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Results:

• 51. 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

• 52. 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

• 53. 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

• 54. 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

• 55. VI_2020_011_en

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

• 56. Terms and conditions

  Meteorological Office's web-site: Unless stated otherwise, you are free to use data on this web-site; however, if the data are used for presentation or publication, reference must be made to the Icelandic Meteorological Office. The same stipulation applies to the graphical representation of IMO data. Unless stated otherwise, there are no restrictions on the use of IMO data, neither for private nor /about-imo/the-web/conditions

• 57. Terms and conditions

  Meteorological Office's web-site: Unless stated otherwise, you are free to use data on this web-site; however, if the data are used for presentation or publication, reference must be made to the Icelandic Meteorological Office. The same stipulation applies to the graphical representation of IMO data. Unless stated otherwise, there are no restrictions on the use of IMO data, neither for private nor /about-imo/the-web/conditions/

• 58. Protective measures

  resolution pdf for printing, 28 Mb; order free paper copies) Background for the determination of dam height in the SATSIE dam design guidelines (IMO Int. Rep. 08003, 2008, authors T. Jóhannesson, Kristín M. Hákonardóttir, C. B. Harbitz and U. Domaas) (pdf 1.0 Mb) Software for the computation of run-up of snow avalanches on catching and deflecting dams as well as on natural terrain /avalanches/imo/protective/

• 59. Workshop on Jökulhlaup Hazards

  17:30 Reception The workshop will be held at the Icelandic Meteorological Office (IMO), with attendance limited to ~20 participants due to the size of the venue. Attendance is free-of-charge and lunch will be provided; any access or dietary needs should be communicated via e-mail (see below). How to Attend If you wish to participate in the workshop, then please contact Matthew J. Roberts /about-imo/news/nr/2251

• 60. Bardarbunga_kafli20140825

  have extensive ice cover. The 2009 m high Bárðarbunga central volcano lies at the NW edge of the ice cap, with only its NW slopes ice free. It is dominated by a 80 km2 and up to 700 m deep ice-filled caldera. Bedrock rises to 1850 m in the northwest caldera rim and is lowest in a narrow gap the east rim where minimum elevation is 1350 m. The ice free fissure swarm north of Vatnajökull strikes /media/jar/Bardarbunga_kafli20140825.pdf