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• 11. Information about the conference

  presentations will take place during the refreshment intervals. We request that posters be on display from before the opening session to the close of the conference. Each poster is allocated a display area measuring 90 cm wide by 110 cm high. Related topics /earthquakes-and-volcanism/conferences/jsr-2009/info/

• 12. Registration

  to give an oral or poster presentation, whether you intend to participate in the excursion to Langjökull on Friday afternoon, and whether you arrive on June 19 or 20. A block booking of rooms has been made at the Reykholt hotel. Potential participants are encouraged to register early due to limited number of hotel rooms. The deadline for registration was: April 15 – abstract, registration /lidar/lidar-2013/registration/

• 13. Kok_and_Veldkamp_editorial_ES-2011-4160

  agreement on use of terminology. Third, all scoping papers stress that there is no silver bullet solution, with a different view on both scale and governance being appropriate depending on the specific case. Buizer et al. (2011) are strongest on this view by presenting and discussing a framework. Termeer et al. (2010) confirm that there is no best governance approach, drawing an analogue /media/loftslag/Kok_and_Veldkamp_editorial_ES-2011-4160.pdf

• 14. Session program Wednesday 12. October

  Infrasonic and Seismic Signatures of the 2014 Askja Landslide Giulia Barfucci, Maurizio Ripepe, Giorgio Lacanna, Emanuele Marchetti, Kristín Jónsdóttir, Kristín S. Vogfjörð 10:00 – 10:30 Coffeebreak and poster session 10:30 – 11:50 Oral session - Chair: Björn Lund 10:30 – 10:50 Calibration of a new ground motion model to earthquake strong-motion /norsem/norsem2016/program/wednesday

• 15. Daniell_etal-2010

  and evaluating impacts (see also Swallow et al. 2001, van Ast and Boot 2003). METHODS AND DATA This article is based on empirical data that originated from the analysis of the participatory exercise in the Dhuenn basin. The strong involvement of researchers from two research projects (NeWater[1] and ACER[2]) linked by a joint case study led to the variety of sources available for exploration, including /media/loftslag/Daniell_etal-2010.pdf

• 16. The third CES Workshop was held at DONG Energy in Copenhagen, May 2009

  with a welcome from Dong Energy and presentations on new challenges in renewable energy and on COP 15. In the next session, PI’s of each working group presented the status of the work ending with a discussion on the progress and the implementation plan. The second day the working groups split into breakout sessions where the groups could focus on their detailed plan. In a poster session preliminary /ces/nr/1690

• 17. 47th Nordic Seismology Seminar

  on the respective day. Poster presentations (during all three coffee breaks) Tuesday 11 October Arrival and check-in. Most flights will arrive in the afternoon, so you should be at your hotel around 17:00/18:00.19:00 Kickoff party at IMO (Bústaðavegur 7, 108 Reykjavík). We will meet you at 18:30 outside Grand Hotel and walk together to IMO. Should anybody prefer to get a lift by car, please /norsem/norsem2016/program/

• 18. The third CES Workshop was held at DONG Energy in Copenhagen, May 2009

  on their detailed plan. In a poster session preliminary results of the CES project were presented. Partners CICERO, Center for Klimaforskning, Norway Denmark Meteorological Institute Ea Energianalyse A/S, Danmark /ces/nr/1690/

• 19. Call for abstracts

  July at the latest (early submissions in June) Submission deadline for final abstracts: 15 August 2010 Language: English Maximum length: 350 words, TimesRoman, 12pt The submission should include names and affiliations of all authors, plus contact information (e-mail) of corresponding author Scientific Committee Adriaan Perrels, Finnish Meteorological Institute Jens Christian Refsgaard /nonam/workshop/abstracts/

• 20. 2013_001_Nawri_et_al

  and a pressure of 1013.25 hPa. In the case of Iceland, the climate deviates significantly from these standard atmospheric conditions. Additionally, terrain elevation varies considerably across the island. Therefore, seasonal and annual differences in air density from the standard value, as well as spatial variability, need to be taken into account. Approximate air density can be calculated by assuming /media/vedurstofan/utgafa/skyrslur/2013/2013_001_Nawri_et_al.pdf