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  • 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. 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
  • 3. Future Climate and Renewable Energy - Impacts, Risks and Adaptation 31 May - 2 June Presentations

    system in 2020 - Impacts from changing climatic conditions Claude Demers Impacts and adaptation of the hydroelectric industry in the province of Québec, Canada Úlfar Linnet Hydropower in Iceland: Impacts and adaptation in future climate Ashraful Alam Forest biomass for energy production - potentials, management and risks under climate change Dougal Burnett Climate change and the UK solar /ces/publications/nr/2016
  • 4. 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
  • 5. askja_minnisblad_ens

    and rescue team saw a white plume rise up above Askja at 23:27. The steam plume was created when the slide exposed shallow geothermal areas in the release area. In addition, a dust cloud created by the rock slide may have contributed to the plume. The release area of the rockslide is approximately 800 m wide and 350 m above the lake surface. It may have been a "rotational slide movement", which /media/ofanflod/myndasafn/frodleikur/askja_minnisblad_ens.pdf
  • 6. Eriksson_Garvill_Nordlund_2006

    and infringement on freedom, and indirectly associated with the acceptability of road pricing. In addition, relations between beliefs about effectiveness and acceptability of TDM measures have been shown. More specifically, the more effective a measure is perceived to be, the more acceptable it is (e.g. Bamberg & Ro¨lle, 2003; Nordlund & Garvill, 2006; Rienstra et al., 1999). For coercive measures /media/loftslag/Eriksson_Garvill_Nordlund_2006.pdf
  • 7. Rockslide in Askja, July 21 2014 - Preliminary results of observations

    plume rise up above Askja at 23:27. The steam plume was created when the slide exposed shallow geothermal areas in the release area. In addition, a dust cloud created by the rock slide may have contributed to the plume. The release area of the rockslide is approximately 800 m wide and 350 m above the lake surface. It may have been a "rotational slide movement", which means that the failure surface /avalanches/articles/nr/2929
  • 8. Group5-Stakeholders_involvement

    Horsens case / Stakeholders involvement draft report Patience, Yuan, Emmanuel Horsens case / Stakeholders involvement • Overall objective Facilitate adaptation of horsens municipality to climate change • Purpose Negociated catalogue of coping measures adopted at the end of the participatory process • Stakeholders • Participation stages • Milestones 26 August 2011 PM/YZ /media/loftslag/Group5-Stakeholders_involvement.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. event_numbers_17022015

    Earthquakes since 16. August 2014 00:00 all intrusion caldera Kistufell Askja HB / HBT TFJ Kverkfj. automatic ~ 35.000 - - - - - - - checked ~ 20.000 ~ 8.000 ~ 9.000 ~ 200 ~ 300 ~ 1.800 ~ 600 ~ 20 M3.0-3.9 1208 99 1089 6 2 4 7 1 M4.0-4.9 655 7 646 1 1 0 0 0 M>5.0 79 0 79 0 0 0 0 0 HB / HBT Herðubreið and Herðubreiðartögl TFJ Tungnafellsjökull Kverkfj. Kverkfjöll Kistufell cluster north /media/jar/myndasafn/frodleikur/event_numbers_17022015.pdf

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