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• 11. VI_2022_006_extreme

  season cannot begin before March prevents untimely detection. Once the maximum is found, the first 10-day period with accumulated melting exceeding 20 mm and a median temperature above 0°C is identified and the first day of this period selected as the onset date. In the case of Búðarháls in Figure 6, the filter picked 06/04 correctly as the beginning of the melt season. The third filter /media/vedurstofan-utgafa-2022/VI_2022_006_extreme.pdf

• 12. 2010_017

  an important part of the runoff from many areas. In total, approximately 20% of runoff in Iceland originates from groundwater (Hjartarson, 1994a). In the above mentioned previous simulation of runoff map for Iceland for the period 1961– 1990, groundwater was omitted. Effects of groundwater flowing across watershed boundaries were simulated by scaling the precipitation for each watershed. On watersheds /media/ces/2010_017.pdf

• 13. Savolainen_Ilkka_CES_2010

  of authors) Two commenting reviews for the draft report Executive summary (of about 20 pages) will discussed and accepted by line by line procedure by government delegations early in 2011 1203/02/2010 Relative position within innovation chain 1303/02/2010 Book: Energy Vision 2050, VTT 2009 1403/02/2010 1503/02/2010 1603/02/2010 Total investments needed by 2050 are huge In addition to electricity /media/ces/Savolainen_Ilkka_CES_2010.pdf

• 14. Johannesson_Thomas_CES_2010

  -Vatnajökull, coupled model Ice volume, Icelandic and Swedish glaciers Runoff change, Icelandic and Swedish glaciers Retreat of Langjökull and Hofsjökull, 1990-2100 Sverrir Guðmundsson, Tómas Jóhannesson, Finnur Pálsson, Guðfinna Aðalgeirsdóttir, Helgi Björnsson, Oddur Sigurðsson, Þorsteinn Þorsteinsson Before, 1981-2000 mean After, at ~2100, DMI scenario Annual discharge, HBV/GLS models 20 25 /media/ces/Johannesson_Thomas_CES_2010.pdf

• 15. Avalanche notices on the web - an improved map

  /about-imo/news/nr/2838

• 16. Avalanche notices on the web - an improved map

  /about-imo/news/nr/2838/

• 17. Bardarbunga_Daily_status_report_290814

  Bárðarbunga update 29082014 2014-08-29 16:20 UTC Bárðarbunga update Compiled by Icelandic Met Office and University of Iceland Þórður Arason (Ed.) Based on Seismic, GPS, Hydrology, Radar, Webcam, PIREP, visual observations Eruption plume Height (a.s.l.) No plume was detected by radar (detection limit above 1 km) and webcam indicated low level gases and steam from lava fountains during the night /media/jar/Bardarbunga_Daily_status_report_290814.pdf

• 18. The weather in Iceland in 2022

  Skjaldþingsstaðir 3.8 # 13 29 -0.3 Egilsstaðir 4 0.1 19 to 20 68 -0.2 Dalatangi 4.5 0.1 24 84 -0.3 Teigarhorn 4.7 0.1 23 149 -0.2 Höfn í Hornaf. 5.4 # -0.1 Fagurhólsmýri 5.6 0.3 18 to 19 120 0.1 Vatnsskarðshólar 6.2 0.5 8 to 9 83 0.3 /about-imo/news/the-weather-in-iceland-in-2022

• 19. A minor eruption underway

  the eruption will last. The current magma is rich in MgO (8.5%) which indicates that it is from depths of around 17-20 km. There has been constant gas pollution close to the eruption site, spatially determined by local wind conditions. Gases can accumulate to life-threatening levels in certain weather conditions. There have been no indications of significant tectonic movements since the eruption /about-imo/news/earthquake-swarm-in-reykjanes-peninsula

• 20. ces-glacier-scaling-memo2009-01

  and ice caps may be derived from data about the area distribution of ice bodies in the drainage basin. Since the exponents g in the volume–area scalings v = csg for both ice caps and glaciers TóJ 3 5.12.2009 Memo Area (km2) Volume (km 3 ) 50 100 50 100 150 200 250 50 100 150 200 250 a71 a71a71 a71 a71 10 50 500 500020 1000 1 5 10 0 100 0 2 2 0 20 0 200 0 100 10000 Icelandic ice /media/ces/ces-glacier-scaling-memo2009-01.pdf