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• 51. News

  in Holuhraun 31 August 2014. This photo is taken 31 January 2015 of the lava field, by then closely approaching 85 square kilometers. A month later, 28 February 2015, the eruption is declared over. News 2023 2022 2021 2020 2019 2018 2017 /about-imo/news/bigimg/3097

• 52. Hazard zoning

  Hazard zoning © Morten S. Riishuus The eruptive fissure, seen from NW 28 September at 13:20. Most of the degassing /pollution-and-radiation/volcanic-gas/hazard-zoning/bigimg/3042

• 53. Warning - high winds

  Warning - high winds 20 - 28 m/s in the South and the West 24.2.2015 Bad weather is expected with poor travel conditions tomorrow, first in the south and west. Northeast wind, 5 to 13 m/s and snow showers /about-imo/news/nr/3090

• 54. Glacial outburst flood probably in progress

  in Vatnajökull is also being closely monitored (see plot 17 - 29 September), the last jökulhlaup from there having occurred in 2010. Remark 29.9.2015 at 22:28: Floodwater is beginning to drain from the eastern Skaftá ice-cauldron, located beneath Vatnajökull. According to GPS measurements, the ice-surface above the lake began to subside late on 27 September. The rate of subsidence is increasing /about-imo/news/nr/3199

• 55. Violent storm expected in the South

  Violent storm expected in the South 3.12.2015 A strong gale warning (average windspeed above 20 m/s) is effect in Iceland on Friday afternoon, and a violent storm (average wind speed, above 28 m/s) is expected in the southern /about-imo/news/nr/3242

• 56. VI_2015_005

  mean surface air temperature anomalies ....................................... 28 14 Surface air temperature anomalies over Scandinavia ...................................... 29 15 Composite mean precipitation anomalies..................................................... 30 6 1 Introduction Extratropical low-pressure systems, persisting for at least a few days, have long been recognised as one /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_005.pdf

• 57. Kok_JGEC658_2009

  to be simple and therefore has important drawbacks. Future improvements should be made in the light of applications within a larger toolbox of scenario methods.  2008 Elsevier Ltd. All rights reserved. * Tel.: +31 317 482422; fax: +31 317 419000. E-mail address: kasper.kok@wur.nl. Contents lists available at ScienceDirect Global Environmental Change journa l homepage: www.e lsev ier .com/ locate /media/loftslag/Kok_JGEC658_2009.pdf

• 58. Lorenzoni_Pidgeon_2006

  level, surveys commissioned by the European Com- munity/the European Union provide an indication of trends in concern about cli- mate change. Since 1992, such surveys have been undertaken among representative samples of citizens in its Member States, and specifically on topics related to the environment (Special Eurobarometers (EB) in 1992, 1995, 2002; and a Flash EB in 2002). These have included /media/loftslag/Lorenzoni_Pidgeon_2006.pdf

• 59. 2013_001_Nawri_et_al

  . . . . . . . . . . . . . . . . . 28 9 Weibull shape parameter at 50 and 100 mAGL for all wind directions . . . . . . . 30 10 Average wind power density based on corrected WRF model data . . . . . . . . . 33 11 Average wind power density based on NORA10 data . . . . . . . . . . . . . . . . 34 12 Differences in wind power density between northerly and southerly winds . . . . . 35 13 Directional /media/vedurstofan/utgafa/skyrslur/2013/2013_001_Nawri_et_al.pdf

• 60. Mo_Birger_CES_2010

  Simulation results Hydropower Thermal production Energy balance CO2-emissions 4 Summary and concluding remarks Sintef Energy Research Quantitative system analysis 8 of 21 Introduction Electricity system model Simulation results Summary and concluding remarks Hydropower Thermal production Energy balance CO2-emissions Annual average in ow over the year, GWh 0 14 28 42 52 0 500 1;000 1;500 2;000 2;500 /media/ces/Mo_Birger_CES_2010.pdf