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• 11. 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/

• 12. 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

• 13. Traffc-maintenance_expenditures

  362 1975 29 182 96 108 5 630 130 753 - 1 597 6 708 4 435 2 697 - - - 277 111 1 306 154 1974 24 528 82 192 3 441 119 169 - 1 176 7 717 3 555 3 012 - - - 244 792 1 385 993 1973 21 401 66 649 3 725 117 723 - 1 769 6 430 3 219 3 123 - - - 224 040 1 602 542 1972 19 347 62 519 2 126 108 481 - 1 539 6 664 2 584 1 774 - - - 205 035 1 688 811 1971 17 268 47 427 2 390 96 727 - 548 6 046 2 349 474 - - - 173 /media/loftslag/Traffc-maintenance_expenditures.pdf

• 14. The weather in Iceland in 2022

  156 Stykkishólmur 794.1 108 107 29.8 211 136 Hólar í Dýrafirði 940.9 # 79 62.5 236 132 Litla-Ávík 874.1 # 100 30.2 245 149 Sauðanesviti 1252.5 142 133 57.9 234 153 Akureyri 600.9 105 92 33.2 203 115 Grímsstaðir 551.4 141 123 23.9 234 124 /about-imo/news/the-weather-in-iceland-in-2022

• 15. The weather in Iceland in 2018

  A record snow depth for December (105 cm) was also reached in Akureyri on 3 December. The greatest snow depth measured in the country was 123 cm, at Lerkihlíð on 9 March. The number of days with snow cover in Reykjavík was above normal in February and May and below normal in March, November and December. In Akureyri the days with total snow cover was above normal in January /about-imo/news/the-weather-in-iceland-in-2018

• 16. VI_2013_006

  lightning by the ATDnet system during (a) Grímsvötn 2004, (b) Eyjafjallajökull 2010 and (c) Grímsvötn 2011. A blue circle is at the vent location. 11 Figure 5. A map view, North (km) vs. East (km), of Grímsvötn 2011 lightning for the first 30 min (123 lightning), 1 hour (888), 3 hours (3340) and 24 hours (16041). The actual eruption site is marked with a black circle /media/vedurstofan/utgafa/skyrslur/2013/VI_2013_006.pdf

• 17. 2005EO260001

  (1995), Absolute and relative locations of similar events with application to microearthquakes in southern Iceland, Geophys. J. Int., 123, 409-419. Author Information K. S. Vogfjörd, S. S. Jakobsdóttir, G. B. Gudmundsson, M. J. Roberts, K. Ágústsson, T. Arason, H. Geirsson, S. Karlsdóttir, S. Hjaltadóttir, U. Ólafsdóttir, B. Thorbjarnardóttir, T. Skaftadóttir, E. Sturkell, E. B. Jónasdóttir /media/jar/myndsafn/2005EO260001.pdf

• 18. Paper-Olafur-Rognvaldsson_91

  The role of orography was found to be crucial in determining the precipitation dis- tribution and amount. Atmospheric flow over Iceland was simulated for the period January 1961 through June 2006 using version 3–7–3 of the PSU/NCAR MM5 mesoscale model (Grell et al., 1995). The domain used is 123× 95 points, centered at 64◦ N and 19.5◦ W, with a horizontal resolution of 8 km. There are 23 vertical /media/ces/Paper-Olafur-Rognvaldsson_91.pdf

• 19. Lorenzoni_Pidgeon_2006

  that personal and social goals take priority over other issues, including environmental ones (Bord et al., 1998; see also Palmgren et al., 78 I. LORENZONI AND N. F. PIDGEON Figure 2. Percentage of respondents in the EU-15 worried “very much” or “quite a lot” about future trends in climate change (Flash EB 123; Eos Gallup Europe, 2002). In comparison to the other three issues people were asked about /media/loftslag/Lorenzoni_Pidgeon_2006.pdf

• 20. VI_2022_006_extreme

  77 91 109 Hraunaveita 132 116 136 159 117 140 169 Kvíslaveita 48 42 49 58 42 51 61 Sultartangi 66 57 68 80 58 69 84 Þingvallavatn 96 84 99 117 85 102 123 Þórisvatn 47 41 49 57 42 50 60 Tungnaá 76 67 79 92 67 80 98 Ufsarlón 104 92 108 126 93 112 134 36 Figure 19 – 1M5 maps for catchment Hálslón based on the ICRA dataset without projection (top left), with RCP 2.6 and 10th percentile /media/vedurstofan-utgafa-2022/VI_2022_006_extreme.pdf