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  • 21. Nordic Seismology Seminar in Iceland

    Thursday evening. Those who are interested in attending, are encouraged to apply for participation.The deadline for registration is 31 August. The abstract submission deadline is 15 September. The venue is Grand Hotel Reykjavík. Rooms have been reserved and can be booked through the registration process, although participants are of course free to book other accommodation.Wide range /about-imo/news/nordic-seismology-seminar-in-iceland
  • 22. Glacier mapping – IPY

    km², since some ice-free areas outside the ice caps are included, and also some areas have been measured twice for research and quality assurance purposes. Comparable digital elevation models of glaciers in Iceland have hitherto not been available. The new models will serve as a baseline for comparison with all other measurement, past and future. With repeated measurements it is possible /about-imo/arctic/glacier-mapping-IPY/
  • 23. Registration

    In the registration mail please send your name and e-mail, name of the institution where you work or study, and dates of arrival and departure. Participation, including 2 lunches and a dinner, is free of charge. Participants, other than speakers, have to cover travel and hotel costs themselves. Approaching Reykjavík Recreation park Heiðmörk and Reykjavík in background. Photo: Guðrún Pálsdóttir /nonam/workshop/registration/
  • 24. Refsgaard_etal-2007-Uncertainty-EMS

    BIOMATH, Ghent University, Gent, Belgium d Water Quality Modelling modelEAU, University Laval, Quebec, Canada Received 20 December 2005; received in revised form 5 February 2007; accepted 7 February 2007 Available online 27 April 2007 Abstract A terminology and typology of uncertainty is presented together with a framework for the modelling process, its interaction with the broader water /media/loftslag/Refsgaard_etal-2007-Uncertainty-EMS.pdf
  • 25. IMO at the Arctic Circle Assembly 2017

    at IMO, participated off-venue in a workshop on "Energy in the Arctic".Aldís Elfarsdóttir, currently working as an intern at IMO, worked with the Arctic Circle management team during the assembly, writing statements for the Arctic Circle´s social media accounts on Twitter and Facebook.More pictures from the conference and IMO sessions are online, by OZZO Photography /about-imo/news/imo-at-the-arctic-circle-assembly-2017
  • 26. 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
  • 27. NONAM conference in August

    or Workshop in Reykjavík. Participation, including 2 lunches and a dinner, is free of charge. Participants, other than speakers, have to cover travel and hotel costs themselves. Participants are invited to bring a poster of their projects. Abstracts for posters are to be submitted before 1st July to hanna.virta@fmi.fi. Notification of acceptance is given in early July. Guidelines: maximum /nonam/news/nr/1932
  • 28. 2013_001_Nawri_et_al

    values. For Part 2, data files describing the local wind statistics on the regular model grid covering Iceland are made available through an online wind atlas (follow the link from http://www.vedur.is/vedur/vedurfar/vindorka/). The files contain estimates of Weibull parameters at each grid point, for twelve wind direction sectors, five heights (10, 25, 50, 100, 200 m above ground level (mAGL /media/vedurstofan/utgafa/skyrslur/2013/2013_001_Nawri_et_al.pdf
  • 29. Crochet_Philippe_CES_2010

    (Svartá), North (ice free) Snowmelt rateSurface ru ff (snowmelt + rain) Discharge VHM-144 (Austari-Jökulsá), central N, glacier covered Snow and ice melt rates ∆timing Surface runoff (snowmelt + glacial melt + rain) All years 1971-2000 25% coldest 25% warmest ∆Qpeak % Change in average daily discharge in coldest and warmest years relative to 1971-2000 Ice free North D+S VHM-10 VHM-19 VHM-26 /media/ces/Crochet_Philippe_CES_2010.pdf
  • 30. Lorenzoni_Pidgeon_2006

    % designated responsibility onto scientists. Interestingly, 27.8% of respondents maintained individuals were responsible, while 23.7% ascribed re- sponsibility to environmental agencies, and only 3.3% to the media. We have seen this may be as a result of a combination of perceived low individual efficacy (e.g. problem of free-riders), a desire for institutional accountability (e.g. Hinchliffe, 1996 /media/loftslag/Lorenzoni_Pidgeon_2006.pdf

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