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  • 61. Bárðarbunga 2014 - September events

    that the lava was still flowing northwards, possibly also east according to thermal images but that has not been confirmed by the field team. Displacements: The subsidence of the Bárðarbunga caldera continues with same rate as before. GPS measurements show continuing slow movements. Water monitoring: No change was detected in water monitoring. Forcast for gas dispersion: For the next few days many low /earthquakes-and-volcanism/articles/nr/3001
  • 62. Bardarbunga-2014_September-events

    was detected in water monitoring. Forcast for gas dispersion: For the next few days many low pressure areas will pass Iceland. Wind direction will be changing quite frequently. In such conditions gas dispersion forecasting is difficult. The gas should move quite rapidly with the winds, and not accumulate in one specific area. After the weekend, south and southeast winds are prevalent /media/jar/Bardarbunga-2014_September-events.pdf
  • 63. Bárðarbunga 2014 - September events

    that the lava was still flowing northwards, possibly also east according to thermal images but that has not been confirmed by the field team. Displacements: The subsidence of the Bárðarbunga caldera continues with same rate as before. GPS measurements show continuing slow movements. Water monitoring: No change was detected in water monitoring. Forcast for gas dispersion: For the next few days many low /earthquakes-and-volcanism/articles/nr/3001/
  • 64. Eriksson_Garvill_Nordlund_2006

    (see e.g. Steg, 2003). In studies from several countries, push measures are perceived as less acceptable compared to pull measures (e.g. Ho¨lzer, 2003; Rienstra, Rietveld, & Verhoef, 1999; Steg & Vlek, 1997). For example, in a European study, over 90% of the car users supported improved public transport and park-and-ride schemes, while less than 20% approved of reduced parking space and cordon /media/loftslag/Eriksson_Garvill_Nordlund_2006.pdf
  • 65. BIIS_windrose_2005-2014

    1 6 Wind rose BIIS March 2005−2014 90 80 70 60 50 40 30 2010360350340 330 320 310 300 290 280 270 260 250 240 230 220 210 200 190 180 170 160 150 140 130 120 110 100 2 4 6 8 10 12 Frequency of wind direction (%) Aerodrome Total observations: 2611 Calm: 9.8% Variable winds: 16% Average wind speed for wind direction Wind direction (°) Wind speed (knots ) 0 5 10 15 0 45 90 135 180 225 270 315 360 N /media/vedur/BIIS_windrose_2005-2014.pdf
  • 66. Hare-2011-ParticipatoryModelling

    basic forms of participatory modelling, identied by classifying nine example participatory modelling processes. The second part considers the potential widespread adoption of participatory modelling by resource managers in the water sector, concluding that this potential is low. It proposes recommendations as to how the potential for the adoption of participatory modelling by water managers can /media/loftslag/Hare-2011-ParticipatoryModelling.pdf
  • 67. Factsheet_Bardarbunga_20141203

    University of Iceland along with representatives from the Icelandic Civil Protection, the Environmental Agency of Iceland, Vatnajokull National Park and the Directorate of Health. Main points  An overview of the activity in Bardarbunga and the volcanic eruption in Holuhraun  Air quality  Scenarios Notes  Today the Scientific Advisory Board of the Icelandic Civil Protection /media/jar/Factsheet_Bardarbunga_20141203.pdf
  • 68. The landslide in Seyðisfjörður is the largest landslide

    slopes; these are comparable to the landslides that have occurred in several places in recent weeks, as shown on the map above.Althingi ‒ the national parliament of Iceland ‒ recently approved a five-year budget plan, increasing government funding for the construction of avalanche defences by 1.6 billion ISK annually. The funding means that the construction of defence structures in hazardous /about-imo/news/the-landslide-in-seydisfjordur-is-the-largest-landslide-to-have-damaged-an-urban-area-in-iceland
  • 69. The landslide in Seyðisfjörður is the largest landslide

    slopes; these are comparable to the landslides that have occurred in several places in recent weeks, as shown on the map above.Althingi ‒ the national parliament of Iceland ‒ recently approved a five-year budget plan, increasing government funding for the construction of avalanche defences by 1.6 billion ISK annually. The funding means that the construction of defence structures in hazardous /about-imo/news/the-landslide-in-seydisfjordur-is-the-largest-landslide-to-have-damaged-an-urban-area-in-iceland/
  • 70. Snorrason_Arni_CES_2010

    and hydrology. • Climate and hydrological projections for the near future (2020-2050). • Effects of a changing climate and hydrology on renewable energy. • Risks and opportunities for renewable energy caused by climate change. • Adaptation strategies. Toppforskningsinitiativet (TFI) Budget: DKK 400 million over 5 years Joint funding through: Nordic Council of Ministers National Funding /media/ces/Snorrason_Arni_CES_2010.pdf

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