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

  with whom a slot is proposed to be swapped. In the closing session on Friday afternoon another two Workshop participants will be offered the opportunity of presenting a brief summary of key impressions and messages (2 x 5 minutes). This will require some degree of co-ordination among the rapporteurs. The Conference organizers need to know in time (Friday morning at the latest) who will present /media/loftslag/programme2---PhD-Workshop-preceding-Adaptation-Research-Conference.pdf

• 2. 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

• 3. Bárðarbunga earthquakes - interactive model

  the operating system does not support the requirements or the hardware causes problems. But most of the users of en.vedur.is should be able to find their way to enjoy this product. A demo version is available below. Instructions The topography is exaggerated by factor 5, while depth in the model is not exaggerated. The depth of the earthquakes is indicated by two planes, at 5 km and 10 km, but in fact /earthquakes-and-volcanism/articles/nr/2971

• 4. Bárðarbunga earthquakes - interactive model

  the operating system does not support the requirements or the hardware causes problems. But most of the users of en.vedur.is should be able to find their way to enjoy this product. A demo version is available below. Instructions The topography is exaggerated by factor 5, while depth in the model is not exaggerated. The depth of the earthquakes is indicated by two planes, at 5 km and 10 km, but in fact /earthquakes-and-volcanism/articles/nr/2971/

• 5. Group1-Adaptive_Management_in_a_relation_to_climate_change2

  areas may experience intense rainfall resulting in heavy floods, while other areas may witness less rainfall due to living in highland. Research Flood frequency and intensity communication capacity Area of residence (Flood prone /non prone areas) Uncertanties High willingness to pay Low willingnes to pay Dikes High taxation -Early warning systems -Soft structural measures /media/loftslag/Group1-Adaptive_Management_in_a_relation_to_climate_change2.pdf

• 6. Information and help

  terrain, in particular in areas where the snow cover changes from thin to thick or from hard to soft. Persistent weak layers What? Characteristics The avalanche problem is related to the presence of persistent weak layers in the old snowpack. These weak layers typically include buried surface hoar, depth hoar or faceted crystals.. Expected avalanche types Dry /avalanches/forecast/help

• 7. News

  News Measurements from early morning 23 May 2011. Two ash layers can be detected, at altitudes of 500 and 1200 m /about-imo/news/bigimg/2183

• 8. Henriksen_Barlebo-2008-AWM_BBN-Journ_Env_Management

  negotiation between ARTICLE IN PRESS parties involved will emerge and become more difficult. Encoding and populating BNs with numbers and CPTs are the most critical part of the construction process but at the same time the most important and powerful feature of BNs, compared to more soft tools for participatory integrated assessment e.g. ‘brainstorming’, ‘multi-criteria techniques’, ‘consensus /media/loftslag/Henriksen_Barlebo-2008-AWM_BBN-Journ_Env_Management.pdf

• 9. Mo_Birger_CES_2010

  Simulation results Hydropower Thermal production Energy balance CO2-emissions 4 Summary and concluding remarks Sintef Energy Research Quantitative system analysis 8 of 21 Introduction Electricity system model Simulation results Summary and concluding remarks Hydropower Thermal production Energy balance CO2-emissions Annual average in ow over the year, GWh 0 14 28 42 52 0 500 1;000 1;500 2;000 2;500 /media/ces/Mo_Birger_CES_2010.pdf

• 10. News

  are aligned above the eastern rim of the Katla caldera, which lurks underneath the ice-cap. In the center of the caldera, the ice is over 500 m thick. Melt water from the surface of the glacier has collected in the bowl, giving the blue colour, but that is irrelevant to the activity discussed in this article /about-imo/news/bigimg/3369