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• 21. A year since the Eyjafjallajökull eruption began

  the eruption, it was necessary to hold frequent meetings with aviation authorities, flight companies, communities in the vicinity of the volcano and civil protection authorities. IMO was guided by London VAAC, one of the volcanic ash advisory centres. In September 2010, after the eruption, an Atlantic Conference on Eyjafjallajökull and Aviation was held. The Keilir Aviation Academy organized /about-imo/news/2011/nr/2164

• 22. PhD Workshop 2012

  decision support models and procedures and processes applied in analyzing, planning and implementing adaptation to climate change. Virtually all sub-themes mentioned in the Conference call, as well as many others not described, can be related to the practical uptake of adaptation. Studies, that address sectoral or regional dimensions of adaptation, are of particular interest. Character /nonam/adaption/phd-workshop-2012/

• 23. Session program Wednesday 12. October

  Infrasonic and Seismic Signatures of the 2014 Askja Landslide Giulia Barfucci, Maurizio Ripepe, Giorgio Lacanna, Emanuele Marchetti, Kristín Jónsdóttir, Kristín S. Vogfjörð 10:00 – 10:30 Coffeebreak and poster session 10:30 – 11:50 Oral session - Chair: Björn Lund 10:30 – 10:50 Calibration of a new ground motion model to earthquake strong-motion /norsem/norsem2016/program/wednesday

• 24. Jens_Christian_Refsgaard_(GEUS,_Dk)

  Refsgaard JC, van der Sluijs JP, Højberg AL, Vanrolleghem PA (2010) Uncertainty analysis in model–based water management: Better modelling practices. In: Vanrolleghem PA, Modelling Aspects of Water Framework Directive Implementation Volume 1. IWA Publishing, London, UK, 271-331. van der Keur P, Henriksen HJ, Refsgaard JC, Brugnach M, Pahl-Wostl C, DeWulf A, Buiteveld H (2008) Identification /media/loftslag/Jens_Christian_Refsgaard_(GEUS,_Dk).pdf

• 25. IPPC-2007-ar4_syr

  Approximate CO2-eq concentrations corresponding to the computed radiative forcing due to anthropogenic GHGs and aerosols in 2100 (see p. 823 of the WGI TAR) for the SRES B1, AIT, B2, A1B, A2 and A1FI illustrative marker scenarios are about 600, 700, 800, 850, 1250 and 1550ppm, respectively. d) Temperature changes are expressed as the difference from the period 1980-1999. To express the change relative /media/loftslag/IPPC-2007-ar4_syr.pdf

• 26. Evidences that Grímsvötn volcano is getting ready for

  Representatives from the Civil Protection, ISAVIA-ANS and Police Dept. of the South-Iceland also participated.An inflation started again close to GrindavíkIn mid-May deformation data (GPS and InSAR measurements) started to show again signs of inflation, suggesting that a third intrusion since the beginning of this year is occurring west of Thorbjörn. The intrusion began around mid of May /about-imo/news/evidences-that-grimsvotn-volcano-is-getting-ready-for-the-next-eruption

• 27. vonKorff_etal-2010

  played a role in this first phase as the author tables on decision analysis show. In summary, the comparison resulted in the reconstruction of 10 steps on which there appears to be considerable agreement among the five guides. 1. DA 1: Assemble a team for decision analysis as part of the participation design. Its members should belong to the lead agency, e.g., the water board, but can also /media/loftslag/vonKorff_etal-2010.pdf

• 28. ces-oslo2010_proceedings

  change over the North Atlantic and in some simulations also for Iceland. In all areas, including the North Atlantic and Iceland, a clear climate change signal compared to the spread between the simulations is seen. The standard deviation calculated from 17 of the simulations are less than 1°C in all areas apart from Iceland where it reaches between 1 and 2°C and in parts of the Barents Sea where /media/ces/ces-oslo2010_proceedings.pdf

• 29. Continued inflation around Mt. Þorbjörn

  RVIT and SYRF. Magma can accumulate for longer periods of time without an eruptionAs was already stated by the Civil Protection Scientific Advisory Board, the most likely explanation for this deformation is magma accumulation at depth. “Although we see the signs that uplift has started again, it does not mean that the events at Þorbjörn are accelerating, nor that an eruption will begin any /about-imo/news/continued-inflation-around-mt-thorbjorn

• 30. Jokull-guidlines

  mm and the distance between lines not less than 0.2 mm. Foldouts can only be accepted in exceptional cases. All illustrations should be identified lightly with a pencil on the back with the name of the author and the figure number. Formulae and algebraic symbols should be indicated clearly. Equations should be numbered sequentially. Numbers in brackets can refer to formulae /media/jar/Jokull-guidlines.pdf