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• 31. 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/

• 32. GA_2009_91A_4_Andreassen

  the melt (e.g. Laumann and Reeh 1993;Braithwaite 1995). Surface energy balance mod- els compute each of the relevant energy fluxes be-tween the atmosphere and the surface and require additional meteorological measurements and ob- servations, for example cloudiness and humidity.For studies of climate sensitivity to free-atmos-phere changes, data from stations outside the gla- cier boundary layer /media/ces/GA_2009_91A_4_Andreassen.pdf

• 33. Early work and an overview of measurements

  to quantify the temperature variability by an assessment of the influence the East-Greenland sea ice on the temperature, as the variability of the sea ice off the coasts of Iceland is fairly well known back to the 17th century. He also used the earlier compilations of Finnsson and Thoroddsen of years of dearth and bounty. Climatic proxies and written sources The glaciers of Iceland are very sensitive /climatology/articles/nr/1138

• 34. Early work and an overview of measurements

  to quantify the temperature variability by an assessment of the influence the East-Greenland sea ice on the temperature, as the variability of the sea ice off the coasts of Iceland is fairly well known back to the 17th century. He also used the earlier compilations of Finnsson and Thoroddsen of years of dearth and bounty. Climatic proxies and written sources The glaciers of Iceland are very sensitive /climatology/articles/nr/1138/

• 35. 2012-Refsgaard_etal-uncertainty_climate-change-adaptation-MITI343

  and are frequently of local scope. Planned actions on the other hand are normally taken by public agencies or large private sector entities, often in anticipation of climate change and with a longer term perspective and wider spatial scope. Within planned actions we have some that consist of ‘hard’ or ‘structural’ measures (e.g. investment in physical assets) and others of ‘soft’ or ‘non-structural’ measures /media/loftslag/2012-Refsgaard_etal-uncertainty_climate-change-adaptation-MITI343.pdf

• 36. 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

• 37. 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

• 38. 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

• 39. 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

• 40. 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