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Results:

• 1. programme2---PhD-Workshop-preceding-Adaptation-Research-Conference

  with whom a slot is proposed to be swapped. In the closing session on Friday afternoon another two Workshop participants will be offered the opportunity of presenting a brief summary of key impressions and messages (2 x 5 minutes). This will require some degree of co-ordination among the rapporteurs. The Conference organizers need to know in time (Friday morning at the latest) who will present /media/loftslag/programme2---PhD-Workshop-preceding-Adaptation-Research-Conference.pdf

• 2. Traffc-maintenance_expenditures

  847 2) 59 650 88 048 4) 20 165 9 582 - 8 110 161 728 322 974 636 1 244 770 2002 .. 633 847 2) 54 354 81 892 4) 19 329 9 071 - 4 853 162 705 163 966 014 1 260 860 2001 .. 542 806 2) 81 295 50 734 4) 19 889 9 000 - 5 690 141 203 48 850 666 1 132 021 2000 .. 533 629 2) 125 273 32 157 4) 23 190 6 997 - 5 332 115 674 197 842 483 1 149 476 1999 .. 526 558 2) 141 789 8 744 4) 26 555 6 463 14 403 2 827 109 /media/loftslag/Traffc-maintenance_expenditures.pdf

• 3. VI_2014_005

  reanalysis project is 37h1.2. The simulations were run on the c2a supercomputer at the European Centre for Medium Range Weather Forecasts (ECMWF). The model domain is the same as the one used for the IMO operational forecast runs (DOMAIN=ICELAND)2, with 300 240 horizontal grid points, and a horizontal grid-point spacing of about 2.5 km in both directions. HARMONIE uses a terrain-following sigma /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_005.pdf

• 4. The segmented dyke intrusion explained

  An article in Nature on the rifting event at Bárðarbunga 15.12.2014 Advanced online publication in Nature today reports research by an international team of geoscientists on the formation of the intrusive dyke which extends 45 km in the subsurface from the Bárðarbunga /about-imo/news/nr/3038

• 5. Bárðarbunga 2015 - March, April, May

  obtained are: The depth of the caldera subsidence is the same as obtained with the BARC GPS station until contact was lost in March, the maximum being 62 m. The volume of the subsidence bowl is now 1.9 km³. This is an increase of about 0.1 km³ since 3rd February. It is likely that most of this volume increase occurred in Febuary. Geothermal activity: Ice cauldrons at the SE rim /earthquakes-and-volcanism/articles/nr/3122

• 6. Bárðarbunga 2015 - March, April, May

  obtained are: The depth of the caldera subsidence is the same as obtained with the BARC GPS station until contact was lost in March, the maximum being 62 m. The volume of the subsidence bowl is now 1.9 km³. This is an increase of about 0.1 km³ since 3rd February. It is likely that most of this volume increase occurred in Febuary. Geothermal activity: Ice cauldrons at the SE rim /earthquakes-and-volcanism/articles/nr/3122/

• 7. Bardarbunga-2015_MarchAprMay-events

  surveys were conducted from TF-FMS over Bárðarbunga, after six weeks of waiting for the right weather. The results obtained are:  The depth of the caldera subsidence is the same as obtained with the BARC GPS station until contact was lost in March, the maximum being 62 m.  The volume of the subsidence bowl is now 1.9 km³. This is an increase of about 0.1 km³ since 3rd February. It is likely /media/jar/Bardarbunga-2015_MarchAprMay-events.pdf

• 8. QA on the eruption in Eyjafjallajökull 2010

  accessible. Has ash fallen in Iceland? Yes, in the southeast and extreme south of the country (downwind). Wind has been quite strong, so dry ash that fell earlier has, at times, been blowing with the wind causing local reduction of visibility. How fine is the ash? One sample taken by the Environment Agency on Mýrdalssandur (50 km away from the eruption site) after the ashfall 14-16 April /earthquakes-and-volcanism/articles/nr/1880

• 9. Kok_and_Veldkamp_editorial_ES-2011-4160

  Copyright © 2011 by the author(s). Published here under license by the Resilience Alliance. Kok, K., and T. (A.) Veldkamp. 2011. Scale and governance: conceptual considerations and practical implications. Ecology and Society 16(2): 23. [online] URL: http://www.ecologyandsociety.org/vol16/iss2/ art23/ Guest Editorial, part of a Special Feature on Scale and Governance Scale and Governance /media/loftslag/Kok_and_Veldkamp_editorial_ES-2011-4160.pdf

• 10. Daniell_etal-2010

  Copyright © 2010 by the author(s). Published here under license by the Resilience Alliance. Moellenkamp, S., M. Lamers, C. Huesmann, S. Rotter, C. Pahl-Wostl, K. Speil, and W. Pohl. 2010. Informal participatory platforms for adaptive management. insights into niche-finding, collaborative design and outcomes from a participatory process in the rhine basin. Ecology and Society 15(4): 41. [online /media/loftslag/Daniell_etal-2010.pdf