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• 21. Kok_2-scenarios-lecture-2

  understand the driving forces leading to land degradation and desertification in the Northern Mediterranean and to contribute to policy- making to address these issues Scenarios 2000-2030 Decision Support Systems Policy Support Framework Stake- holders Main products of MedAction Workshops with Local actors Target Area Scenarios Multi-scale scenario development 3 European Scenarios (from VISIONS) 3 /media/loftslag/Kok_2-scenarios-lecture-2.pdf

• 22. 2011_005

  ........... 31 Table 21. Recommended survey stations for the national network. ...................................... 36 Table 22. Recommended monitoring stations for volcanic activity. ...................................... 36 7 1 Introduction The group's main task was to assess the present status of the CGPS network, focusing on hardware issues, communication routes, network optimization, data /media/vedurstofan/utgafa/skyrslur/2011/2011_005.pdf

• 23. IMO at the Arctic Circle Assembly 2017

  at IMO, participated off-venue in a workshop on "Energy in the Arctic".Aldís Elfarsdóttir, currently working as an intern at IMO, worked with the Arctic Circle management team during the assembly, writing statements for the Arctic Circle´s social media accounts on Twitter and Facebook.More pictures from the conference and IMO sessions are online, by OZZO Photography /about-imo/news/imo-at-the-arctic-circle-assembly-2017

• 24. Kok_JGEC658_2009

  Change 19 (2009) 122–133 A R T I C L E I N F O Article history: Received 14 November 2007 Received in revised form 21 August 2008 Accepted 25 August 2008 Keywords: Fuzzy Cognitive Maps Scenario Participation Resilience Brazil A B S T R A C T The main drawback of the Story-and-Simulation approach is the weak link between qualitative and quantitative scenarios. A semi-quantitative tool, Fuzzy /media/loftslag/Kok_JGEC658_2009.pdf

• 25. VI_2020_005

  . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 9 2 Background . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 11 2.1 Factors affecting sea level . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 12 2.1.1 Main factors affecting sea level in Scandinavia, the UK and Iceland . . . . 13 2.2 Sea level data /media/vedurstofan-utgafa-2020/VI_2020_005.pdf

• 26. VI_2014_005

  and rivers), and ocean (including sea ice) (Le Moigne, 2009). SURFEX uses input from the 1Further information can be found online at http://hirlam.org/index.php/documentation/harmonie. 2In this section, expressions in parentheses refer to parameter values and settings in the config_exp.h model configuration file. 7 lowest level of the atmospheric model, together with static fields describing the model /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_005.pdf

• 27. Lorenzoni_Pidgeon_2006

  to other environmental, personal and social issues. For instance, although 62% of respondents of a 2002 British sur- vey maintained they were fairly to very concerned about climate change (Poortinga and Pidgeon, 2003a), typically their main priorities lay with health, family, safety and finances. These results are consistent with the findings of a 1997 survey among 1225 US citizens, indicating /media/loftslag/Lorenzoni_Pidgeon_2006.pdf

• 28. 2013_001_Nawri_et_al

  values. For Part 2, data files describing the local wind statistics on the regular model grid covering Iceland are made available through an online wind atlas (follow the link from http://www.vedur.is/vedur/vedurfar/vindorka/). The files contain estimates of Weibull parameters at each grid point, for twelve wind direction sectors, five heights (10, 25, 50, 100, 200 m above ground level (mAGL /media/vedurstofan/utgafa/skyrslur/2013/2013_001_Nawri_et_al.pdf

• 29. 2010_012rs

  operation of the SIL automatic seismic system in Iceland, the network has recorded foreshocks before all medium to large earthquakes in SW-Iceland. If such foreshocks can be located with high-precision before the following main shock occurs, the foreshocks may already have delineated the fault plane of the coming main shock, thus allowing its fault plane to be immediately inferred /media/vedurstofan/utgafa/skyrslur/2010/2010_012rs.pdf

• 30. VI_2016_006_rs

  in the future due to warming climate. There is geological evidence for three or four large, prehistoric landslides reaching the Fjarðará river or the sea below Botnabrún during the last several thousand years that demonstrates that danger due to large landslides extends to essentially all the current settlement south of Fjarðará. The main source areas for landslides that threaten the settlement /media/vedurstofan-utgafa-2016/VI_2016_006_rs.pdf