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• 31. 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/

• 32. 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/

• 33. 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

• 34. 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

• 35. 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

• 36. 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

• 37. 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

• 38. 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

• 39. glacier_mass_balance_poster

  compiled by using i) aerial photographs taken between 1979 to 1984 by the American Defense Map Agency (DMA) and the Icelandic Geodetic Survey, ii) airborne EMISAR radar images obtained in 1998 by the Electromagnetic system (EMI) of the Technical University of Denmark, and iii) two image pairs from the SPOT 5 high resolution stereoscopic (HRS) instrument from 2004. The ice-free part of the EMISAR /media/ces/glacier_mass_balance_poster.pdf

• 40. VI_2020_011_en

  /media/vedurstofan-utgafa-2020/VI_2020_011_en.pdf