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• 11. CES_D2.4_task1

  :18:00 +14:46:59 11 TP 118 SANDVIG DK +55:16:59 +14:46:59 12 TP 119 KOEBENHAVN: LANDBOHOJSKOLEN DK +55:40:59 +12:31:59 9 T 178 BARKESTAD NO +68:49:00 +14:48:00 3 P 180 LIEN I SELBU NO +63:12:32 +11:06:56 255 P 181 MESTAD I ODDERNES NO +58:12:55 +07:53:26 151 P 183 NORD ODAL /media/ces/CES_D2.4_task1.pdf

• 12. Wind turbines

  and each spade measures 22 metres in length. When the spades are at their highest position each unit will achieve a height of 77 metres. Like all large structures, wind turbines have an inevitable visual impact. However, a permanent impact on the overall appearance of the environment is not considered high in comparison to other types of power plants. Wind turbines can be easily dismantled, leaving /about-imo/news/nr/2642

• 13. 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

• 14. The weather in Iceland in 2022

  Miðfjarðarnes 765.4 # 124 60.2 214 104 Skjaldþingsstaðir 1199.6 # 93 43.4 226 131 Dalatangi 1610.3 97 94 55.1 264 161 Höfn í Hornafirði 1642.9 # 109 52.2 199 163 Vatnsskarðshólar 1639.8 95 90 37.2 251 178 Hjarðarland 1377.6 103 104 47.5 194 /about-imo/news/the-weather-in-iceland-in-2022

• 15. 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

• 16. 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

• 17. Huntjens_etal-2010-Climate-change-adaptation-Reg_Env_Change

  ORIGINAL ARTICLE Climate change adaptation in European river basins Patrick Huntjens • Claudia Pahl-Wostl • John Grin Received: 1 July 2008 / Accepted: 24 December 2009 / Published online: 2 February 2010  The Author(s) 2010. This article is published with open access at Springerlink.com Abstract This paper contains an assessment and stan- dardized comparative analysis of the current water man /media/loftslag/Huntjens_etal-2010-Climate-change-adaptation-Reg_Env_Change.pdf

• 18. 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/

• 19. 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 '/

• 20. 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 '/