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• 21. 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

• 22. 2010_005_

  Century control runs, as well as 21st Century forecast runs, submitted by various institutions to the Intergovernmental Panel on Climate Change (IPCC) for their Forth 11 Table 1. General circulation and regional climate models that were considered in this study. Model Version Model Name, Institute BCCR BCM 2.0 Bergen Climate Model, Bjerknes Centre for Climate Research, Bergen, Norway CCCMA CGCM 3.1 /media/ces/2010_005_.pdf

• 23. Group2-PresentationWithPictures[1]

  Scenarios for Horsens Fjord Al Azhar, Bjarke, Maria and Kerstin 26.08.2011 Scenarios for Horsens Fjord • Horsens Fjord • Policy agency and stakeholders • Several goals, focus on water quality • Backcasting to develop scenarios • Uncertainties Exploring Backcasting Collective Individual Society 3 Scenario process: socio economic Society 1 Society 2 Scenario process: climate /media/loftslag/Group2-PresentationWithPictures[1].pdf

• 24. 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

• 25. 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/

• 26. Publications 2012

  Nawri, Halldór Björnsson, Guðrún Nína Petersen & Kristján Jónasson 44 pp 3,1 Mb 2012-009 Empirical Terrain Models for Surface Wind and Air Temperature over Iceland Nikolai Nawri, Halldór Björnsson, Guðrún Nína Petersen & Kristján Jónasson 33 pp 1,8 Mb 2012-008 Surface Wind and Air Temperature over Iceland based on Station Records and ECMWF Operational Analyses Nikolai Nawri /about-imo/publications/2012/

• 27. Bardarbunga_Daily_status_report_260814

  a significant part, or all, of the fissure is beneath the glacier. This would most likely produce a flood in Jökulsá á Fjöllum and perhaps explosive, ash-producing activity. Other scenarios cannot be excluded. For example, an eruption inside the Bárdarbunga caldera is possible but presently considered to be less likely. /media/jar/Bardarbunga_Daily_status_report_260814.pdf

• 28. Eyjafjallajokull_status_2010-05-18_IES_IMO

  measurements, web cameras, ATDnet – UK Met. Offices lightning detection system, NOAA satellite images and web-based ash reports from the public. Eruption plume: Height (a.s.l.): According to radar observations, the plume has been mostly at 7 km/21,000 ft. South and southwesterly winds (25-35 kt) over the volcano. Near the surface, the wind was easterly, blowing ash from the ground /media/jar/Eyjafjallajokull_status_2010-05-18_IES_IMO.pdf

• 29. Eyjafjallajokull_status_2010-06-11_IES_IMO

  water to flow up onto a road west of a bridge, as there it now not much difference between the height of the bridge and the river channel. Conditions at eruption site: A lake, about 300 m in diamenter, has formed at the bottom of the big crater. Steam is rising from the rims, especially from the north side. In the morning the steam cloud only rose about 100 m over the crater /media/jar/Eyjafjallajokull_status_2010-06-11_IES_IMO.pdf

• 30. Eyjafjallajokull_status_2010-06-15_IES_IMO

  been observed at GPS stations at or around the glacier. However, a station at the northeastern caldera rim (AUST), moved about three centimeters towards the southwest from the 9th to the 13th of June, inward to the caldera. Overall assessment: The level of water in the crater lake only rose about 1 – 2 meters over the weekend. Several days or weeks are therefore likely to pass /media/jar/Eyjafjallajokull_status_2010-06-15_IES_IMO.pdf