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Results:

• 11. Paper-Olafur-Rognvaldsson_92

  in reasonable agreement. This is partly due to a compensation of the errors on a shorter timescale (days). Probability of false alarms (model predicts precipitation, but none is observed) is highest in N-Iceland, particularly during win- ter. The probability of missing precipitation events (precipitation ob- served but none is predicted by the model) is highest in the summer inland in N-Iceland. Secondly /media/ces/Paper-Olafur-Rognvaldsson_92.pdf

• 12. GA_2009_91A_4_Andreassen

  Reconstruction of mass balance prior to 1949The mass balance of Storbreen prior to 1949 wasmodelled using bw-m2 (Psolid when Tair < 3°C in win-ter) and bs-m1. Reconstructed specific mass balanceover 1923/24–1948/49, representing 25 mass bal- ance years, shows highly negative summer balanc- es (Fig. 7). The resulting cumulative mass deficit is c. –30 m w.e., nearly twice as much as for the 58year period 1949 /media/ces/GA_2009_91A_4_Andreassen.pdf

• 13. 2010_016

  Mean monthly temperature for Sandá í Þistilfirði (vhm 26), 1961–2005. Month Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec Win Sum Year Mean MM5 [C°] -3.2 -3.1 -3.2 -1.6 1.8 5.8 8 7.5 4.3 1.2 -1.7 -3.1 -3.1 7.1 1.1 Mean obs. [C°] -4.3 -4.1 -3.8 -1.6 1.8 5.4 7.4 7.1 3.9 0.5 -2.5 -4.1 -4.1 6.6 0.5 Difference 1.1 1.0 0.6 0.0 0.0 0.4 0.6 0.4 0.4 0.7 0.8 1.0 1.0 0.5 0.6 Figure 3 /media/ces/2010_016.pdf

• 14. 2010_017

  ith a broke ere correc a arose wh peratures ures were a le 4 and Fi Jökulsá wat most prono lace in war vation grad ause the ad hold. Adde uch less pr 1–2005. Win Sum -3.1 7.1 -4.1 6.6 1.0 0.5 ndá í Þist n red curv ted to fit th en calibrat to the inter lso system gure 6. ershed (see unced for t m events a ient for th dition of a d unrealis onounced t Year 1.1 0.5 0.6 ilfirði e /media/ces/2010_017.pdf

• 15. NONAM_1st_workshop_summary_v3

  organization. The group went on discussing a next step: 2. Create common vision. The group here found that this would require a merging of the two loops, the regular cycle with the learning cycle. Task could be: (i) call everybody in and let them explore their visions about the area; playground, (ii) identify basic points of views and representatives, (iii) discover different win-win solutions /media/vedurstofan/NONAM_1st_workshop_summary_v3.pdf

• 16. News

  2015. For an updated graph, see link in main text. News 2023 2022 2021 2020 2019 2018 2017 2016 2015 2014 2013 2012 2011 2010 2009 2008 2007 2006 /about-imo/news/bigimg/3203

• 17. Radiation

  Radiation © Veðurstofa Íslands An example of a graph showing UV-index for a single day. See life link in text /pollution-and-radiation/radiation/bigimg/1215

• 18. A new banner on our web-site

  A new banner on our web-site 2.10.2009 For easy promotion of projects, conferences and lectures, a new banner will appear intermittently on our web-site, at the top of each page. The banner is a link which takes the reader directly to relevant information /about-imo/news/nr/1724

• 19. VI_2015_005

  to fluctuations in atmospheric vari- ables that are not directly linked to local MSLP changes. Orographic effects on the interaction between MSLP and precipitation fluctuations are found over the western half of Greenland, where correlation between MSLP and precipitation in win- 12 Figure 5. Coefficient of determination, with the sign of correlation, between mean sea level pressure and the zonal /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_005.pdf

• 20. Ash carried southward and east

  is about 16,000 feet, periodically up to 24,000 feet. Winds from the north carry the ash southward, where westely winds in the upper atmosphere carry it towards the east. The wind directions are not expected to change much during the next few days. Check London VAAC for further information. Click on the link "Issued graphics" above the map, and choose the most recent map. Glacial floods /about-imo/news/nr/1879