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Results:

• 11. EEA

  national challenges, such as drought, floods or storm surges Adaptation policies and practices in cities, agriculture and in coastal areas The need to think beyond national borders Participants are those countries and actors involved in the EEA Grants programmes and/or in the development of adaptation policies in the EU. Árni Snorrason, Dir. General of the Icelandic Meteorological Office /about-imo/news/nr/2763

• 12. A new IMO has been launched

  exceptional trust and good-will among the nation," she added, wishing him well on a six months research leave in New Zealand. In fact, a survey by Capacent Gallup last year revealed that 90% of the population claim IMO provide good or very good services and that over 60% choose IMO's web-site for information. Our new Director General, Árni Snorrason, has lead a thorough re-organization /about-imo/news/nr/1449

• 13. Gareth_James_Lloyd_(DHI,_Dk)

  Gareth James Lloyd, DHI Water Policy/UNEP-DHI Centre – What is the difference between adaptation and adaptive management? Adaptation refers both to the process of adapting and to the condition of being adapted. The term has specific interpretations in particular disciplines. The IPCC (2007) defines climate adaptation as, “adjustment in natural or human systems in response to actual /media/loftslag/Gareth_James_Lloyd_(DHI,_Dk).pdf

• 14. Bardarbunga_kafli20140825

  have not been located it is not clear whether eruptions on the central part of the system belong to a central volcano or the ice covered fissure swarm. Both cases will generate jökulhlaups from rapidly melting ice. All explosive eruptions originating below ice are therefore described together. 4 4.1 Bárðarbunga central volcano and adjacent ice covered fissure swarm 1. Phreatomagmatic /media/jar/Bardarbunga_kafli20140825.pdf

• 15. Keskitalo_et_al-MLG_and_adaptation_FINAL

  areas: to the regional arm of the state (the county administrative boards) to coordinate adaptation; to specific governmental bodies and agencies to develop a common elevation data basis; and for the assessment of flood risk and erosion defense measures around Lake Vänern. Risks considered by the Bill include the flooding of central Gothenburg, the second largest city of Sweden (a risk /media/loftslag/Keskitalo_et_al-MLG_and_adaptation_FINAL.pdf

• 16. Savolainen_Ilkka_CES_2010

  (run-off, soil humidity) Risks concerning decision making (policy risks) 303/02/2010 Illustrative map of future climate change impacts related to freshwater which threaten the sustainable development of the affected regions. Ensemble mean change in annual runoff (%) between present (1980–1999) and 2090–2099 for the SRES A1B emissions scenario. Areas with blue (red) colours indicate /media/ces/Savolainen_Ilkka_CES_2010.pdf

• 17. Case_B___Road_transport_operation_and_infrastructure_planning

  on the Shifts of climatic zones from cooler or wetter to warmer or drier (a) 1971-2000 (b) 2010-39 A1B observational data set (0.25º grid) from Haylock et al. (2008) (b-d) Based on CMIP3 GCM runs for A1B & the delta-change method (c) 2040-69 A1B (d) 2070-99 A1B Jylhä et al. (2010) Uncertainties in climate change schematically Observed climate Future climate Natural /media/loftslag/Case_B___Road_transport_operation_and_infrastructure_planning.pdf

• 18. Hare_1_Part2

  is important to the person about a management issue a71 the important concepts in that system a71 and their relationships to one another (causal, structural etc.) a108 can identify beliefs about how the system works, as well as its problems and their solutions cognitive mapping Knowledge Elicitation 1. Individual SH cognitive maps (Hodgson‘s hexagon modelling) 2. Scientists‘ agent-based /media/loftslag/Hare_1_Part2.pdf

• 19. norsem_voss

  broad band station was installed in Northern Jutland on OCT 8th, 2015, with the ISC code for this station is: OVD. Together with partners from Sweden and Finland we took part analyzing small finish earthquakes for NKS. North of Copenhagen we conducted a short noise study before the summer of 2016 and by the end of 2016 we will take part in the EU project INTAROS with colleagues /media/norsem/norsem_voss.pdf

• 20. Water_resources_man_Veijalainen_etal

  range 90% 93.15–93.29 93.27–93.36 75.43–75.56 94.59–94.71 2040–2069 range 90% 93.09–93.31 93.28–93.40 75.41–75.56 94.72–94.83 2070–2099 range 90% 93.02–93.32 93.24–93.43 75.38–75.61 94.79–94.91 Lowest water level (in the 30 year period) (m) Reference period 92.86 92.72 75.20 94.27 2010–2039 range 90% 92.62–92.91 92.96–93.13 75.24–75.33 94.47–94.59 2040–2069 range 90% 92.55–92.82 92.88–93.12 75.19 /media/ces/Water_resources_man_Veijalainen_etal.pdf