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• 51. Bardarbunga_daily_status_report_21082014

  stations do near Bárðarbunga. The new GPS measurements will provide scientists with an improved understanding of how the magma is moving within the crust. Overall assessment There are no measurements to suggest that an eruption is imminent. Previous intrusion events in Iceland have lasted for several days or weeks, often not resulting in an eruption. However an eruption of Bárðarbunga cannot /media/jar/Bardarbunga_daily_status_report_21082014.pdf

• 52. Outline_for_the_case_Road_maintenance_in_a_changing_climate

  demand of road transport services directly, e.g. climate change may alter the supply chains in forest and food industries. The competitive position of road transport may change for better or worse, depending on how other modes respond to changing circumstances and risks, on the regulatory and costs effects of explicit adaptation policy, on the interaction with other policies (mitigation, clean /media/loftslag/Outline_for_the_case_Road_maintenance_in_a_changing_climate.pdf

• 53. 2013_001_Nawri_et_al

  the Fljótsdalsheiði region . . . . . . . 47 18 Seasonal mean wind power density within the Fljótsdalsheiði region . . . . . . . . 48 19 Directional mean wind power density within the Gufuskálar region . . . . . . . . . 49 20 Seasonal mean wind power density within the Gufuskálar region . . . . . . . . . . 50 21 Directional mean wind power density within the Hellisheiði region . . . . . . . . . 51 22 Seasonal mean /media/vedurstofan/utgafa/skyrslur/2013/2013_001_Nawri_et_al.pdf

• 54. Water_resources_man_Veijalainen_etal

  Based on a report by Verta et al. (2007) 92. 5 93. 0 93. 5 94. 0 94. 5 95. 0 M A MJ F J J A S O N D Mean 19702000 Min and max 1970–2000, natural rating curve Target water level zone 1 Target water level zone 2 Q=+20% Q=+10% Q= 0% Q=15% Q=30% 92.90 m snow target 1 92.70 m snow target 2 Water level (m ) Month the regulation limits Lake Syväri has target water level zones, which are not legally /media/ces/Water_resources_man_Veijalainen_etal.pdf

• 55. Grímsvötn 2010

  on 03 Nov. 2010. Flow direction is from the lower right to the upper left. Note how floodwater accumulates upstream from the bridge due to the constriction created by the levees of the bridge. At Grímsfjall mountain in Vatnajökull Aerial view of the eastern edge of Grímsfjall at 13:25 GMT on 03 Nov. 2010. Fresh crevasses at the base of Grímsfjall illustrate how the ice-cover over /hydrology/articles/nr/2040

• 56. Grímsvötn 2010

  on 03 Nov. 2010. Flow direction is from the lower right to the upper left. Note how floodwater accumulates upstream from the bridge due to the constriction created by the levees of the bridge. At Grímsfjall mountain in Vatnajökull Aerial view of the eastern edge of Grímsfjall at 13:25 GMT on 03 Nov. 2010. Fresh crevasses at the base of Grímsfjall illustrate how the ice-cover over /earthquakes-and-volcanism/articles/nr/2040

• 57. 2012-Refsgaard_etal-uncertainty_climate-change-adaptation-MITI343

  in climate change adaptation should reflect the nature of the uncertainty sources and how they interact with risk level and decision making: (i) epistemic uncertainties can be reduced by gaining more knowledge; (ii) uncertainties related to ambiguity can be reduced by dialogue Mitig Adapt Strateg Glob Change DOI 10.1007/s11027-012-9366-6 J. C. Refsgaard (*) Geological Survey of Denmark /media/loftslag/2012-Refsgaard_etal-uncertainty_climate-change-adaptation-MITI343.pdf

• 58. Information and help

  and temporally. Local avalanche danger may, thus, be in more areas than the bulletin describes, and avalanches may have released in more areas than reported. Nobody should travel in steep slopes during winter time without knowing how to assess avalanche danger and make appropriate terrain selection. The safety can be increased considerable by avoiding all terrain steeper than 30°. Should /avalanches/forecast/help

• 59. Factsheet_Bardarbunga_20141208

  outbreak.  Seismic activity in Bardarbunga continues to be strong. The strongest earthquake since noon on Friday, 5. December, was magnitude M5,1 on Friday at 21:05. About 20 earthquakes between M4,0-5,0 were detected since Friday and 10 earthquakes between magnitude M3,0-4,0. In total about 300 earthquakes were detected in Bardarbunga since noon on Friday.  Little seismic activity /media/jar/Factsheet_Bardarbunga_20141208.pdf

• 60. Factsheet_Bardarbunga_20150220

  to The Environment Agency through the email gos@ust.is. The Environment Agency is especially looking for information from people who have been in contact with high concentrations of gas; where they were, at what time it happened, how the gas cloud looked (colour and thickness of the cloud) and how they were affected by it.  The volcanic eruption has now been going on for almost half a year. The lava /media/jar/Factsheet_Bardarbunga_20150220.pdf