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Results:

• 61. Registration

  are requested to send applications before the above deadline. The applications must include a brief description of their PhD/research project and a recommendation from their supervisor supporting their participation. Please apply for participation through this link to FIVA's web-site. The applicants will be informed of the acceptance shortly after the registration deadline. Planet worth fighting /nonam/phd-summerschool/registration/

• 62. Kok_et_al._TFSC_published_2011

  l e i n f o a b s t r a c t Article history: Received 30 November 2009 Received in revised form 11 January 2011 Accepted 14 January 2011 Available online 17 February 2011 Social, natural and cultural systems are changing rapidly, influencing the future of Europe's fresh waters. One of the drivers shaping this future is the implementation of the Water Framework Directive. Participatory scenario /media/loftslag/Kok_et_al._TFSC_published_2011.pdf

• 63. 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

• 64. Factsheet_Bardarbunga_20140929

  caldera continues with slightly slower rate and is now around 40 cm pr. 24 hours.  Seismic activity in Bardarbunga continues on similar rate as the last few days. Six earthquakes bigger then M3,0 were recorded since noon yesterday. The biggest one was M5,2 at 12:34 yesterday.  Smaller earthquakes were detected in north part of the dyke and around the eruption site.  GPS measurements /media/jar/Factsheet_Bardarbunga_20140929.pdf

• 65. 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

• 66. Notes on the 2010 eruptions

  in river Hvanná, see graph. Specific weather forecast for the area. Link to satellite image (IKONOS) showing the volcanic site in 1 m resolution. An earthquake reported but tremor levels have decreased and GPS measurement show deflation, indicating that this eruption is now possibly over. 14.04.2010 Reporting new earthquake activity, location and depth. Announcing an eruption in Eyjafjallajökull /earthquakes-and-volcanism/articles/nr/2467

• 67. 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

• 68. ces-oslo2010_proceedings

  /media/ces/ces-oslo2010_proceedings.pdf

• 69. 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

• 70. Factsheet_Bardarbunga_20141001

  is similar to the last few days. Nine earthquakes greater than M3.0 were recorded since noon yesterday, the largest M4.8 at 19:24 yesterday. Fewer earthquakes are now detected in the northern part of the dyke and around the eruption site.  GPS measurements show minor, irregular movements.  No change was detected in water monitoring that cannot be explained by changing weather. Air /media/jar/Factsheet_Bardarbunga_20141001.pdf