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  • 11. Bárðarbunga 2014 - September events

    geoscientist on duty Since midnight, just over 40 earthquakes have been located at Bárðarbunga and just over 30 in the intrusive dike. Especially in the dike, these are somewhat higher numbers than at the same time yesterday which could stem from the fact that it has been less windy today (as explained yesterday, high winds can blur the detection of small earthquakes). No earthquake has reached 5 in size /earthquakes-and-volcanism/articles/nr/3001/
  • 12. A new ice-cauldron in Öræfajökull volcano

    to the Icelandic Meteorological Office. The cauldron is about 1 km in diameter and it reflects a recent increase in geothermal activity within the caldera.It seems that geothermal water has been slowly released from underneath the cauldron to the glacial river of the Kvíárjökull outlet-glacier (SE flank of Öræfajökull volcano). Associated with this water release sulphur smell has been reported /about-imo/news/a-new-ice-cauldron-in-oraefajokull-volcano
  • 13. 2013_001_Nawri_et_al

    there is therefore a small positive bias of the Weibull fits compared with measurements, and a small negative bias compared with model data. Mean absolute differences are 0.10 m s 1 (0.05 m s 1) in winter (summer) for station data, and 0.15 m s 1 (0.05 m s 1) in winter (summer) for WRF model data. This amounts to 1 – 2% of the directly calculated averages. Once the two Weibull parameters have been determined /media/vedurstofan/utgafa/skyrslur/2013/2013_001_Nawri_et_al.pdf
  • 14. Grimsvotn_status_2011-05-30_IES_IMO

    Since Thursday the tremor had been intermittent. Today, Monday 30 May, it has been confirmed by the participants of Iceland Glaciological Society's spring expedition that the eruption has ended. The end of the Grímsvötn eruption is set to 7 UTC Saturday morning 28 May 2011. /media/jar/Grimsvotn_status_2011-05-30_IES_IMO.pdf
  • 15. field_report_04032015

    Field report - Holuhraun 4 March 2015 By Baldur Bergsson, Benedikt Ófeigsson, Richard Yeo, Sara Barsotti General description of the eruption site No signs of activity have been revealed. A diffuse bluish haze, at ground level, was visible across the lava field. The crater rim has several cracks at the very edge. While standing close to the crater rim it was possible to hear rumbling due /media/jar/field_report_04032015.pdf
  • 16. Activity in Bárðarbunga volcano

    Activity in Bárðarbunga volcano 16.8.2014 20:51 Seismic activity in Bárðarbunga volcano has increased. A seismic swarm has been ongoing since 03AM this morning, and near continuous earthquakes have been occurring since then. The depths of earthquakes in the present /about-imo/news/nr/2936
  • 17. Eyjafjallajokull_status_2010-05-18_IES_IMO

    measurements, web cameras, ATDnet – UK Met. Offices lightning detection system, NOAA satellite images and web-based ash reports from the public. Eruption plume: Height (a.s.l.): According to radar observations, the plume has been mostly at 7 km/21,000 ft. South and southwesterly winds (25-35 kt) over the volcano. Near the surface, the wind was easterly, blowing ash from the ground /media/jar/Eyjafjallajokull_status_2010-05-18_IES_IMO.pdf
  • 18. Eyjafjallajokull_status_2010-05-19_IES_IMO

    weather radar measurements, web cameras, ATDnet – UK Met. Offices lightning detection system, NOAA satellite images and web-based ash reports from the public. Eruption plume: Height (a.s.l.): According to radar and pilots observations, the plume has been slightly lower today than yesterday, at 5-6 km/18,000-20,000ft. Southerly winds prevailed this morning over the volcano, turning /media/jar/Eyjafjallajokull_status_2010-05-19_IES_IMO.pdf
  • 19. Preparing a merger

    of the National Energy Authority, which has been lead by Árni Snorrason since 1987. Árni Snorrason, PhD in hydrological engineering from the University of Illinois in USA in 1983, has been a lecturer at the Universities of New Hampshire and in Arizona, as well as being a leading scientist in this field in Iceland. He was selected from eleven applicants and has begun preparing the task at hand /about-imo/news/nr/1384
  • 20. Eyjafjallajokull_status_2010-05-26_IES_IMO

    : Similar as yesterday, estimated through a webcamera. But in the afternoon the visibility has been very poor caused by ash that has been blown up around the volcano. Because of this, the visibility in Vestmannaeyjar was 1 km and 2 km in Vatnsskarðshólar and the volcano could not be seen on the webcameras in the afternoon. Seismic tremor: Volcanic tremor is still more than before /media/jar/Eyjafjallajokull_status_2010-05-26_IES_IMO.pdf

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