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Results:

• 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. 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. IPPC-2007-ar4_syr

  Approximate CO2-eq concentrations corresponding to the computed radiative forcing due to anthropogenic GHGs and aerosols in 2100 (see p. 823 of the WGI TAR) for the SRES B1, AIT, B2, A1B, A2 and A1FI illustrative marker scenarios are about 600, 700, 800, 850, 1250 and 1550ppm, respectively. d) Temperature changes are expressed as the difference from the period 1980-1999. To express the change relative /media/loftslag/IPPC-2007-ar4_syr.pdf

• 4. Daniell_etal-2010

  and evaluating impacts (see also Swallow et al. 2001, van Ast and Boot 2003). METHODS AND DATA This article is based on empirical data that originated from the analysis of the participatory exercise in the Dhuenn basin. The strong involvement of researchers from two research projects (NeWater[1] and ACER[2]) linked by a joint case study led to the variety of sources available for exploration, including /media/loftslag/Daniell_etal-2010.pdf

• 5. VanderKeur_etal-2008-Uncertainty_IWRM-WARM

  cia l sy ste m ): th re e m ai n gr ou ps o fthreat s ar e at th e scene : cl im at e, so ci o -e co n o m ic s an d gover nanc e 1: M ai nl y ep ist em ic pl us som e onto logi ca l 2:S cenari o Pa rti ci pa to ry pr oc es s (PP ) imp ortan tt o de al w ith un certaint y Pa rti cip at o ry pr o ce ss (PP )im po rta n tt o de al w ith u n ce rta in ty : Pa rti ci pa to ry go al se tti ng :c o n /media/loftslag/VanderKeur_etal-2008-Uncertainty_IWRM-WARM.pdf

• 6. 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

• 7. ces-oslo2010_proceedings

  change over the North Atlantic and in some simulations also for Iceland. In all areas, including the North Atlantic and Iceland, a clear climate change signal compared to the spread between the simulations is seen. The standard deviation calculated from 17 of the simulations are less than 1°C in all areas apart from Iceland where it reaches between 1 and 2°C and in parts of the Barents Sea where /media/ces/ces-oslo2010_proceedings.pdf

• 8. Sigurður Th. Rögnvaldsson

  Hengill. Rit Veðurstofu Íslands VÍ-R98006-JA05. Sigurður Th. Rögnvaldsson, Þóra Árnadóttir, Kristján Ágústsson, Þórunn Skaftadóttir, Gunnar B. Guðmundsson, Grímur Björnsson, Kristín S. Vogfjörð, Ragnar Stefánsson, Reynir Böðvarsson, R. Slunga, Steinunn S. Jakobsdóttir, Einar Kjartansson, Bergþóra Þorbjarnardóttir, Pálmi Erlendsson, Bergur H. Bergsson, Sturla Ragnarsson, Páll Halldórsson, Barði /earthquakes-and-volcanism/conferences/jsr-2009/sigurdur/

• 9. Sigurður Th. Rögnvaldsson

  Hengill. Rit Veðurstofu Íslands VÍ-R98006-JA05. Sigurður Th. Rögnvaldsson, Þóra Árnadóttir, Kristján Ágústsson, Þórunn Skaftadóttir, Gunnar B. Guðmundsson, Grímur Björnsson, Kristín S. Vogfjörð, Ragnar Stefánsson, Reynir Böðvarsson, R. Slunga, Steinunn S. Jakobsdóttir, Einar Kjartansson, Bergþóra Þorbjarnardóttir, Pálmi Erlendsson, Bergur H. Bergsson, Sturla Ragnarsson, Páll Halldórsson, Barði /earthquakes-and-volcanism/conferences/jsr-2009/sigurdur

• 10. glacier_mass_balance_poster

  - accuracy on cm scale at gentle sloping terrain - higher errors at rough and steep sloping terrain - often false values due to frequent occurence of clouds in the area c) GPS profiles and points observed at ice free areas - accuracy ~1 m in elevation Characteristics Ice cap E: Eyjafjallajökull To: Torfajökull Ti: Tindfjallajökull Area (km2) Range in elevation (m a.s.l.) 81 15 14 180-1630 660-1480 /media/ces/glacier_mass_balance_poster.pdf