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  • 21. Seismic activity around Mt. Þorbjörn has decreasing

    is to properly handle furniture and other interior objects so that they do not fall off in the event of an earthquake. The effects of an earthquake on the Reykjanes Peninsula, can be felt in a large area, and the capital area is not excluded.The Scientific Advisory Board, therefore, encourages people to check with their home and workplaces and fix unstable hanging objects. Information on earthquake /about-imo/news/seismic-activity-around-mt-thorbjorn-has-decreasing-significantly
  • 22. Icelandic climate in general

    of the Aurora Borealis on a clear night sky draws an increasing number of tourists. During summertime tourists should bring a windbreaker, rainwear, a thick pullover (wool or fleece) and sturdy walking shoes. Travellers who are camping or heading into the interior will need warm underwear and socks, rubber boots and a warm sleeping bag. During wintertime tourist should bring warm clothing, warm /climatology/iceland/nr/1268
  • 23. Icelandic climate

    pullover (wool or fleece) and sturdy walking shoes. Travellers who are camping or heading into the interior will need warm underwear and socks, rubber boots and a warm sleeping bag. During wintertime tourist should bring warm clothing, warm coat, mittens etc. Iceland has many swimming pools, usually with geothermally heated water. Hence, in either season a visitor should bring a swim suit /weather/climate_in_iceland/
  • 24. VI_2021_008

    a seismic network (see Figure 2), several stations must identify this signal before an audio alarm is set off. If enough stations within a particular filter vote, a tremor event will be detected in that bandpass filter, and the filter will be put into a triggered state. At this point, the audio alarm will be sounded in the monitoring room, and a new tremor event will be added to the tremor catalog /media/vedurstofan-utgafa-2021/VI_2021_008.pdf
  • 25. 2010_005_

    scenario, precipitation increased by 10–15% from 1961–90 to 2070–99, and by 5–10% for the lower emitting scenarios (corresponding to approximately 0.5–1% per decade). The CE project also examined RCM results for Iceland based on the HIRHAM model (Haugen and Iversen, 2006). These results showed enhanced warming over the interior of Iceland compared with the coastal zone, and a tendency for enhanced /media/ces/2010_005_.pdf
  • 26. Latest observations at Eyjafjallajökull

    days. A volcanic crater has formed in the south-western corner of the cauldron. Erupted material from the vent continues to accumulate on the flanks of the crater. The rim of the volcanic crater is ~50 m lower than the surrounding ice cauldron. Volcanic spatter was observed from the vent, with ejected lava reaching heights of 100-200 m. Unstable plumes of ash rise regularly from the vent. Lava /about-imo/news/nr/1891
  • 27. Latest observations at Eyjafjallajökull

    days. A volcanic crater has formed in the south-western corner of the cauldron. Erupted material from the vent continues to accumulate on the flanks of the crater. The rim of the volcanic crater is ~50 m lower than the surrounding ice cauldron. Volcanic spatter was observed from the vent, with ejected lava reaching heights of 100-200 m. Unstable plumes of ash rise regularly from the vent. Lava /about-imo/news/2010/nr/1891
  • 28. AnneFleig_May2010_CES

    “Regional hydrological droughts and weather types in north-western Europe “ University of Oslo Droughts WTs SummaryRelationsIntroduction Outlook Weather types (WTs) • simple, discrete characterization of the current atmospheric conditions over a region on the nominal scale; • may be based on one or several meteorological variables. • Weather type classification (WTC): the set of WTs describing /media/ces/AnneFleig_May2010_CES.pdf
  • 29. 2010_017

    measurements instead of river discharge data. The National Energy Authority has supported this work with contracts on 8 hydrological modelling and groundwater research. The model was then used to make a future projection of runoff for two watersheds in Iceland for the period of 2021–2050 (Einarsson & Jónsson, 2010). The WaSiM model (Jasper et al., 2002; Jasper & Kaufmann, 2003) was first set up /media/ces/2010_017.pdf
  • 30. Workshop on Earthquakes in North Iceland

    of Akureyri Institute of Earth Sciences, University of Iceland KAUST, King Abdullah University of Science and Technology Húsavík Academic Center Icelandic Meteorological Office Earthquake Engineering Research Centre, University of Iceland Civil Protection Department, National Commisioner of the Icelandic Police Iceland Catastrophe Insurance Husavik Academic centre Ministry of the Interior /about-imo/news/nr/2701

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