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• 11. The weather in Iceland in 2022

  but 0.3 below the mean of the last ten years. In Egilsstaðir the annual average was 4.0°C, 0.1°C above the 1991 to 2020 mean. In the country as a whole the temperature was equal to the 1991 to 2020 mean but 0.3°C below the mean of the last ten years. Table 1: Annual mean temperature at several stations, the deviation relative to the 1991-2020 mean and the deviation relative to the last ten /about-imo/news/the-weather-in-iceland-in-2022

• 12. 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

• 13. 2005EO260001

  The recognition of geophysical precursors to volcanic activity is a primary challenge in volcano monitoring. That challenge was successfully met by scientists at the Icelandic Meteorological Offi ce (IMO) before the 1 November 2004 eruption of Grímsvötn, a subglacial volcano beneath the Vatnajökull ice cap, Iceland (Figure 1). Seismic and geodetic precursors were prop- erly recognized /media/jar/myndsafn/2005EO260001.pdf

• 14. 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

• 15. Öræfajökull : Recent research

  (pdf 2.75 Mb)Pages 123–140Emmanuel PagneuxShort summaryChapter VII. Öræfajökull: Evacuation time modelling of areas prone to volcanogenic floods (pdf 2.96 Mb)Pages 141–164Emmanuel PagneuxShort summaryRecommended citation for individual chapters (example):Roberts, M. J., & Gudmundsson, M. T. (2015). Öræfajökull Volcano: Geology and historical floods. In E. Pagneux, M. T. Gudmundsson, S. Karlsdóttir /volcanoes/about-volcanoes/oraefajokull/new-research/

• 16. Lorenzoni_Pidgeon_2006

  findings from various surveys and studies, which highlight both the distinctiveness and some shared perspectives at a generalised level. We reflect upon these in relation to trust and responsibility for climate change action, and risk communication, supporting the call for discourses about climate change to also be situated in people’s locality, as a means of increasing its saliency. 1 /media/loftslag/Lorenzoni_Pidgeon_2006.pdf

• 17. VI_2022_006_extreme

  J. Roberts Tinna Þórarinsdóttir VÍ 2022-006 Skýrsla +3 5 4 522 6000 vedur@ve d u r.i s Veðursto f a Ísland s B ú sta ð a rve g u r 7–9 108 Reyk j a vík Contents 1 INTRODUCTION .................................................................................................................. 4 2 STUDY AREA /media/vedurstofan-utgafa-2022/VI_2022_006_extreme.pdf

• 18. VI_2009_013

  frá Kötlu og Upptyppingum. Upplýsingar um VOLUME verkefnið má finna á vefsíðunni: http://www.volume-project.net/ 7 Contents LIST OF FIGURES ............................................................................................................. 7  LIST OF TABLES .............................................................................................................. 8  1  ABSTRACT /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_013.pdf

• 19. VI_2009_006_tt

  the discharge in Skaftá and the temperature of the flood water close to the glacier margin were measured. The dis- charge from the subglacial lake during the jökulhlaup was calculated using a hypso- metric curve for the subglacial lake, estimated from the form of the surface cauldron after jökulhlaups. The maximum outflow from the lake during the jökulhlaup is esti- mated as 123 m3 s 1 while /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_006_tt.pdf

• 20. vanRoosmalen_etal-2009-WRR_2007WR006760

  and Irrigationa Scenario Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec Current 101 85 59 13
  6
  4
  1 6 39 79 84 97 A2 145 132 73 10
  10
  7
  6
  8 4 75 92 123 B2 137 119 75 16
  6
  6
  6
  5 21 74 110 141 aValues are in millimeters. 10 of 18 W00A15 VAN ROOSMALEN ET AL.: CLIMATE AND LAND USE CHANGE W00A15 time and larger area where groundwater levels rise above the drain levels. Table 6 shows the mean discharges /media/loftslag/vanRoosmalen_etal-2009-WRR_2007WR006760.pdf