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Results:

• 41. Moberg_Anders_CES_2010

  -010-9816-7, Figs. 1&3 North American droughts last 1200 years Cook et al. JQS 2010, 25(1), p.48-61, Figs. 4&7 Volcanic aerosols Changing solar radiation Changing greenhouse gas concentrat ions – natural and human Anthropogenic and natural emissions of aerosols Changed land use Internal dynamics IPCC 2007, Fig. 6.13 Reasons behind the changes Mann et al. Science 2009, 326, p.1257, Fig. 1 Past /media/ces/Moberg_Anders_CES_2010.pdf

• 42. Hock_Regine_CES_2010rs

  Projections -50% -48%-73% -78% -80% +3% Storglaciären Mårmaglaciären Scandinavia Comparison with all other glacier regions Volume reduction and sea-level equivalent (SLE) until 2100 for 19 glacier regions Radic and Hock, submitted Antarctica Sub-Antarctic Islands Greenland New Zealand South America II South America I Iceland Arctic Canada West Canada and West US Alaska High Mountain Asia North /media/ces/Hock_Regine_CES_2010rs.pdf

• 43. 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

• 44. norsem_atakan_ip

  European Plate Observing System Implementation Phase (EPOS-IP): Services for Solid Earth Science Kuvvet Atakan1 and the EPOS-Consortium2 1 Department of Earth Science, University of Bergen, Norway, E-mail: Kuvvet.Atakan@uib.no 2 EPOS www.epos-eu.org The European Plate Observing System (EPOS) aims to create a pan-European infrastructure for solid Earth science to support a safe /media/norsem/norsem_atakan_ip.pdf

• 45. norsem_janutyte

  Fault plane solutions of the earthquakes in Nordland, Norway Ilma Janutyte(1), Jan Michalek(2), Conrad Lindholm(1), and Lars Ottemoller(2) (1) NORSAR, Kjeller, Norway, (2) University of Bergen, Bergen, Norway This study is a part of the ongoing NEONOR2 project which is carried out in Nordland, norther Norway. This work aims to define the fault plane solutions (FPS) of the earthquakes /media/norsem/norsem_janutyte.pdf

• 46. ces_SA_group_flyer_new

  are being used to analyse the occurrence of dry spells, both from historical data and from climate scenario simulations. There is significant year-to-year variability in the pattern of rainfall, and this variability is assessed based on the range of values from individual years in the analysis. No change Increase Decrease 1 9 6 1 - 1 9 9 0 1 9 3 1 - 1 9 9 0 Photo by V. Kudryavskiy, LEGMA Regional /media/ces/ces_SA_group_flyer_new.pdf

• 47. VI_2013_006

  winds. Location of this lightning is far from the eruption site. Photo Þórður Arason from a 72 km distance on 17 April 2010 at 04:47:09 UTC (30 s exposure time). Lightning location data Lightning is an electric current through air which occurs when electric charges accumulate to a point where the electric charge difference and thus the electric field between two places becomes too high /media/vedurstofan/utgafa/skyrslur/2013/VI_2013_006.pdf

• 48. VI_2021_008

  off an audio alarm. This feature is especially useful when there is an ongoing eruption (i.e. Fagradalsfjall 2021), as the stations around this eruptive area can be muted to enhance signals from other regions in Iceland. • Remove stations: Stations can be removed from the trigger calculations for all bandpass filters. Removed stations will not be accounted for in the tremor catalog /media/vedurstofan-utgafa-2021/VI_2021_008.pdf

• 49. Climate and Modeling Scenarios

  & Ruosteenoja, K. (2009). Comparing regional risks in producing turnip rape and oilseed rape - Impacts of climate change and breeding. Acta agriculturae Scandinavica 59B:2, 129-138. doi:10.1080/09064710802022895 (http://www.ingentaconnect.com/content/tandf/sagb/2009/00000059/00000002/art00004). Pryor, S.C., Barthelmie, R.J., Clausen, N.E., Drews, M., MacKellar, N. & Kjellström, E. (2010). Analyses /ces/publications/nr/1680

• 50. Hazard zoning

  for seasonal variability have been produced. The CALPUFF model has been initialized with SO2 flux data as coming from the DOAS monitoring system (Gislason et al., 2015). Maps based on ten years of meteorological data Each map below shows the likelihood that at a specific location the hourly ground concentration of SO2 will exceed a specific threshold. The threshold values are shown in bold blue /pollution-and-radiation/volcanic-gas/hazard-zoning/