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• 21. CES_D2.4_VMGO

  size. References 1. Meehl, G.A., C. Covey, T. Delworth, M. Latif, B. McAvaney, J.F.B. Mitchell, R.J. Stouffer and K.E. Taylor, 2007: The WCRP CMIP3 Multimodel Dataset: A New Era in Climate Change Research, BAMS, 88, 1383-1394, DOI: 10.1175/BAMS-88-9-1383. 2. Naki �enovi � N., J. Alcamo, G. Davis, B. de Vries, J Fenhann, S. Gaffin, K. Gregory, A.Grübler, T.Y. Jung, T. Kram, E.L. La Rovere /media/ces/CES_D2.4_VMGO.pdf

• 22. PhD_course-Programme_26Aug2011-final

  Christian Refsgaard, GEUS All week AP Adriaan Perrels, FMI All week SK Sigrún Karsldóttir, IMO All week FU Frederik Uldal, University of Copenhagen Logistic support Course material Papers and book chapters - recommended reading Henriksen HJ, Barlebo HC (2008) Reflections on the use of Bayesian belief networks for adaptive management. Journal of Environmental Management, 88, 1025- 1036. doi:10.1016 /media/vedurstofan/PhD_course-Programme_26Aug2011-final.pdf

• 23. The weather in Iceland in 2021

  station total mm 1991-2020% 2011-2020 % max 24-hr mm prec.days >=1.0 mm Reykjavík 765.3 87 82 18.6 232 150 Stykkishólmur 675.7 92 88 29.9 211 124 Hólar í Dýrafirði 1237.3 # 105 112 235 132 Litla-Ávík 836.2 # 92 45.7 225 145 Skeiðsfoss 915.6 94 /about-imo/news/the-weather-in-iceland-in-2021

• 24. BIGJ_windrose_2005-2014

  direction (%) Aerodrome Total observations: 88 Calm: 1.1% Variable winds: 0% Average wind speed for wind direction Wind direction (°) Wind speed (knots ) 0 5 10 15 20 0 45 90 135 180 225 270 315 360 N E S W N (Number of observations for wind direction) Icelandic Met Office 02. júl. 2015 5 5 4 7 13 7 5 1 1 1 1 2 2 4 2 2 4 7 1 2 1 8 2 Wind rose BIGJ June /media/vedur/BIGJ_windrose_2005-2014.pdf

• 25. vonKorff_etal-2010

  /media/loftslag/vonKorff_etal-2010.pdf

• 26. VI_2022_006_extreme

  towards the northern part of Vatnajökull. Table 8 – Median 1M5 values (mm 24-h-1) for eleven hydropower catchments with and without climate projections for the period 2080 – 2100. Catchment 1M5 median value mm 24-h-1 Original RCP 2.6 RCP 8.5 10% 50% 90% 10% 50% 90% Blönduvirkjun 48 41 49 58 42 50 61 Búðarháls 46 40 47 56 40 48 59 Hágöngulón 63 55 65 76 55 66 81 Hálslón 85 75 88 104 /media/vedurstofan-utgafa-2022/VI_2022_006_extreme.pdf

• 27. A minor eruption underway

  to view alarger image or to download the picture. This picture shows the location where the magma chamber is forming under the earth's crust. When magma flows into the sedimentary strata and forms magma tunnels, as is currently the case in the area of unrest between Keilir and Fagradalsfjall, pressure is formed in the earth's crust. This creates tension on the east and west sides of the area /about-imo/news/earthquake-swarm-in-reykjanes-peninsula

• 28. Climate and Modeling Scenarios

  Climate Modelling and Scenarios Deliverable D2.3). 36 pp. Venäläinen, A., Saku, S., Jylhä, K., Nikulin, G., Kjellström, E. & Bärring, L. (2009). Climate extremes and safety of nuclear power plants: Extreme temperatures and enthalpy in Finland and Sweden in a changing climate. Nordisk Kärnsäkerhet, NKS-194. pp 33. ISBN 978-87-7893-261-7. http://www.nks.org/download/pdf/NKS-Pub/NKS-194.pdf Ylhäisi, J /ces/publications/nr/1680

• 29. VI_2020_008

  /media/vedurstofan-utgafa-2020/VI_2020_008.pdf

• 30. VI_2021_008

  such as increase and decrease in eruptive activity, individual earthquakes, and even man-made noise linked to on-site maintenance and operations. Figure 15. Screenshot of Tremv’s “live” cursor feature. 21 Figure 16. Example of web-based RSAM data request form. For a selected data range, passband filter, and list of stations, the web page will download a csv file of RSAM data by user /media/vedurstofan-utgafa-2021/VI_2021_008.pdf