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• 21. CES_D2.4_task1

  :51 +11:39:06 123 P 2589 RYGGE NO +58:22:59 +10:47:17 40 TP 2590 SARPSBORG NO +59:17:08 +11:06:52 57 P 2591 STROMSFOSS SLUSE NO +59:18:02 +11:39:38 113 P 2592 MOSS NO +59:26:02 +10:40:00 31 P 2593 MOSS BRANNSTASJON NO +59:26:34 +10:41:03 32 P 2594 ASKER /media/ces/CES_D2.4_task1.pdf

• 22. Eriksson_Garvill_Nordlund_2006

  -orientation. Subsequently, a mean for the 15 NEP items was calculated for each respondent, represent- ing a measure of pro-environmental orientation (Dunlap et al., 2000). The scale had a reasonably high internal consistency (a ¼ 0:77). Problem awareness was calculated using the mean of the five items regarding the extent to which private car use was perceived as a global, local, and personal threat /media/loftslag/Eriksson_Garvill_Nordlund_2006.pdf

• 23. 2010_003rs

  is N197°E. The J21 fault, on the other hand, is more linear but with varying dip. South of the epicentre the fault is vertical but north of it, dip changes to 77°. It is 15.5 km long, strikes N179°E and deepens to the south from 6 km to 9 km. Many other smaller faults in Southwest Iceland that were illuminated by the 2000 activity have also been mapped, including the fault planes of three M~5 /media/vedurstofan/utgafa/skyrslur/2010/2010_003rs.pdf

• 24. hafisskyrsla_11052011

  Eins og sjá má af meðfylgjandi korti er ísinn næst landi um 77 sjml NNV af Straumnesi, 82 sjml NV af Horni, og 146 sjml N af Skaga. Ekki var unnt að greina ísinn vel sökum lágskýja, en útbreiðsla sést vel á SLAR myndum, sem og á eftirlitsratsjá. Ísdreifar voru að sjá á ratsjá um 1-2 sjómílur frá megin ísröndinni. Gunnar Örn Arnarson Yfirstýrimaður TF-SIF /media/hafis/skyrslur_lhg/hafisskyrsla_11052011.pdf

• 25. The weather in Iceland 2014

  Hornafirði 6.5 1.9 1.2 Fagurhólsmýri 6.4 1.8 1 112 0.9 Stórhöfði 6.2 1.4 2 138 0.4 Hveravellir 0.9 1.9 2 50 0.6 Árnes 5.3 1.7 2 134 0.7 Eyrarbakki 5.6 1.5 3 123 0.4 Annual temperature at a few stations and deviation from the 1961 to 1990 and 2004 to 2013 averages. The highest annual temperature was registered in Surtsey (off the South coast), 7.2 /about-imo/news/nr/3082

• 26. Markarfljót outwash plain and Öræfajökull

  the results should be considered carefully by the local and national authorities for planning and emergency evacuation purposes. Chapter VI. Öræfi district and Markarfljót outwash plain: Spatio-temporal patterns in population exposure to volcanogenic floods (pdf 2.75 Mb) Pages 123–140 Emmanuel Pagneux Short summary A spatio-temporal exploration of population exposure is performed /hydrology/hazard-risk-assessments/glacial-outburst-floods/markarfljotsaurar-oraefajokull/

• 27. ved-eng-2014

  5.8 2.1 1 142 1.1 Höfn í Hornafirði 6.5 1.9 1.2 Fagurhólsmýri 6.4 1.8 1 112 0.9 Stórhöfði 6.2 1.4 2 138 0.4 Hveravellir 0.9 1.9 2 50 0.6 Árnes 5.3 1.7 2 134 0.7 Eyrarbakki 5.6 1.5 3 123 0.4 Annual temperature at a few stations and deviation from the 1961 to 1990 and 2004 to 2013 averages. The highest annual temperature was registered in Surtsey (off the South coast), 7.2°C /media/vedurstofan/utgafa/skylduskil/ved-eng-2014.pdf

• 28. Hare-2011-ParticipatoryModelling

  Resources Management approach. Copyright © 2011 John Wiley & Sons, Ltd and ERP Environment. Keywords: adaptive management; participation; model adoption; participatory modelling; policy-science Introduction PARTICIPATORY MODELLING DESCRIBES A DIVERSE RANGE OF MODELLING ACTIVITIES WHOSE COMMON ELEMENT IS THATthey involve stakeholders in one or more stages of the modelling process, from data collection /media/loftslag/Hare-2011-ParticipatoryModelling.pdf

• 29. VONA message

  reached its peak discharge yesterday morning (05.12). The ice-shelf in Grímsvötn has subsided 77 m since the flood started and the rate of the subsidence has decreased significantly since yesterday. The discharge in Gígjukvísl river was measured twice yesterday, 2800 m3/s around noon and 2310 m3/s in the afternoon. Therefore it is assumed that the maximum discharge of the glacial flood was reached /earthquakes-and-volcanism/volcanoes/vona-notifications/

• 30. VONA message

  reached its peak discharge yesterday morning (05.12). The ice-shelf in Grímsvötn has subsided 77 m since the flood started and the rate of the subsidence has decreased significantly since yesterday. The discharge in Gígjukvísl river was measured twice yesterday, 2800 m3/s around noon and 2310 m3/s in the afternoon. Therefore it is assumed that the maximum discharge of the glacial flood was reached /earthquakes-and-volcanism/volcanoes/vona-notifications/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/' link '/