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Results:

• 1. programme2---PhD-Workshop-preceding-Adaptation-Research-Conference

  During the conference all of you are requested to act as rapporteur in two or three sessions. A preliminary allocation of rapporteur sessions has been made (see below), while accounting for your expertise in certain areas. Participants can suggest changes in the rapporteur session allocation, on the condition a convincing argumentation is provided as well as a confirmed alternative rapporteur /media/loftslag/programme2---PhD-Workshop-preceding-Adaptation-Research-Conference.pdf

• 2. Avalanche dams

  ofan byggðarinnar. (Náttúrufræðingurinn, 69, 1, 3−10, 1999, authors T. Jóhannesson, O. Pétursson, J. G. Egilsson and G. G. Tómassson) [abstract] (html) A map on a selected front page shows recent observations of avalanches. For user access to avalanche and landslide data, an avalanche map viewer is available /avalanches/imo/dams/

• 3. hafisskyrsla_11052011

  Hafísskýrsla TF-SIF 11. maí 2011 Flug nr. 03511.025 Ískönnunarflug 11. maí 2011 Í dag var farið í ískönnunarflug um vesturmið. Enginn hafís var sjáanlegur í íslenskri lögsögu, en þéttur hafís rétt inn þeirrar grænlensku. Gerðum hafískönnun með SLAR ratsjá og ELTA eftirlitsratsjá. Skyggni á svæðinu leifði ekki athugun með berum augum. Hér að neðan fylgir punktalisti yfir legu /media/hafis/skyrslur_lhg/hafisskyrsla_11052011.pdf

• 4. IMO_AnnualReport2014

  used to produce probabilistic hazard maps for SO2 concentration at ground. The maps have been produced using a wind statistics based on 10 years. The final prod- ucts have been adopted by the Civil Protection for the definition of the restricted area around the eruption site. Baldur Bergsson, Árni Snorrason and Amy Donovan measuring gas at Holuhraun. Photo: Hermann Arngrímsson. Bárðarbunga /media/vedurstofan/utgafa/skyrslur/2015/IMO_AnnualReport2014.pdf

• 5. Recent publications

  The Icelandic Meteorological Office annually publishes a variety of reports, journals and articles. Below are examples of recent publications, most of which contribute to Arctic issues in general. Large-scale atmospheric conditions associated with major avalanche cycles and cold season weather hazards in Iceland (2013) The wind energy potential of Iceland (2013) Surface wind and air temperature over /about-imo/arctic/completed-projects/publications/

• 6. Joining forces in weather forecasting and climate research

  Panel on Climate Change (IPCC) described the unprecedented changes to the global climate as a ‘ code red for humanity '. We are experiencing more extreme weather patterns due to a warmer global climate, and with global temperatures projected to increase further over the next decades, weather patterns are expected to become more extreme and more challenging to forecast.The collaboration between /about-imo/news/joining-forces-in-weather-forecasting-and-climate-research

• 7. Avalanches in Iceland

  and landslides have caused both death and injury and done great damage to infrastructure and property in Iceland. In the twentieth century, 193 persons died, thereof 69 persons after 1974. Financial cost between 1974 and 2000 amounts to 3.3 billion IKR. Catastrophic avalanches in the villages Súðavík (January) and Flateyri (October) 1995, which killed 34 people and caused extensive economic damage /avalanches/avalanches

• 8. Avalanches in Iceland

  and landslides have caused both death and injury and done great damage to infrastructure and property in Iceland. In the twentieth century, 193 persons died, thereof 69 persons after 1974. Financial cost between 1974 and 2000 amounts to 3.3 billion IKR. Catastrophic avalanches in the villages Súðavík (January) and Flateyri (October) 1995, which killed 34 people and caused extensive economic damage /avalanches/avalanches/

• 9. Flood from Skaftá

  eastern and western, are located in the western part of Vatnajökull Ice-cap. They form because of geothermal activity that melts the glacier from below and water accumulates beneath them. When the hydro static pressure is high enough for the water to lift the ice above and flow from below the cauldrons it causes a flood. Floods from the eastern-cauldron are usually larger than the floods /about-imo/news/flood-in-estern-skafta

• 10. Flood from Skaftá

  eastern and western, are located in the western part of Vatnajökull Ice-cap. They form because of geothermal activity that melts the glacier from below and water accumulates beneath them. When the hydro static pressure is high enough for the water to lift the ice above and flow from below the cauldrons it causes a flood. Floods from the eastern-cauldron are usually larger than the floods /about-imo/news/flood-in-estern-skafta/