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  • 31. program17012012

    K. Maack, Director General Icelandic CAA Ash measurements, experience 2010 and 2011 9:45 Eruptions in Eyjafjallajökull, Etna and Grímsvötn, airborne OPC measurements and quality assurance Konradin Weber, UAS, Düsseldorf Germany 10:15 Observations in plumes and vicinity of airports Jonas Eliasson HÍ (UI) Initial and boundary data acquisition and improvements in modelling 10:45 /media/vedurstofan/utgafa/hlidarefni/program17012012.pdf
  • 32. Poster presentations

    on Intraplate Seismicity in Central Fennoscandia Annakaisa Korja, Uski, M., Lund, B., Grigull, S., Nironen, M., E., Högdahl, K. Relative earthquake location in Southern Iceland Bergþóra S. Þorbjarnardóttir and Ingi Þ. Bjarnason This year's update on the Burträsk fault seismicity Darina Buhcheva and Björn LundThe SIL-system from an operational standpointJón Söring Communication between /norsem/norsem2016/program/poster
  • 33. Guidelines2-for-rapporteurs

    ). This can be helpful with respect to finding a common structure in presenting as well in session reporting (for which angles mentioned in the opening session statements of the Workshop participants can provide checkpoints).” Session rapporteur allocation M o n d a y 2 9 . 8 Y u a n g Z h e n g A t h a n a s i o s V o t s i s E i v i n d J u n k e r M i c h a e l L a i h o H e c to r /media/loftslag/Guidelines2-for-rapporteurs.pdf
  • 34. Statistical Analysis

    & Hannah, D.M. (2010). Regional hydrological drought in north-western Europe: linking a new Regional Drought Area Index with weather types. Hydrological Processes , 24 (in press), doi: 10.1002/hyp.7644. Fleig, A., Tallaksen, L.M., Hisdal, H., Stahl, K. & Hannah, D.M. (2009). Inter-comparison of weather and circulation type classifications for hydrological drought development. Physics /ces/publications/nr/1943
  • 35. PhD_course-Programme_26Aug2011-final

    Journal of Environmental Psychology, 26, 15-26. doi:10.1016/j.jenvp.2006.05.003 Hare M P, Krywkow J (2005) Participatory processes for the design of water storage areas. Technical report, Seecon Deutschland GmbH, Osnabrück. Seecon TR no. 01/2005 for the EU Interreg IIIB TRUST project. Short version available in electronic format. Kok K (2009) The potential of Fuzzy Cognitive Maps for semi /media/vedurstofan/PhD_course-Programme_26Aug2011-final.pdf
  • 36. Outline_for_the_case_Road_maintenance_in_a_changing_climate

    o t o - a g e n d a D e f i n e a n d i n v i t e s t a k e h o l d e r s T e c h n i c a l i n p u t a n d v i s i o n s - I n t e r n a l e x p e r t s - s t a k e h o l d e r e x p e r t s F r am e p r o b l e m - t r p s e r v i c e ( q u a l i t y ) l e v e l s - t y p e s o f s c e n a r i o s A n a l y z e p r o b l e m T e c h n i c a l i n p u t f r /media/loftslag/Outline_for_the_case_Road_maintenance_in_a_changing_climate.pdf
  • 37. Hare-2011-ParticipatoryModelling

    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 Fr am ew o rk Cr ite ria u se d M ain pu rp o se o fframewor k Participator y m od ell in g purpos e Particip ator y structur e Contro lo f ow of in for m a tio n betwee n stakeholder s Timin g of event s Participatio n mod e Mo de l typ e Participator y m et ho ds use d Actor sinvolve d (at eac h /media/loftslag/Hare-2011-ParticipatoryModelling.pdf
  • 38. 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
  • 39. Aurora and the Earth's magnetic field

    surface. As a simple scale of Aurora activity we use the Kp-index, which describes strength of variations in the magnetic field of the Earth. The Kp-index is from 0 to 9, where 0 describes minimum activity and 9 maximum. Most of the time the Kp-index is 0-3 and the highest numbers are very rare. The Kp-index is calculated as a weighted mean of K-indices from many magnetic observatories around /weather/articles/nr/2549
  • 40. Eyjafjallajökull eruption 2010 - the role of IMO

    of the volcanic behaviour, plume activity and interaction between plume and weather. For further information, a slide show from a lecture on the subject (pdf 1.4 Mb) is available. Also, other articles on the Eyjafjallajökull eruption 2010 can be read on our web-site as well as the then current news on the subject. Reference * Vogfjörð K., Jakobsdóttir S.S., Guðmundsson G.B., Roberts M.J., Ágústsson K /earthquakes-and-volcanism/articles/nr/2072

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