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• 11. 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

• 12. Hare-2011-ParticipatoryModelling

  are labelled according to the geographical area of application. Examples such as Zürich and Hase II have already been reviewed and categorized in Hare et al. (2003) and Bots and van Daalen (2008), respectively. The entire Iskar process, of which Iskar (Phase I) is a part, has been categorized by Barreteau et al. (2010). All are included in this review to provide alternative analytical perspectives /media/loftslag/Hare-2011-ParticipatoryModelling.pdf

• 13. 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

• 14. Huntjens_etal-2010-Climate-change-adaptation-Reg_Env_Change

  can be found in Huntjens et al. (2007), Chapter 4 of NeWater Deliverable 1.7.9a (http://www.newater.info). Climate change adaptation in European river basins 265 123 interactions, by private and public actors, to achieve adaptation and to enhance the capacity of processes, institutional arrangements and actors to adapt to future environmental changes (Huitema et al. 2009). Adaptive governance /media/loftslag/Huntjens_etal-2010-Climate-change-adaptation-Reg_Env_Change.pdf

• 15. 2013_001_Nawri_et_al

  and a pressure of 1013.25 hPa. In the case of Iceland, the climate deviates significantly from these standard atmospheric conditions. Additionally, terrain elevation varies considerably across the island. Therefore, seasonal and annual differences in air density from the standard value, as well as spatial variability, need to be taken into account. Approximate air density can be calculated by assuming /media/vedurstofan/utgafa/skyrslur/2013/2013_001_Nawri_et_al.pdf

• 16. Refsgaard_1-Welcome

  – Print yourselves • Case descriptions and tasks/questions • Lecturers’ presentations – Handouts during the week – Pdfs will be uploaded at website afterwards Practicalities • PC login – Internet access • Printing • Lunch • Coffee – tea • Posters Monday afternoon + refreshments • Dinner Tuesday at 19:00 Students • Brief presentation round – now • 2-minutes presentation of research topics /media/loftslag/Refsgaard_1-Welcome.pdf

• 17. Factsheet_Bardarbunga_20141027

  University of Iceland along with representatives from the Icelandic Civil Protection and the Environmental Agency of Iceland. Main points  Volcanic eruption in Holuhraun  Air quality  Scenarios Notes  The volcanic eruption in Holuhraun continues with similar intensity.  Seismic activity in Bardarbunga continues to be strong. Over 200 earthquakes have been detected in the caldera /media/jar/Factsheet_Bardarbunga_20141027.pdf

• 18. Factsheet_Bardarbunga_20141029

  University of Iceland along with representatives from the Icelandic Civil Protection and the Environmental Agency of Iceland. Main points  Volcanic eruption in Holuhraun  Air quality  Scenarios Notes  The volcanic eruption in Holuhraun continues with similar intensity.  Seismic activity in Bardarbunga continues to be strong. 130 earthquakes have been detected in the caldera over /media/jar/Factsheet_Bardarbunga_20141029.pdf

• 19. Factsheet_Bardarbunga_20141031

  around magnitude M1,0 and smaller.  GPS measurements in the active area show minor changes. A recommendation by the Scientific Advisory Board of the Icelandic Civil Protection: The Scientific Advisory Board concludes that it is necessary to increase monitoring of SO4 so it is possible to evaluate the concentration of sulphuric acid particles and its potential influence on health. Air /media/jar/Factsheet_Bardarbunga_20141031.pdf

• 20. Factsheet_Bardarbunga_20141103

  site in Holuhraun. Most reliable are the forecast maps approved my meteorologist on duty, see Gas forecast. And although still being developed further, an automatic forecast, see Gas model, is also available (trial run, see disclaimer). • A new online gas detector has been put up in Hofn in Hornafjordur. Measurements of air quality can be found on the NATIONAL COMMISSIONER OF THE ICELANDIC /media/jar/Factsheet_Bardarbunga_20141103.pdf