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Results:

• 21. Reykholt-abstracts

  ................................................................................................................... 8 Liss M. Andreassen, Hallgeir Elvehøy, Sindre Engh and Bjarne Kjøllmoen ..................... 9 Lidar measurements of Norwegian glaciers – an overview Neil Arnold* and Gareth Rees .............................................................................................. 10 Calculation of glacier velocity from repeat /media/vatnafar/joklar/Reykholt-abstracts.pdf

• 22. Hare-2011-ParticipatoryModelling

  Dispatch: 02.08.11 CE: E E T 5 9 0 No. of Pages: 19 ME: 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17 18 19 20 21 22 23 24 25 26 27 28 29 30 31 32 33 34 35 36 37 38 39 40 41 42 43 44 45 46 47 48 49 50 51 52 53 54 55 56 57 Another possible driving force behind its popularity is changing legislation requiring environmental managers and policy-makers to increase stakeholder participation in their work [e.g /media/loftslag/Hare-2011-ParticipatoryModelling.pdf

• 23. VI_2015_005

  This is also the case with cyclones in all three sectors. Cyclones in the eastern or western sector are also strongly affected by the presence of central cyclones. In both sectors, cyclones tend to move east, unless there are cyclones in the neighbouring sector, in which case pressure tendencies are reversed. 21 Figure 10. Composite mean temporal MSLP tendencies, for different MSLP modes. Com- posite mean /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_005.pdf

• 24. Lorenzoni_Pidgeon_2006

  and promoter of the Protocol and the UK has taken up a leading role on the issue, especially during its presidency of the EU and the G8 in 2005. The USA, on the other hand, as the greatest emitter of greenhouse gases, withdrew from the Kyoto Protocol in 2001 and has based its ∗Preasent address: School of Psychology, Cardiff University, Tower Building, Park Place, Cardiff CF 10 3AT, UK, E-mail /media/loftslag/Lorenzoni_Pidgeon_2006.pdf

• 25. Kok_JGEC658_2009

  ) describes a 10-step approach where narrative storylines are developed and linked to dynamic models in an iterative procedure. Stories are developed by a stakeholder panel consisting of the relevant actors in the region under study, while models are developed and applied by experts. Examples of global exercises that have used an approach similar to Story-and- Simulation include the Millennium /media/loftslag/Kok_JGEC658_2009.pdf

• 26. VI_2019_009

  ................................................................................................... 9 2 Instruments................................................................................................. 10 2.1 Vaisala Ceilometer (CL51) ....................................................................... 10 2.2 Vaisala Present Weather Detector /media/vedurstofan-utgafa-2019/VI_2019_009.pdf

• 27. 2013_001_Nawri_et_al

  . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 59 A.10 Melrakkaslétta . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 61 A.11 Mýrar . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 63 A.12 Skagi . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 65 A.13 Snæfellsnes /media/vedurstofan/utgafa/skyrslur/2013/2013_001_Nawri_et_al.pdf

• 28. VI_2016_006_rs

  of W-Strandartindur and the gullies below .................................................................................................. 23 4.5 Areas 7 and 8: Botnabrún ........................................................................ 24 4.6 Areas 9 and 10: Nautaklauf and Klauf ........................................................ 24 5 Assessment of the hazard potential /media/vedurstofan-utgafa-2016/VI_2016_006_rs.pdf

• 29. VI_2020_004

  for the Hekla eruptive scenario ............................... 30 Figure 9 Selected locations investigated for the Öræfajökull eruptive scenario ...................... 31 Figure 10 Basic structure of the methodology adopted for this study ..................................... 32 Figure 11 Vertical profile of the vertical velocity of the volcanc mixture. .............................. 33 Figure 12 /media/vedurstofan-utgafa-2020/VI_2020_004.pdf

• 30. VI_2013_008

  A A A A A Vatnajökull Mýrdalsjökull Hofsjökull Langjö k ull Drangajökull VHM-66 VHM-19 VHM-10 VHM-145 VHM-64 VHM-26 0 10050 Km A Gauging StationWatershedGlacier A m.a.s.l1 - 200200 - 400400 - 600600 - 800800 - 10001000 - 12001200 - 14001400 - 16001600 - 18001800 - 2000 Figure 1. Topography of Iceland and location of watersheds considered here. Table 1. Characteristics of the considered watersheds. Letter /media/vedurstofan/utgafa/skyrslur/2013/VI_2013_008.pdf