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• 11. The weather in Iceland 2013

  at Skaftafell in the Southeast. The following day, the precipitation was 153.4 mm – a total of 307.5 mm in 48 hours. At the automatic station at Kvísker in the same area the highest 24-hour precipitation total was 176.3 mm, but the two day total was not quite as high as in Skaftafell. The number of days with precipitation measuring 1.0 mm or more was 161 in Reykjavík, 13 days above the average /weather/articles/nr/2824

• 12. ved-eng-2013

  The following day, the precipitation was 153.4 mm – a total of 307.5 mm in 48 hours. At the automatic station at Kvísker in the same area the highest 24-hour precipitation total was 176.3 mm, but the two day total was not quite as high as in Skaftafell. The number of days with precipitation measuring 1.0 mm or more was 161 in Reykjavík, 13 days above the average. In Akureyri such days were 112, 9 days /media/vedurstofan/utgafa/skylduskil/ved-eng-2013.pdf

• 13. The weather in Iceland 2010

  was amongst the driest ever in the south- and west parts of the country. The annual sum in Reykjavík, 592.3 mm is the second lowest registered. The precipitation measurements in Reykjavík started in 1884 but there is a gap in the series from 1907 to 1920. During that time the years 1915, 1916 and 1917 were very dry in the area. The precipitation in Reykjavík was below the average in all months /about-imo/news/2011/nr/2112

• 14. The weather in Iceland 2010

  was amongst the driest ever in the south- and west parts of the country. The annual sum in Reykjavík, 592.3 mm is the second lowest registered. The precipitation measurements in Reykjavík started in 1884 but there is a gap in the series from 1907 to 1920. During that time the years 1915, 1916 and 1917 were very dry in the area. The precipitation in Reykjavík was below the average in all months /about-imo/news/nr/2112

• 15. ved-eng-2010

  Precipitation Precipitation gauge with windshield at IMO's grounds in Reykjavík. Photo by Jón Gunnar Egilsson, 15 September 2010. Precipitation The year was amongst the driest ever in the south- and west parts of the country. The annual sum in Reykjavík, 592.3 mm is the second lowest registered. The precipitation measurements in Reykjavík started in 1884 but there is a gap in the series /media/vedurstofan/utgafa/skylduskil/ved-eng-2010.pdf

• 16. Program

  Operation IceBridge: using instrumented aircraft to bridge the observational gap between ICESat and ICESat-2 laser altimeter measurements Michelle Hofton, B. Blair, D. Rabine and S. Luthcke, Dept of Geographical Sciences, University of Maryland, USA. Using NASA's LVIS wide-swath, full-waveform laser altimeter system to precisely and accurately image ice surfaces from high altitude Video discussion /lidar/lidar-2013/program/

• 17. 2010_003rs

  /media/vedurstofan/utgafa/skyrslur/2010/2010_003rs.pdf

• 18. BIIS_windrose_2005-2014

  (Number of observations for wind direction) Icelandic Met Office 02. júl. 2015 28 6 85 3 223 1 339 5 367 0 315 2 161 9 89 4 34 6 11 7 18 7 9 7 7 7 15 9 8 7 7 2 14 9 7 4 22 6 36 9 69 6 148 3 183 1 148 5 96 9 45 1 21 1 9 3 7 8 2 0 1 7 2 4 1 2 1 6 7 3 11 6 Wind rose BIIS January 2005−2014 90 80 70 60 50 40 30 2010360350340 330 320 310 300 290 280 270 260 /media/vedur/BIIS_windrose_2005-2014.pdf

• 19. Kok_and_Veldkamp_editorial_ES-2011-4160

  using insights from the political sciences. Veldkamp et al. (2011) discuss scale from a geographical/ecology perspective, but the focus is on bridging the gap toward economic governance. Termeer et al. (2010) provide a broad overview of different types of governance, treating scale from a multilevel governance perspective. There are a number of interesting similarities between the three scoping /media/loftslag/Kok_and_Veldkamp_editorial_ES-2011-4160.pdf

• 20. Kok_2-scenarios-lecture-2

  - Brazil Crimea - Ukraine Participatory FCMs – group model building Lower Tisza - Hungary Lake Peipsi - Estonia Participatory FCMs – dynamic output -2 -1.5 -1 -0.5 0 0.5 1 1.5 sta rt ve cto r loo p4 loo p8 loo p1 2 loo p1 6 loo p2 0 loo p2 4 loo p2 8 loo p3 2 loo p3 6 loo p4 0 loo p4 4 loo p4 8 C0; population C1; awareness C2; gap demand&supply C3; water quality C4; agriculture (intensive) C5; freq /media/loftslag/Kok_2-scenarios-lecture-2.pdf