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11. 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
12. 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
13. 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/
14. VI_2015_006

Meteorological Office (IMO) between 2011 and 2014. The model do- main is also the same as for the IMO operational runs, with 300 240 horizontal grid points cov- ering the whole of Iceland and parts of the surrounding ocean, and with a horizontal grid-point spacing of about 2.5 km in both directions. The model is run with the standard 65 vertical levels, and with a non-hydrostatic dynamic core /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_006.pdf
15. 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
16. Hare-2011-ParticipatoryModelling

ea th , th e m et ho d u se d at th is st ag e fo r th es e st ak eh o ld er typ es is sp ec ied .Sh oul d ther e be tw o o r mor e model sbein g develope d in th e process ,the n th e typ e o fmode lt o whic h th e metho d wa s applie d is show n in parentheses .O T re fe rs to th e co m po si tio n o ft he o rg an iz in g te am . Fo r o rg an iz in g te am in vo lve m en t in di ffe re n t pa rt /media/loftslag/Hare-2011-ParticipatoryModelling.pdf
17. 100 years of seismic observations

York collaborated in installing a seismograph network throughout Iceland, including a network of five seismographs in the interior of the country. During the same period the number of stations in the IMO network increased markedly. A new era of seismic monitoring began in Iceland in 1991, when a digital seismic system, the SIL system, was upgraded to fully automatic operation. It was designed /earthquakes-and-volcanism/conferences/jsr-2009/100_years/
18. 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
19. 2010_017

for 1961–1990 (Jónsdóttir, 2008)...................................................................................................................... 9 Figure 3 Location of the partly glacier covered watershed Austari-Jökulsá, vhm 144 (and its subcatchments vhm 167 and vhm 269), and the non-glacier covered watershed Sandá í Þistilfirði, vhm 26 /media/ces/2010_017.pdf
20. VI_2021_008

analyzes real-time data and creates an alert or warning about volcanic tremor. The most difficult aspect of creating an efficient volcanic tremor detector is isolating the desirable signals from unwanted, non-volcanic sources that can appear at multiple frequency bands and trigger the warning module. For instance, a detector for volcanic tremor should avoid triggering with storm tremor, which rises /media/vedurstofan-utgafa-2021/VI_2021_008.pdf