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  • 1. programme2---PhD-Workshop-preceding-Adaptation-Research-Conference

    During the conference all of you are requested to act as rapporteur in two or three sessions. A preliminary allocation of rapporteur sessions has been made (see below), while accounting for your expertise in certain areas. Participants can suggest changes in the rapporteur session allocation, on the condition a convincing argumentation is provided as well as a confirmed alternative rapporteur /media/loftslag/programme2---PhD-Workshop-preceding-Adaptation-Research-Conference.pdf
  • 2. Traffc-maintenance_expenditures

    229 1 587 160 1970 18 591 42 413 2 166 86 101 - 892 5 131 2 310 201 - - - 157 805 1 652 904 1969 17 559 38 840 2 313 93 776 - 922 4 562 1 571 - - - - 159 543 1 832 354 1968 13 474 36 376 3 074 104 519 - 1 080 4 131 1 156 - - - - 163 811 1 964 368 1967 11 139 34 495 5 940 95 857 - 419 3 032 1 087 - - - - 151 968 1 936 249 1966 9 835 32 581 8 349 94 777 - 587 4 205 1 743 - - - - 152 077 2 032 936 /media/loftslag/Traffc-maintenance_expenditures.pdf
  • 3. 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
  • 4. VI_2013_006

    lightning by the ATDnet system during (a) Grímsvötn 2004, (b) Eyjafjallajökull 2010 and (c) Grímsvötn 2011. A blue circle is at the vent location. 11 Figure 5. A map view, North (km) vs. East (km), of Grímsvötn 2011 lightning for the first 30 min (123 lightning), 1 hour (888), 3 hours (3340) and 24 hours (16041). The actual eruption site is marked with a black circle /media/vedurstofan/utgafa/skyrslur/2013/VI_2013_006.pdf
  • 5. Group2-PresentationWithPictures[1]

    Scenarios for Horsens Fjord Al Azhar, Bjarke, Maria and Kerstin 26.08.2011 Scenarios for Horsens Fjord • Horsens Fjord • Policy agency and stakeholders • Several goals, focus on water quality • Backcasting to develop scenarios • Uncertainties Exploring Backcasting Collective Individual Society 3 Scenario process: socio economic Society 1 Society 2 Scenario process: climate /media/loftslag/Group2-PresentationWithPictures[1].pdf
  • 6. Öræfajökull : Recent research

    and Eyjafjallajökull hazard assessments were applied.The project was funded mainly by the National Avalanche and Landslide Fund, with additional financial contributions from the Icelandic Road and Coastal Administration and the National Power Company.Published materialPagneux, E., Gudmundsson, M. T., Karlsdóttir, S., & Roberts, M. J. (Eds.) (2015). Volcanogenic floods in Iceland: An assessment /volcanoes/about-volcanoes/oraefajokull/new-research/
  • 7. Sigurður Th. Rögnvaldsson

    and beyond year 2000. Phys. Earth Planet. Inter. 113, 89 101. Roberts, R. G., A. Lindfors, A. Christoffersson, Reynir Böðvarsson og Sigurður Th. Rögnvaldsson 1993. Three-component data as an aid to seismic event detection and asociation: A case study using data from the SIL (Iceland) network. Computers and Geosciences 19, pp. 123 134. Slunga, R., Sigurður Th. Rögnvaldsson og Reynir Böðvarsson /earthquakes-and-volcanism/conferences/jsr-2009/sigurdur/
  • 8. Sigurður Th. Rögnvaldsson

    and beyond year 2000. Phys. Earth Planet. Inter. 113, 89 101. Roberts, R. G., A. Lindfors, A. Christoffersson, Reynir Böðvarsson og Sigurður Th. Rögnvaldsson 1993. Three-component data as an aid to seismic event detection and asociation: A case study using data from the SIL (Iceland) network. Computers and Geosciences 19, pp. 123 134. Slunga, R., Sigurður Th. Rögnvaldsson og Reynir Böðvarsson /earthquakes-and-volcanism/conferences/jsr-2009/sigurdur
  • 9. 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
  • 10. The weather in Iceland in 2020

    to the 10-year average. It was relatively warmer in coastal areas but colder in the inland.JuneJune was warm and favorable. It was relatively warmest in the Northeast but cooler in the southwestern part. Wind and precipitation were close to average.July July was rather cold compared to recent years, although the mean was above the 1961 to 1990 average. Yet the weather was not unfavorable /about-imo/news/the-weather-in-iceland-in-2020

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