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Results:

• 21. Reykholt-abstracts

  lidar surveys Joaquín Muñoz-Cobo Belart, Eyjólfur Magnússon and Finnur Pálsson .......................... 11 Mass balance analysis of Drangajökull ice cap from historical photogrammetry and lidar Beata Csatho, Thorsten Markus and Thomas Neumann ................................................... 12 The ICESat-2 mission: design, applications and pre-launch performance assessments /media/vatnafar/joklar/Reykholt-abstracts.pdf

• 22. Lorenzoni_Pidgeon_2006

  level, surveys commissioned by the European Com- munity/the European Union provide an indication of trends in concern about cli- mate change. Since 1992, such surveys have been undertaken among representative samples of citizens in its Member States, and specifically on topics related to the environment (Special Eurobarometers (EB) in 1992, 1995, 2002; and a Flash EB in 2002). These have included /media/loftslag/Lorenzoni_Pidgeon_2006.pdf

• 23. VED_AnnualReport-2013_screen

  and our intention is to run these models dur- ing times of hazardous events and even on a daily basis to further improve monitoring. Avalanche monitoring has progressed. The em- phasis is now on improving our services, especially to the Icelandic Road and Coastal Administration with regard to transport. The reason is that com- munity structure has changed considerably in recent years and the need /media/vedurstofan/utgafa/arsskyrslur/VED_AnnualReport-2013_screen.pdf

• 24. Refsgaard_etal-2007-Uncertainty-EMS

  and possibly the stake- holders at different phases of the modelling project. Many QA guidelines exist such as Middlemis (2000) and Van Waveren et al. (1999). The HarmoniQuA project (Schol- ten et al., 2007; Refsgaard et al., 2005a) has developed a com- prehensive set of QA guidelines for multiple modelling domains combined with a supporting software tool, MoST (downloadable via http /media/loftslag/Refsgaard_etal-2007-Uncertainty-EMS.pdf

• 25. 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

• 26. VI_2019_009

  .............................................................. 10 3 Processing ................................................................................................... 12 4 Data Comparison ......................................................................................... 14 4.1 Bolungarvík.......................................................................................... 14 4.2 Höfn í Hornafirði /media/vedurstofan-utgafa-2019/VI_2019_009.pdf

• 27. VI_2016_006_rs

  ............................................................. 12 3 Landslide history ......................................................................................... 17 3.1 Historical landslides ............................................................................... 17 3.2 Prehistoric landslides .............................................................................. 19 4 Potential starting areas for landslides and debris /media/vedurstofan-utgafa-2016/VI_2016_006_rs.pdf

• 28. GA_2009_91A_4_Andreassen

  the principalmethods have not changed much over the years, theamount of field work has varied. In the first 15 yearsthe monitoring programme at Storbreen was com-prehensive, often three or more snow density pits were dug, snow depth was measured at about 600points and ablation was measured on 30 stakes evenly distri uted on the glacier (Liestøl 1967).Based on experience of the snow pattern, the ob- servations /media/ces/GA_2009_91A_4_Andreassen.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

  ) 555 535 391 753 664 480 % Glacierized area 0 0 0 11 20 12 % Grassland <1 43 25 15 10 25 % Woodland <1 0 0 0 2 2 % Moss 59 25 0 9 14 13 % Little or no vegetation 35 27 30 63 47 36 % Wetland 0 5 46 <1 6 7 % Lakes 6 <1 <1 <1 <1 3 10 3 Data Various meteorological and hydrological parameters were extracted and used to select ana- logues. 3.1 Hydrological data A set of six river basins of various /media/vedurstofan/utgafa/skyrslur/2013/VI_2013_008.pdf