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Results:

• 1. Hare_2-participation

  Participatory processes in the real world Conjugation of “to participate” I participate You participate He participates We participate They profit From Arnstein (1969) Matt Hare, Independent Consultant, Mexico hare@gmx.de Participatory Processes in Practice Long-term planning for change 3 “PartizipA“ Local level measures assessment for the Water Framework Directive (Newig et al 2008) 4 /media/loftslag/Hare_2-participation.pdf

• 2. 47th Nordic Seismology Seminar

  WarningAlert phase from the Civil Protection due to an earthquake swarm in Reykjanes peninsula. WarningDue to the ongoing seismic activity in Reykjanes peninsula people are advised to avoid steep terrain as rocks and boulders can fall and chances of landslides are increased /norsem/norsem2016/transportation/

• 3. Guidelines2-for-rapporteurs

  ). This can be helpful with respect to finding a common structure in presenting as well in session reporting (for which angles mentioned in the opening session statements of the Workshop participants can provide checkpoints).” Session rapporteur allocation M o n d a y 2 9 . 8 Y u a n g Z h e n g A t h a n a s i o s V o t s i s E i v i n d J u n k e r M i c h a e l L a i h o H e c to r /media/loftslag/Guidelines2-for-rapporteurs.pdf

• 4. Group4

  mix, 4) mobility patterns, technological development, 5) equitable distribution of social goods, ethical dynamics Background information and knowledge gaps: 1) time scale-what is the consensus view of when are the CC impacts projected to begin to be felt, 2) spatial scale-where are the impacts expected to occur, 3) vulnerability assessments of differential capacity to adapt to CC impacts /media/loftslag/Group4.pdf

• 5. Lorenzoni_Pidgeon_2006

  of the British population, which are illustrated in Table I (from Poortinga and Pidgeon, 2003a). Here, respondents were ambivalent about the potential for damage and catastrophe arising from climate 82 I. LORENZONI AND N. F. PIDGEON TABLE I Climate change evaluated on various psychometric characteristics by 312 British respondents. The scale ranges from 1 (“totally disagree”) to 5 (“totally agree /media/loftslag/Lorenzoni_Pidgeon_2006.pdf

• 6. Cradden_Lucy_CES_2010

  superimpose both heating and cooling effects, i.e., – wind = cooling – temperature, solar radiation = heating June 2010 5 • Limit to how much heat the wire can be exposed to • Amount of allowable current based on ambient conditions is known as ‘rating’ Network capacity (ampacity) Too much heat causes ‘sag’ where minimum ground clearance is not achieved June 2010 6 How are ratings determined /media/ces/Cradden_Lucy_CES_2010.pdf

• 7. programme2---PhD-Workshop-preceding-Adaptation-Research-Conference

  in the preceding review sessions. The messages can be requests, critical questions, propositions for emphasis on certain topics in future research and/or implementation, educational wishes, etc. In the opening plenary session of the Adaptation Conference on Wednesday morning two PhD students (one from each group) will present the messages (max. 5 minutes each). 2 Tasks in the Conference /media/loftslag/programme2---PhD-Workshop-preceding-Adaptation-Research-Conference.pdf

• 8. Group5-Stakeholders_involvement

  Knowledge gathering Proposal Testing Revision Decision- making Milestones 26 August 2011 PM/YZ/EPP 5 Phase s Du r at i o n ( mon t h s ) O V I s Problem iden t i f i ca t i on 2 A l l St a k ehol d e r s i d ent i f i ed an d selected wi t h i n 2 mo n t h s I n f o r ma t i on pro v i s i on 2 Kic k - of f m e et i n g hel d Knowled g e ga t he r i n g 6 /media/loftslag/Group5-Stakeholders_involvement.pdf

• 9. Veðurstöðvar

  WarningAlert phase from the Civil Protection due to an earthquake swarm in Reykjanes peninsula. WarningDue to the ongoing seismic activity in Reykjanes peninsula people are advised to avoid steep terrain as rocks and boulders can fall and chances of landslides are increased /weather/stations/

• 10. VI_2014_001

  at each site i with the same method used to estimate qR(D;T ), but instead of pooling AMF series for a given duration D from different sites, the estimation is made individually for each site i by pooling AMF series for different durations D (see Crochet, 2012c). The index flood µi(D), is modeled at each site i as a continuous function of D, as follows: µi(D) = µi 1+(D=Di)li ; (5) where µi, Di /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_001.pdf