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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. Group2-PresentationWithPictures[1]

  2050 Planning Clean up landfills23 Monitoring1 Enhanced natural attenuation 2 Isolate the point sources 13 RRR23 Stop pollutants 3 Reduce nutrient 123 New/Modified crops and production2 Close Farms3 Technology 23 Upgrade WWT plants2 Implement a two string system2 Decentralised systems23 Grey water stream to city infrastructure 3 Source separation3 Sustainable fishery2 Waste /media/loftslag/Group2-PresentationWithPictures[1].pdf

• 4. Öræfajökull : Recent research

  (pdf 2.75 Mb)Pages 123–140Emmanuel PagneuxShort summaryChapter VII. Öræfajökull: Evacuation time modelling of areas prone to volcanogenic floods (pdf 2.96 Mb)Pages 141–164Emmanuel PagneuxShort summaryRecommended citation for individual chapters (example):Roberts, M. J., & Gudmundsson, M. T. (2015). Öræfajökull Volcano: Geology and historical floods. In E. Pagneux, M. T. Gudmundsson, S. Karlsdóttir /volcanoes/about-volcanoes/oraefajokull/new-research/

• 5. 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/

• 6. 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

• 7. Huntjens_etal-2010-Climate-change-adaptation-Reg_Env_Change

  The Netherlands 123 Reg Environ Change (2010) 10:263–284 DOI 10.1007/s10113-009-0108-6 On a global scale, the number of disasters caused by weather-related phenomena such as storms, floods, and droughts has more than doubled over the past decade, from 175 in 1996 to 391 in 2005 (IFRC 2008). The same trend (Fig. 1) is being observed in the case-studies under inves- tigation, which is Rivierenland /media/loftslag/Huntjens_etal-2010-Climate-change-adaptation-Reg_Env_Change.pdf

• 8. The weather in Iceland in 2020

  location temp °C dev 1961-1990 rank total Dev 2010-2019 Reykjavík 5.1 0.7 33 150 -0.4 Hvanneyri 4.3 # 16 23 -0.4 Bláfeldur 4.7 # 16 23 -0.5 Stykkishólmur 4.5 1.0 26 to 27 175 -0.4 Bolungarvík 3.8 0.9 32 123 -0.4 Litla-Ávík 3.9 /about-imo/news/the-weather-in-iceland-in-2020

• 9. The weather in Iceland 2014

  Hornafirði 6.5 1.9 1.2 Fagurhólsmýri 6.4 1.8 1 112 0.9 Stórhöfði 6.2 1.4 2 138 0.4 Hveravellir 0.9 1.9 2 50 0.6 Árnes 5.3 1.7 2 134 0.7 Eyrarbakki 5.6 1.5 3 123 0.4 Annual temperature at a few stations and deviation from the 1961 to 1990 and 2004 to 2013 averages. The highest annual temperature was registered in Surtsey (off the South coast), 7.2 /about-imo/news/nr/3082

• 10. Markarfljót outwash plain and Öræfajökull

  the results should be considered carefully by the local and national authorities for planning and emergency evacuation purposes. Chapter VI. Öræfi district and Markarfljót outwash plain: Spatio-temporal patterns in population exposure to volcanogenic floods (pdf 2.75 Mb) Pages 123–140 Emmanuel Pagneux Short summary A spatio-temporal exploration of population exposure is performed /hydrology/hazard-risk-assessments/glacial-outburst-floods/markarfljotsaurar-oraefajokull/