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Results:

• 31. 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

• 32. 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

• 33. 2010_016

  and the groundwater module. The coupling between both modules was done by a net boundary flux between the unsaturated zone and the groundwater (Schulla & Jasper, 2007). Information on land use, soil type, elevation and other general properties of the watershed are given in static distributed grids while a number of parameters describing specific processes are adjusted to the properties of each /media/ces/2010_016.pdf

• 34. 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

• 35. 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

• 36. 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

• 37. GA_2009_91A_4_Andreassen

  ). Meteorological observations carried out on Storbreen in the summer of 1955 (Liestøl1967) revealed that net radiation is the most impor-tant contributor to the ablation at Storbreen. An au-tomatic weather station (AWS) has bee operatedin the ablation zone of Storbreen since September2001 providing a near-continuous series of meteor- ology and surface energy balance data. Analysis ofthe first five years /media/ces/GA_2009_91A_4_Andreassen.pdf

• 38. VI_2020_005

  /media/vedurstofan-utgafa-2020/VI_2020_005.pdf

• 39. 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

• 40. Eyjafjallajokull_status_2010-04-29_IES_IMO

  km south-southwest of the eruption site at 15:00 GMT. Lightning: Four lightning strikes detected over the summit of Eyjafjallajökull between 19:47 and 20:03 GMT on 28 April. Noises: Booming sounds were reported yesterday evening, and again this morning, from Selsund, located ~40 km north-northwest of the eruption site. Additional note: 16:13 GMT: A sulphur smell was detected at 3 /media/jar/Eyjafjallajokull_status_2010-04-29_IES_IMO.pdf