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Results:

• 21. feltvinna-JHI_2015feb_11-12

  tjörn yfir í þá nyrðri. Enn norðar er svo útfall hrauntjarnar inn í hraun. Í báðum gosopum er töluverð suða og gassprengingar. Kvikuuppstreymi er hinsvegar lítið og má greina það best á yfirfalli syðri hrauntjarnar. Enn hefur yfirborð hrauntjarnar sigið og er breidd hennar nú um 100 m. FLIR greining sýnir að kvikan er enn um 1180 til 1190 gráðu heit (°C) þegar hún kemur upp í gosopum. Það /media/jar/feltvinna-JHI_2015feb_11-12.pdf

• 22. FMI_-_Disaster_Mitigation

  Construction • Using the same method we can estimate what the reduction in damages would have been if the best construction practices were in place in all homes. • Potential damage reduction, based on this method, would have been as much as $46 million or 25% less than the permit value of $182 million Potential Economic Impact of Better Construction • Another useful comparison is to look /media/loftslag/FMI_-_Disaster_Mitigation.pdf

• 23. CES_D2.4_solar_CMIP3

  (black) and B1 (green) greenhouse gas scenarios. An unweighted mean of the responses simulated by the 18 models was used to give the best-estimate projection. To construct the probability distribution for the change, a normal distribution was fitted to the projections simulated by the various models and per- centage points were determined from this distribution. Both the best estimate projection /media/ces/CES_D2.4_solar_CMIP3.pdf

• 24. norsem_begga

  and calculated travel time differences for pairs of closely spaced earthquakes observed at a series of recording stations. Each earthquake is paired with several other earthquakes and the best fitting distances between them as a group are determined. Methods based on this kind of minimization are called double-difference (DD) earthquake location algorithms /media/norsem/norsem_begga.pdf

• 25. Group3-Road-scenarios

  but the uncertainty range is large. We are looking two cases: worst case (+4 C degrees increase) and best case (1.5 C increase). Increase in prec: more rain in the winter Decrease in the predictability of weather Natural variability ii. Socioeconomics a. Change in traffic volume b. BAU  Ten-year time steps  National main roads  Geographic area: The whole country Fig. 3 /media/loftslag/Group3-Road-scenarios.pdf

• 26. CES_D2.4_task1

  up to the year 2050, assuming best-estimate climate changes under the SRES A1B emission scenario. Changes in temperature are likely to proceed much faster in comparison with natural variability than those in precipitation. At present (2010), typically about 70% of all months are expected to be warm (above the median for 1961-1990) in northern Europe, and by the year 2050 this fraction /media/ces/CES_D2.4_task1.pdf

• 27. VI_2015_007

  ...................................................................................... 30 7 References .................................................................................................. 31 Appendix I - Identification of homogeneous groups of catchments obtained with the ROI technique and associated growth curves .............................................. 33 Appendix II - WaSiM daily flow simulations: Best run verification for the cali- bration /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_007.pdf

• 28. VI_2020_011_en

  Grain size distribution from heimaey 1973 eruption ..................................................... …64 D. Age of vents relative to best fit line ............................................................................... …65 E. Weight-bearing capacity of homes in heimaey .............................................................. …67 F. How to contextualize the probabilities given /media/vedurstofan-utgafa-2020/VI_2020_011_en.pdf

• 29. EUROVOLC – a networking project kick-off meeting

  Research Infrastructures themselvesdrive best practice at Volcano Observatories,link scientists and stakeholdersopen pathways for enterprise to better exploit georesources such as geothermal energy in volcanic areas.The project will exploit and build-upon existing and emerging national and pan-European research infrastructures, such as the ongoing European Plate Observing System (EPOS) and the recently /about-imo/news/eurovolc-a-networking-project-kick-off-meeting

• 30. VI_2013_006

  from Grímsvötn 2004 and 2011 indicate that the wind at the 500 hPa level, backtraced for 500 s gives the best results. For Eyjafjallajökull 2010 this time constant was closer to 200 s. The system has been described in posters and presentations at conferences in 2013 (Arason et al., 2013a, b; Petersen et al., 2013). 10 Review of lightning data during previous eruptions Prior /media/vedurstofan/utgafa/skyrslur/2013/VI_2013_006.pdf