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Results:

• 1. Hare_2-participation

  An Example - assessment of measures for local level implementation of WFD Preparation is therefore vital Preparation (see also Hemmati 2002) • Specifying participatory and operational goals –Deciding on the link between process and actual decision-making processes • Securing funding • Stakeholder analysis and selection • Specifying rules of stakeholder communication • Getting stakeholder buy /media/loftslag/Hare_2-participation.pdf

• 2. Daniell_etal-2010

  /media/loftslag/Daniell_etal-2010.pdf

• 3. Lorenzoni_Pidgeon_2006

  taking into account the context, including multiple value preferences for characteristics and functions of natural and human systems, over short and longer timescales. Failure to take public values and views into consideration when taking decisions on climate risk management will inevitably prove problematic, for several reasons. At a basic level, climate policies will require a degree of ‘buy /media/loftslag/Lorenzoni_Pidgeon_2006.pdf

• 4. vonKorff_etal-2010

  bodies of management, decision-support, risk, and participation literature. d’Aquino (2008) Patrick d’Aquino relies on 20 years of implementation and evaluation experience, mostly in a natural resource management context and in developing countries. His approach is, at this point, the least conceptually developed design method of the guides presented here, although it is linked to a theoretical /media/loftslag/vonKorff_etal-2010.pdf

• 5. Factsheet_Bardarbunga_20141105

  and on the road into the area making observation of the eruption more difficult for the scientists in the field.  Seismic activity in Bardarbunga continues to be strong. Since Monday, the 3. of November, 200 earthquakes have been detected in the caldera. The largest measured earthquake was on Tuesday, November 4. at 20:45 of M4,8. A total of 15 earthquakes were of sizes between M 4 and 5; 15 of sizes /media/jar/Factsheet_Bardarbunga_20141105.pdf

• 6. Bárðarbunga 2015 - March, April, May

  by officers on site. The restricted area extends 20 m outside the edges of the new lava field, to the edge of Dyngjujökull glacier on the south side, the river Jökulsá á Fjöllum to the east and to the westernmost branches of Jökulsá á Fjöllum in the west. Enlarge. 12 March 2015 - from the Scientific Advisory Board Notes from the Meeting of the Scientific Advisory Board 10 March (pdf 0.3 Mb) are now /earthquakes-and-volcanism/articles/nr/3122

• 7. Bárðarbunga 2015 - March, April, May

  by officers on site. The restricted area extends 20 m outside the edges of the new lava field, to the edge of Dyngjujökull glacier on the south side, the river Jökulsá á Fjöllum to the east and to the westernmost branches of Jökulsá á Fjöllum in the west. Enlarge. 12 March 2015 - from the Scientific Advisory Board Notes from the Meeting of the Scientific Advisory Board 10 March (pdf 0.3 Mb) are now /earthquakes-and-volcanism/articles/nr/3122/

• 8. Bardarbunga-2015_MarchAprMay-events

  monitoring so that warnings may be issued if necessary. Vatnajökull National Park will issue locations of viewing areas. Information on evacuation routes will be issued by officers on site. The restricted area extends 20 m outside the edges of the new lava field, to the edge of Dyngjujökull glacier on the south side, the river Jökulsá á Fjöllum to the east and to the westernmost branches /media/jar/Bardarbunga-2015_MarchAprMay-events.pdf

• 9. Moellenkampetal_etal-2010

  supported by the majority of responses to one of the quantitative questions (to which 13 out of 20 participants responded on a five-point Likert scale—strongly agree, agree, neither agree or disagree, disagree, strongly disagree), where 11 respondents “agreed” that the activities in the workshop helped them to share their views and opinions with others, and the other two “neither agreed nor disagreed /media/loftslag/Moellenkampetal_etal-2010.pdf

• 10. Hydropower - Glacier, Snow and Ice

  Guðmundsson, S., Björnsson, H., Pálsson, F., Jóhannesson, T., Hannesdóttir, H. o.fl. (2011). Modelling the 20th and 21st century evolution of Hoffellsjökull glacier, SE-Vatnajökull, Iceland. The Cryosphere, 5, 961-975, doi:10.5194/tc-5-961-2011. Andreassen, L. M., & Oerlemans, J. (2009). Modelling long-term summer and winter balances and the climate sensitivity of Storbreen, Norway. Geogr. Ann., 91 /ces/publications/nr/1940