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Results:

• 21. VI_2020_005

  and CNES, n.d.; National Center for Atmospheric Research Staff, 2016; Quante and Colijn, 2016). Now, additional altimeters at different orbits perform slightly less accurate measurements up to 82 N and S (Rhein et al., 2013). These records are used to estimate sea surface changes and calculate global mean sea level, a temporal average sea level averaged over the oceans (Church, Clark, et al., 2013 /media/vedurstofan-utgafa-2020/VI_2020_005.pdf

• 22. IMO at the Arctic Circle Assembly 2017

  the USA, the European Space Agency (ESA) and China.Ingvar Kristinsson, managing director at IMO, participated in a session on the potential effects of volcanic ash clouds from Icelandic volcanoes on aviation in the Arctic airspace. In a special session on issues related to Arctic Freshwater, Halldór Björnsson and Þorsteinn Þorsteinsson contributed to a discussion on freshwater fluxes /about-imo/news/imo-at-the-arctic-circle-assembly-2017

• 23. The segmented dyke intrusion explained

  to time of occurrence and the colour code is shown at the top of the map. The earthquake locations delineate the track of the dyke intrusion from Bárðarbunga volcano to the eruption site at Holuhraun. Vertical cross sections through the crust are also shown; looking from the south (below) and east (to the right). Triangles mark the locations of seismic stations in and around the glacier. Data /about-imo/news/nr/3038

• 24. Refsgaard_etal-2007-Uncertainty-EMS

  The advantage of Monte Carlo analysis is its general appli- cability and that it does not impose many assumptions on prob- ability distributions and correlations and that it can be linked to any model code. The key limitation is the large run times for computationally intensive models and the huge amount of outputs that are not always straightforward to analyse. 4.8. Multiple model simulation Multiple model /media/loftslag/Refsgaard_etal-2007-Uncertainty-EMS.pdf

• 25. VI_2016_006_rs

  of 100–140 m a.s.l. Several debris flows are recorded in Búðará since the beginning of the 20th century. It is not clear whether the upper or lower area is the main source for these debris flows. The return time for sizeable debris flows in Búðará is around 20 years. It appears that the land- slide activity has been more frequent in the last 30 years than earlier in the 20th century. 4.5 Areas 7 /media/vedurstofan-utgafa-2016/VI_2016_006_rs.pdf

• 26. Karlsdottir-Risk_analysis_IMO_SK

  in animals  followed by death intoxicated grass Ash dispersion in the free atmosphere threat to aviation Natural Hazards – IMO’s Domestic Collaboration IMO Civil Protection Department – National Commissioner of the Icelandic Police Civil Aviation Authority ISAVIA – Air Navigation Service Provider Icelandic Maritime Administration Universities in Iceland Icelandic Road Authority Icelandic /media/loftslag/Karlsdottir-Risk_analysis_IMO_SK.pdf

• 27. Bárðarbunga 2015 - March, April, May

  to reduce risk in the area will be taken and decisions on further opening of the area will then be made. The Aviation Colour Code for Bárðarbunga was changed from orange to yellow when the eruption ended. 5 March 2015 - field trip yesterday Burn out From Holuhraun lava field 4 March 2015. The photo is taken from the central part of crater Baugur, view to the North along the crater /earthquakes-and-volcanism/articles/nr/3122

• 28. Bárðarbunga 2015 - March, April, May

  to reduce risk in the area will be taken and decisions on further opening of the area will then be made. The Aviation Colour Code for Bárðarbunga was changed from orange to yellow when the eruption ended. 5 March 2015 - field trip yesterday Burn out From Holuhraun lava field 4 March 2015. The photo is taken from the central part of crater Baugur, view to the North along the crater /earthquakes-and-volcanism/articles/nr/3122/

• 29. Bardarbunga-2015_MarchAprMay-events

  and May. New material is added to the top of the article. In combination, the monthly articles give an overview of events: August, September, October, November, December, January, February, March-April-May and the overview article (list of links). Calendar Below is a short-cut to additions in March, April and May plus an announcement 1st June. March: 2-3-4-5-9-12-16-24-26. April: 1-3-8-11 /media/jar/Bardarbunga-2015_MarchAprMay-events.pdf

• 30. Milly_etal-2008-Stationarity-dead-Science

  ), S. Solomon et al., Eds. (Cambridge Univ. Press, New York, 2007), pp. 1–18; www.ipcc.ch/press/index.htm. 5. IPCC, in Climate Change 2007: Climate Change Impacts, Adaptation and Vulnerability, Contribution of WG2 to AR4, M. L. Parry et al., Eds. (Cambridge Univ. Press, New York, 2007), pp. 1–16. 6. I. M. Held, B. J. Soden, J. Clim. 19, 5686 (2006). 7. T. P. Barnett, J. C. Adam, D. P. Lettenmaier /media/loftslag/Milly_etal-2008-Stationarity-dead-Science.pdf