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Results:

• 11. Seismic activity still great

  than those described above, have occurred in Bárðarbunga, where the activity started. This is the same pattern as during previous days. The highest magnitude during the last 24 hours was about 3.8, measured at 23:38 last night (20th August). In addition to the news Additional material on the web, now available in English, can be found through links on the long banner at the top of our front page /about-imo/news/nr/2951

• 12. Reykholt-abstracts

  University of Innsbruck, Austria 36 Michael Studinger* NASA Goddard Space Flight Center, USA 37 Guðmundur Valsson National Land Survey of Iceland 38 Christian Wever TopScan GmbH, Germany 39 Ian Willis Scott Polar Res. Inst. (SPRI), Univ. of Cambridge, UK * Video conference Lidar measurements of the cryosphere Reykholt, Iceland, June 20–21, 2013 Andreassen and others 9 Lidar measurements /media/vatnafar/joklar/Reykholt-abstracts.pdf

• 13. BIGR_windrose_2005-2014

  (°) Wind speed (knots ) 0 5 10 15 20 0 45 90 135 180 225 270 315 360 N E S W N (Number of observations for wind direction) Icelandic Met Office 02. júl. 2015 23 26 34 38 45 25 16 3 4 58 55 4 3 39 28 30 21 9 9 4 8 8 13 8 1 3 34 24 34 9 7 9 4 4 5 3 6 8 25 Wind rose BIGR March 2005−2014 90 80 70 60 50 40 30 2010360350340 330 320 310 300 290 280 270 260 250 240 230 220 210 /media/vedur/BIGR_windrose_2005-2014.pdf

• 14. Adalgeirsdottir-etal-tc-5-961-2011

  The Cryosphere, 5, 961–975, 2011 www.the-cryosphere.net/5/961/2011/ doi:10.5194/tc-5-961-2011 © Author(s) 2011. CC Attribution 3.0 License. The Cryosphere Modelling the 20th and 21st century evolution of Hoffellsjökull glacier, SE-Vatnajökull, Iceland G. Aðalgeirsdóttir1,2, S. Guðmundsson1, H. Björnsson1, F. Pálsson1, T. Jóhannesson3, H. Hannesdóttir1, S. Þ. Sigurðsson4, and E. Berthier5 /media/ces/Adalgeirsdottir-etal-tc-5-961-2011.pdf

• 15. Hare-2011-ParticipatoryModelling

  Dispatch: 02.08.11 CE: E E T 5 9 0 No. of Pages: 19 ME: 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17 18 19 20 21 22 23 24 25 26 27 28 29 30 31 32 33 34 35 36 37 38 39 40 41 42 43 44 45 46 47 48 49 50 51 52 53 54 55 56 57 Another possible driving force behind its popularity is changing legislation requiring environmental managers and policy-makers to increase stakeholder participation in their work [e.g /media/loftslag/Hare-2011-ParticipatoryModelling.pdf

• 16. BIKF_windrose_2005-2014

  observations: 13639 Calm: 1.9% Variable winds: 0.22% Average wind speed for wind direction Wind direction (°) Wind speed (knots ) 0 5 10 15 20 0 45 90 135 180 225 270 315 360 N E S W N (Number of observations for wind direction) Icelandic Met Office 02. júl. 2015 25 3 43 7 55 9 69 3 58 3 49 1 74 0 82 8 70 5 47 8 44 2 40 7 41 1 52 4 51 1 41 7 38 2 36 7 32 1 29 7 29 3 29 9 37 0 39 9 44 1 35 8 32 3 21 3 /media/vedur/BIKF_windrose_2005-2014.pdf

• 17. vanRoosmalen_etal-2009-WRR_2007WR006760

  - charge, the RMS values are calculated as in equation (8). An RMS value of 0 implies a perfect match between simulated and observed values. The RMS value increases with the discrepancy between the simulated and observed values. [38] At the downstream discharge stations of the three stream systems an average value of E = 0.81 and RMS = 1.84 m3/s was found for the validation period 1996–1999 /media/loftslag/vanRoosmalen_etal-2009-WRR_2007WR006760.pdf

• 18. Earthquakes last 48 hours

  0.501.05 12:17:2553.56.8 km NW of Grímsfjall 0.601.05 11:38:13Check.6.9 km NNW of Grímsfjall 0.301.05 11:36:41Check.7.7 km NE of Krýsuvík 0.701.05 11:31:58Check.4.6 km SE of Bárðarbunga 0.501.05 10:53:07Check.5.1 km S of Fagradalsfjall 1.001.05 09:20:04Check.3.1 km E of Flatey 0.501.05 08:53:41Check.4.8 km W of Þrengsli 0.901.05 08:35:09Check.2.4 km NE /m/earthquakes/latest

• 19. BITN_windrose_2005-2014

  (°) Wind speed (knots ) 0 5 10 15 0 45 90 135 180 225 270 315 360 N E S W N (Number of observations for wind direction) Icelandic Met Office 02. júl. 2015 12 12 12 16 23 27 32 19 23 15 8 10 13 17 24 20 7 9 21 38 36 26 24 35 22 7 6 9 11 12 19 23 13 8 6 23 Wind rose BITN May 2005−2014 90 80 70 60 50 40 30 2010360350340 330 320 310 300 290 280 270 260 250 240 230 220 210 200 190 180 /media/vedur/BITN_windrose_2005-2014.pdf

• 20. Alam_Ashraful_CES_2010

  FOREST BIOMASS FOR ENERGY PRODUCTION – POTENTIALS, MANAGEMENT AND RISKS UNDER CLIMATE CHANGE Ashraful Alam, Antti Kilpeläinen, Seppo Kellomäki School of Forest Sciences, University of Eastern Finland, Joensuu F t Cli t d R bl E I t Ri k d Ad t tiu ure Cl ma e an enewa e nergy – mpac s, s s an ap a on Oslo, Norway 2 June, 2010 Contents • Forestry in Finland • Challenges • Objectives /media/ces/Alam_Ashraful_CES_2010.pdf