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  • 1. 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
  • 2. 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
  • 3. Bárðarbunga earthquakes - interactive model

    (central mouse scroll), pan (right click), turn over (left click) choose speed 1x, 2x, 10x (available in some browsers (e.g. Chrome but not Firefox) coloured patches on/off (ring icon) choose landscape map (mountain icon) or satellite image (bell icon) for the surface Tryggvi Hjörvar, specialist at the Icelandic Met Office, created this model. An easier presentation - demo In a video /earthquakes-and-volcanism/articles/nr/2971
  • 4. Bárðarbunga earthquakes - interactive model

    (central mouse scroll), pan (right click), turn over (left click) choose speed 1x, 2x, 10x (available in some browsers (e.g. Chrome but not Firefox) coloured patches on/off (ring icon) choose landscape map (mountain icon) or satellite image (bell icon) for the surface Tryggvi Hjörvar, specialist at the Icelandic Met Office, created this model. An easier presentation - demo In a video /earthquakes-and-volcanism/articles/nr/2971/
  • 5. Spatial_perception_of_flood_hazard_in_the_urban_area_of_Selfoss,_Iceland

    A survey on flood risk perception was conducted in the town of Selfoss from May to August 2009 among the residents aged above 18. The respondents were proposed to draw the boundaries of areas flooded from the beginning of the 20th century on an orthophotograph of Selfoss at scale 1:10.000. The spatial representations of the flood area were processed with a regulated grid of 10 x 10 metres /media/loftslag/Spatial_perception_of_flood_hazard_in_the_urban_area_of_Selfoss,_Iceland.pdf
  • 6. Demers_Claude_CES_2010

    1 9 6 5 1 9 6 7 1 9 6 9 1 9 7 1 1 9 7 3 1 9 7 5 1 9 7 7 1 9 7 9 1 9 8 1 1 9 8 3 1 9 8 5 1 9 8 7 1 9 8 9 1 9 9 1 1 9 9 3 1 9 9 5 1 9 9 7 1 9 9 9 2 0 0 1 2 0 0 3 2 0 0 5 2 0 0 7 2 0 0 9 G W h Écarts énergétiques annuels du parc total hydraulique d'Hydro-Québec + Churchill Falls Années ConclusionAdaptationClimate & HydrologyContext Hydro-Québec and Climate Change The question to be answered • How /media/ces/Demers_Claude_CES_2010.pdf
  • 7. Linnet_Ulfar_CES_2010

    HYDROPOWER IN ICELAND Impacts and adaption in future climate Authors Óli Grétar Blöndal Sveinsson (Phd) Úlfar Linnet (MSc) Elías B. Elíasson (MSc) Landsvirkjuns system •Installed power 1850 MW • 96 % Hydroelectricity • 4% Geothermal •Production capacity 13 TWh/a •Customer base86 % Large industries • 14 % Small businesses / Household •No connection to other countries •Reliability a major /media/ces/Linnet_Ulfar_CES_2010.pdf
  • 8. Group3-The-future-of-the-Finnish-national-road-network

    ) Best case (1.5 C increase; 2% increase in prec) BAU A B Change +30 % C D Scenario combination Impact Adaptation measures North South North South A * CC: Possible increase in the amount of snow  more snow clearing  increase in operational costs S-E: increase in traffic volume  increased wear of roads  increase in maintenance cost. ** CC: Possibly less snow, more rain /media/loftslag/Group3-The-future-of-the-Finnish-national-road-network.pdf
  • 9. Journal_of_Hydrology_Veijalainen_etal

    A second, but usually smaller, increase in runoff oc- curs in the autumn. In northern Finland more than 95% of annual maximum floods are caused by spring snowmelt (cf. Fig. 7a). Also the small upstream lakes in the northern part of the lake area and the northernmost of the coastal rivers fall mainly into this cat- egory. In most coastal rivers the major floods can be caused by either snowmelt /media/ces/Journal_of_Hydrology_Veijalainen_etal.pdf
  • 10. Henriksen_Barlebo-2008-AWM_BBN-Journ_Env_Management

    the body of knowledge in any given area by mapping out cause-and-effect relationships among key variables and encoding them with numbers that represent the extent to which one variable is likely to affect another (Jensen, 2002). Factors, associations and probabilities can be adjusted and validated and BNs are powerful for integrating data and knowledge from different sources and domains, e.g /media/loftslag/Henriksen_Barlebo-2008-AWM_BBN-Journ_Env_Management.pdf

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