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• 11. Ved-eng-2006

  The first part of December was rather cold, but unusually warm after the seventeenth. The month was quite stormy, wind causing damage in many areas. The Eyjafjordur area in the North was hit by heavy mountain precipitation and snowmelt around the twentieth, generating flooding of roads and damaging landslides causing both loss of property and livestock. There was also extensive flooding /media/vedurstofan/utgafa/skylduskil/Ved-eng-2006.pdf

• 12. Keranen_Jaana_CES_2010

  tance ◊ energy losses hot w e ather decre ase s the lifetim e of tra nsform ers increas ing w ater capa city V ery like ly, the pro bability tha t the next decad e is w arm er is 90%. Phe nom ena 1.1 - higher te m peratures, espe cially during winter Sc en ario 1. war mer clim ate Conseque nce categ ory acc ording to own ra nking Lik elihood according to own rank in g Th e op /media/ces/Keranen_Jaana_CES_2010.pdf

• 13. VI_2021_008

  off an audio alarm. This feature is especially useful when there is an ongoing eruption (i.e. Fagradalsfjall 2021), as the stations around this eruptive area can be muted to enhance signals from other regions in Iceland. • Remove stations: Stations can be removed from the trigger calculations for all bandpass filters. Removed stations will not be accounted for in the tremor catalog /media/vedurstofan-utgafa-2021/VI_2021_008.pdf

• 14. IM_flyer

  Climate and Energy Systems, 2007-2010. Information Management http://www.os.is/ces The Information management group is responsible for information dissemination, active stakeholder involvement and the public outreach. At the national level, CES-national groups will be established to secure national collaboration between the activities. All participants in the CES project have access /media/ces/IM_flyer.pdf

• 15. Factsheet-Bardarbunga-140905

  fissures are substantially smaller than in the older fissure. Steam and gas rises in a south eastern direction from the fissure. o The cauldron in Dyngjujökull seems to have grown deeper since the last observation. o No changes are visible in Bárðarbunga.  Substantial amounts of SO2 are still being released to the atmosphere in association with the eruption.  Conductivity measurements show /media/jar/Factsheet-Bardarbunga-140905.pdf

• 16. The weather in Iceland 2006

  was registered 1494 hrs, 226 above the 1961-1990 normal, the excess was mainly present during the spring. In Akureyri the bright sunshine hours were 1034, slightly below the 1961-1990 normal. Teigarhorn in Berufjörður Figure 1. Teigarhorn in Berufjörður on the east coast on a summer day in August. © Sigvaldi Árnason. The highest temperature of the year in the country was measured /about-imo/news/2007

• 17. The weather in Iceland 2006

  was registered 1494 hrs, 226 above the 1961-1990 normal, the excess was mainly present during the spring. In Akureyri the bright sunshine hours were 1034, slightly below the 1961-1990 normal. Teigarhorn in Berufjörður Figure 1. Teigarhorn in Berufjörður on the east coast on a summer day in August. © Sigvaldi Árnason. The highest temperature of the year in the country was measured /about-imo/news/2007/

• 18. The weather in Iceland 2006

  was registered 1494 hrs, 226 above the 1961-1990 normal, the excess was mainly present during the spring. In Akureyri the bright sunshine hours were 1034, slightly below the 1961-1990 normal. Teigarhorn in Berufjörður Figure 1. Teigarhorn in Berufjörður on the east coast on a summer day in August. © Sigvaldi Árnason. The highest temperature of the year in the country was measured /about-imo/news/nr/1206

• 19. The weather in Iceland 2006

  was registered 1494 hrs, 226 above the 1961-1990 normal, the excess was mainly present during the spring. In Akureyri the bright sunshine hours were 1034, slightly below the 1961-1990 normal. Teigarhorn in Berufjörður Figure 1. Teigarhorn in Berufjörður on the east coast on a summer day in August. © Sigvaldi Árnason. The highest temperature of the year in the country was measured /about-imo/news/nr/1206/

• 20. Program

  Discuss all the aspects and make summary report 15:15 - 15:45 break 15:45 - 16:30 plenary discussion based on break out session summaries 17:00 - 22:00 Excursion and dinner to The Settlement Centre in Borgarnes Day two: 27 August 2010 9:00 p7 Asbjörn Aaheim (CICERO, Norway).- Exploring reasons why the risks of natural hazards seem to be ignored 9:30 p8 Gyrite Brandt (Local Government /nonam/workshop/program/