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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. case_2_day_2

  Define stakeholders Frame Problem -Service Level -Types of scenarios Analyze Scenarios Elaborate Scenarios Need for further action -Legal -Analyze -Etc. Framing OK Mandate National Government Technical Input Mandate Stakeholders Technical Experties Stakeholders Technical Experties Stakeholders -PEER REVIEW_ Acceptability of separate issues. (Trade off) Stakeholders Physical /media/loftslag/case_2_day_2.pdf

• 3. Mid-Latitudes-Agenda1_nov2013EH

  11:20 – 11:35 11:35 – 11:55 11:55 – 12:15 12:15 – 12:35 12:35 – 12:45 Jet Stream Especially the North Atlantic (Chair: Robert Erdelyi) A long perspective on Atlantic jet variability – T Woollings A comparison of North Atlantic Jet Stream Representation in ERA-Interim and 20th Century Reanalysis Data - R Hall Frozen assets: what can ships' logbooks tell us about Arctic climate change /media/loftslag/Mid-Latitudes-Agenda1_nov2013EH.pdf

• 4. Hock_Regine_CES_2010rs

  Projections -50% -48%-73% -78% -80% +3% Storglaciären Mårmaglaciären Scandinavia Comparison with all other glacier regions Volume reduction and sea-level equivalent (SLE) until 2100 for 19 glacier regions Radic and Hock, submitted Antarctica Sub-Antarctic Islands Greenland New Zealand South America II South America I Iceland Arctic Canada West Canada and West US Alaska High Mountain Asia North /media/ces/Hock_Regine_CES_2010rs.pdf

• 5. 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

• 6. 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

• 7. 2010_017

  m J M5 [C°] -3 obs. [C°] -4 nce 1 re 5. Comp 26); an int temperatu this system y gridded v picion abo -Jökulsá w similar dif han observ h elevation ces the effe months No ly only on high the tem n band wi refore be s onthly tem an Feb Ma .2 -3.1 -3. .3 -4.1 -3. .1 1.0 0.6 arison of m erpolation re is shown atic differe alues, see T ut the qual atershed; b ference wa ations for t gradient fo /media/ces/2010_017.pdf

• 8. norsem_begga

  shock mag. ~3.0 and aftershocks). The DD relocation gives tighter clustering of earthquakes in all three areas, and the strike of a fault segment, unclear in the catalog data, becomes clearly visible after relocation. Relocation shifts the centroids of the clusters by ~300 m from catalog locations, but relative distances between clusters do not change significantly. Our next step is to extend /media/norsem/norsem_begga.pdf

• 9. 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

• 10. 2010_016

  the largest runoff peak of the year. Compared to the period 1961–1990, a warming of about 1°C has already been observed for both watersheds during the period 2000–2009, causing considerable discharge changes in the same direction as the predicted future changes. 8 2 Introduction Increased concentration of greenhouse gases in the atmosphere is predicted to lead to changed climate (IPCC, 2007 /media/ces/2010_016.pdf