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• 31. Hazard zoning

  a year, or its variations with the season. The maps are available in small and large domain. The numbers reported in brackets on the large domain map correspond to the number of times that some UST stations (marked with grey dots) measured a concentration higher than the threshold the map is referring to. The numbers refer to hourly averaged concentration of SO2. At a specific location /pollution-and-radiation/volcanic-gas/hazard-zoning

• 32. norsem_matthew

  river - Jökulsá á Fjöllum. The analysed seismic and infrasound measurements show how fluid movement can generate elastic waves that propagate through the ground and atmosphere. This underlines the potential for using tremor-amplitude and infrasonic measurements as an early warning for hazardous floods, particularly in regions where hydrological measurements are sparse. /media/norsem/norsem_matthew.pdf

• 33. 2011_005

  type is probably the least reliable because of its memory and operation system design. Comprehensive information on how much maintenance has been done for each model has not been collected, but it is advisable to do. In the near future, several of the oldest receivers will have to be upgraded with newer models. Number of receivers for each model is given in Table 5. Table 5. Receiver models /media/vedurstofan/utgafa/skyrslur/2011/2011_005.pdf

• 34. Factsheet_Bardarbunga_20140923

  along with representatives from the Icelandic Civil Protection and the Environmental Agency of Iceland. Main points  Volcanic eruption in Holuhraun  Air quality  Scenarios Notes  The volcanic eruption in Holuhraun continues with similar rate as last few days. The eruption does not seem to be declining. The lava production continues with the same strength.  The lava now flows /media/jar/myndsafn/Factsheet_Bardarbunga_20140923.pdf

• 35. Factsheet_Bardarbunga_20140924

  along with representatives from the Icelandic Civil Protection and the Environmental Agency of Iceland. Main points  Volcanic eruption in Holuhraun  Air quality  Scenarios Notes  The volcanic eruption in Holuhraun continues with similar rate as last few days. The eruption does not seem to be declining. The lava field continues to grow and the lava production continues /media/jar/myndsafn/Factsheet_Bardarbunga_20140924.pdf

• 36. Factsheet_Bardarbunga_20141114

  Convection of sulphuric dioxide from the crater appears to be constant.  Seismic activity in Bardarbunga continues to be strong but number of earthquakes stronger then M5,0 seem to be decreasing. The biggest earthquakes that were detected over the last two days were yesterday, 13. November at 20:46 of magnitude M4,9 and at 23:08 of magnitude M4,8. In total 17 earthquakes bigger then M4,0 were /media/jar/Factsheet_Bardarbunga_20141114.pdf

• 37. Kok_2-scenarios-lecture-2

  Backcasting: background Backcasting: key concepts Test how effective policy measures or other actions are, by evaluating them in a number of plausible futures Evaluate the plausibility of the storylines that have been used (can the future endstate envisioned in the story be reached with a set of concrete policy measures?) Identify ultimately a set of (policy) actions that will lead to a more /media/loftslag/Kok_2-scenarios-lecture-2.pdf

• 38. 2013_001_Nawri_et_al

  This section describes the numerical input data for this study and the associated wind atlas, and the parameterised boundary-layer model and statistical analyses used to process the data. It also addresses the spatial and temporal variability of air density, and its effects on wind energy potential. 3.1 Wind modelling The Icelandic network of weather stations is sufficient to provide a good overview /media/vedurstofan/utgafa/skyrslur/2013/2013_001_Nawri_et_al.pdf

• 39. FAQ

  FAQ FAQ How is the volcanic activitiy in Reykjanes Peninsula monitored? The IMO (Icelandic Meteorological Office /volcanoes/fagradalsfjall-eruption/faq/

• 40. norsem_slunga

  principal stresses. This indicates that the Coulomb failure criterion gives a good description of the crustal stresses. Tthe sizes of the shear stresses do not fit the shear strength of the rock but do fit the shear stresses limited by friction on shearing fractures. Extensive drillings have shown that the crustal rock contains large number of fractures (faults and joints of all sizes). All /media/norsem/norsem_slunga.pdf