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• 51. TF-FMS_20141204_skyrsla

  on the northern site of the lava flow, minor outbreaks were observed in the southwest close to the vents and into a lava-free part in the middle of the flow, see photo on the next page. Eruption site seen from NNW, rather calm bubbling activity. Photo: Martin Hensch EBE-035-1 Eftirlitsflug /media/jar/TF-FMS_20141204_skyrsla.pdf

• 52. 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/

• 53. 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

• 54. 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/

• 55. 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/

• 56. VI_2014_005

  and rivers), and ocean (including sea ice) (Le Moigne, 2009). SURFEX uses input from the 1Further information can be found online at http://hirlam.org/index.php/documentation/harmonie. 2In this section, expressions in parentheses refer to parameter values and settings in the config_exp.h model configuration file. 7 lowest level of the atmospheric model, together with static fields describing the model /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_005.pdf

• 57. Dataseries and components

  ), quantity (mm), pH Heavy metals in aerosol: Pb, Cd, Cu, Zn, Cr, Ni, Fe, Mn, V, As, Al (ng/m3) Cl, NO3-N, SO4-S (µg/m3) Hg (pg/m3) Persistent organic pollutants (POPs), same for precipitation (ng/l) and air (pg/m3): alfa-HCH, beta-HCH, gamma-HCH p,p'-DDE p,p'-DDD o,p'-DDT p,p'-DDT dieldrin HCB cis-chlordan, trans-chlordan, trans-nonachlor, PCB-28, -31, -52, -101, -105, -118, -138, -153, -156 /pollution-and-radiation/pollution/components/

• 58. 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

• 59. 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

• 60. 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