at least 20 m relative to the 24 surrounding grid points over the course of their lifetime. 7 This study is concerned with well-developed, persistent, mid- to high-latitude large-scale weather systems, rather than their early detection and tracking. Therefore, cyclones /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_005.pdf
  • 3. 2013_001_Nawri_et_al

    ] 1000 1006 1012 T0 [ C] 1 5 9 LT [K km 1] 7.1 6.3 5.1 L [K km 1] 2.6 5.7 7.9 within that part of the island with terrain up to 1000 m above mean sea level (mASL). The expo- nential decrease in pressure with height outweighs the linear decrease in temperature, leading to an effective decrease in air density with height. The standard value of 1.225 kg m 3 is therefore only appropriate at low /media/vedurstofan/utgafa/skyrslur/2013/2013_001_Nawri_et_al.pdf
  • 4. Earthquakes offshore north Iceland

    offshore north Iceland 1.10.2013 Two earthquakes reaching magnitude 3 and 3.2 occurred this morning at 06:14 and 07:41 offshore North Iceland, 10 km NW of Gjögurtá. They are a part of swarm activity which has been ongoing since September 25. Roughly 1000 /about-imo/news/nr/2757
  • 5. News

    October 2013 off shore North Iceland. Roughly 1000 earthquakes have been recorded in the swarm. Topography of seabed: Bryndís Brandsdóttir, Institute of Earth Sciences, University of Iceland. News 2023 2022 2021 2020 2019 2018 2017 /about-imo/news/bigimg/2757
  • 6. VI_2014_005

    of Brúarjökull at 866 mASL. 15 Figure 6. Absolute mean errors of SURFEX 2-m air temperature and 10-m wind speed compared with horizontally averaged station data (model minus measurements). Triangles indicated locations, where mean errors (biases) are negative. Terrain elevation contour lines are drawn at 1000 and 1500 mASL. each grid point are linearly projected onto the same heights above ground /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_005.pdf
  • 7. IMO_AnnualReport2014

    of events closely. Photo: Sigurlaug Gunnlaugsdóttir. Bárðarbunga Pálmi Erlendsson, Bergur H. Bergsson and others installing GPS and com- munication equipment. Photos: Þorgils Ingvarsson and Benedikt G. Ófeigsson. I C E L A N D I C M E T O F F I C E / A N N U A L R E P O R T 2 0 1 4 5 The magma intrusion from Bárðarbunga to the eruption site at Holuhraun and related tremor pulses /media/vedurstofan/utgafa/skyrslur/2015/IMO_AnnualReport2014.pdf
  • 8. Henriksen_Barlebo-2008-AWM_BBN-Journ_Env_Management

    improving management policies and practices by learning from the outcomes of implemented management strategies. Partici- patory integrated assessment is here a form of problem structuring for identification of gaps, ambiguity and multiple frames, confrontation, and integration of the most divergent views with respect to a given problem situation. Additional methods and tools that AM require com /media/loftslag/Henriksen_Barlebo-2008-AWM_BBN-Journ_Env_Management.pdf
  • 9. VI_2020_005

  • 10. Low level flight conditions over Iceland

    -13 FL180: 270/25-45KT, but 26015KT by the NE-coast, -29 Overview of weather systems: 1000 km S of Cape Farewell is an extensive 980 mb low. Over Greenland is a 1038 mb high. Near surface winds: N-ly or variable wind, 05-25 KT. Cloud heights/visibility/weather: BKN/OVC at 1000-2500 FT in the N-part and occasional snowshowers with poor visibility. Widely FEW/SCT and good /weather/aviation/llf-iceland/

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