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  • 51. NONAM

    Quiet giant Eyjafjallajökull 30th March 2010, shortly before an eruption began. Climate change will not affect the geophysical processes of volcanic eruptions but in the long run it may affect the icecaps much more than an eruption would. Photo: Baldur Sveinsson /nonam
  • 52. Lava flows

    can run. The hazard related to lava flow is more commonly on infrastructure, that is, damage or destruction of buildings or other structures i.e. power line and roads. Lava flows can also close off escape routes. Lava flows can threaten water sources due to pollution from the magma, it can also slow down the infiltration into aquifers. An example of damages from lava flows is the eruption /volcanoes/volcanic-hazards/lava-flow/
  • 53. NONAM

    Quiet giant Eyjafjallajökull 30th March 2010, shortly before an eruption began. Climate change will not affect the geophysical processes of volcanic eruptions but in the long run it may affect the icecaps much more than an eruption would. Photo: Baldur Sveinsson /nonam/
  • 54. Factsheet_Bardarbunga_20141110

    in Holuhraun. Most reliable are the forecast maps approved my meteorologist on duty, see Gas forecast. And although still being developed further, an automatic forecast, see Gas model, is also available (trial run, see disclaimer).  Measurements of air quality can be found on the webpage www.airquality.is Data from handheld gas monitors, spread around the country, can also be found on that page /media/jar/Factsheet_Bardarbunga_20141110.pdf
  • 55. Factsheet_Bardarbunga_20141126

    provides two-day forecasts on gas dispersion from the eruptive site in Holuhraun. Most reliable are the forecast maps approved my meteorologist on duty, see Gas forecast. And although still being developed further, an automatic forecast, see Gas model, is also available (trial run, see disclaimer).  Measurements of air quality can be found on the webpage www.airquality.is Data from handheld gas /media/jar/Factsheet_Bardarbunga_20141126.pdf
  • 56. ces_geus_paakitsoq_full_report

    to evaluate the potential for hydro-power production (Thomsen et al., 1989; Ahlstrøm, 2007). Future melt-water availability at Paakitsôq was assessed by Ahlstrøm et al. (2008a) based on a scenario run of a Regional Climate Model (RCM). The present study is performed in the framework of the Climate and Energy Systems (CES) project with the aim to better specify uncertainties in future scenarios /media/ces/ces_geus_paakitsoq_full_report.pdf
  • 57. Tomas_Johannesson_(IMO,_Ice)

    period. A new hazard zoning method was developed in Iceland after the snow avalanche accidents in 1995 and in 2000 a new regulation on avalanche hazard zoning was issued. The method and regulation are based on individual risk, or annual probability of death due to avalanches. The major components of the method are the estimation of avalanche frequency, run-out distribution /media/loftslag/Tomas_Johannesson_(IMO,_Ice).pdf
  • 58. VI2010-006_web

  • 59. Awards and press

    to keep an update on Bárðarbunga every day as well as the webcams." Appreciation under the Eyjafjallajökull eruption IMO web team appreciates comments like these from Sandra, 17 May 2010, although the webcams we link to are not run by us: "Thank you for providing a daily activity summary on your website that's in English. It's very helpful to have your experience and authority to rely /about-imo/the-web/awards_and_press/
  • 60. CES_D2_2_poster_3x3

    @fmi.fi THIS POSTER IS A SUBSET OF A DELIVERABLE REPORT AVAILABLE FROM http://www.atm.helsinki.fi/~jaraisan/CES_D2.2/CES_D2.2.html SOURCES OF UNCERTAINTY IN CLIMATE CHANGE FORECASTS A schematic view of sources of uncertainty in climate change as a function of time. In the long run, most of the uncertainty relates to the magnitude of greenhouse gas emissions (unknown future behaviour /media/ces/CES_D2_2_poster_3x3.pdf

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