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• 1. programme2---PhD-Workshop-preceding-Adaptation-Research-Conference

  with whom a slot is proposed to be swapped. In the closing session on Friday afternoon another two Workshop participants will be offered the opportunity of presenting a brief summary of key impressions and messages (2 x 5 minutes). This will require some degree of co-ordination among the rapporteurs. The Conference organizers need to know in time (Friday morning at the latest) who will present /media/loftslag/programme2---PhD-Workshop-preceding-Adaptation-Research-Conference.pdf

• 2. Lecture on abrupt changes in summer sea ice extent

  low in Arctic summer sea-ice extent, with 20% less ice area than the previous all-time record minimum of 2005 - the difference is more than 12 times the area of Iceland. This is part of a long-term trend of more than 8% ice extent decline per decade since the late seventies. Analysis of simulation results from the Community Climate System Model (CCSM3), show that the Arctic could be free of ice /about-imo/news/nr/1665

• 3. VI_2015_006

  in the late summer and early autumn of 2012 are being considered: 27 July, 3 August, and 3 September. As discussed below, these dates were associated with dif- ferent large-scale weather patterns, and characterised by different cloud conditions over Iceland. For each case, four model experiments were performed: two forecast runs, separated in start time by one day (1 and 2 days prior to the days under /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_006.pdf

• 4. TF-FMS_20141204_skyrsla

  eldgosavöktunar - samantekt ________________________________________________________ Eruption site and lava field: No major changes in the eruptive activity and the advance of the lava field have been observed. For the limited time that the vent was well visible, lava was rather surging out of the vents and only one larger bubble burst was seen. The largest outbreak of lava was seen /media/jar/TF-FMS_20141204_skyrsla.pdf

• 5. Public-Choice-2012---Teyssier---Inequity-and-risk-aversion-in-sequential-public-good-games

  movers who are averse to advantageous inequity free-ride less and reciprocate more than do others. Our results emphasize the importance of strategic uncertainty for the correct understanding of which preferences influence cooperation in social dilemmas. Keywords Inequity aversion · Risk aversion · Public good game · Conditional cooperation · Strategic uncertainty JEL Classification C72 · C91 /media/loftslag/Public-Choice-2012---Teyssier---Inequity-and-risk-aversion-in-sequential-public-good-games.pdf

• 6. 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

• 7. 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

• 8. 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/

• 9. 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

• 10. 47th Nordic Seismology Seminar

  Reykjavík, which can be booked during the registration process. Of course, participants are free to book any other accommodation on their own.Other hotelsOther hotels in walking distance from the meeting venue, Grand Hotel, are for instance:Hotel Cabin ($$) Town House Guesthouse ($)Hilton Reykjavík Nordica ($$$)Hotel Lotus ($$) Galaxy Pod Hostel ($)The above accommodation, or any other of your own /norsem/norsem2016/accomodation/