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• 51. Bardarbunga_daily_status_report_21082014

  the Dyngjujökull glacier at 5 - 10 km depth. The dyke has not propagated to the north-east, nor has it progressed to shallower depth. Today three earthquakes exceeding three in magnitude have occurred on the caldera rim of Bárðarbunga (M 3.7 at 10:29, M 4.0 at 10:58 and M 3.4 at 13:02). These earthquakes were at depths around 2 - 5 km. They are interpreted as possible adjustments of the caldera due to changing /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

  effects . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 19 4 Evaluation of model results 22 5 Large-scale overview 26 5.1 Climatological wind conditions . . . . . . . . . . . . . . . . . . . . . . . . . . . . 26 5.2 Wind power density . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 31 6 Test sites 36 7 Conclusions 41 A Resource maps 42 A.1 Blanda /media/vedurstofan/utgafa/skyrslur/2013/2013_001_Nawri_et_al.pdf

• 54. Water_resources_man_Veijalainen_etal

  Volume 24, Number 13 Water Resour Manage (2010) 24:3437–3459 DOI 10.1007/s11269-010-9614-z Climate Change Impacts on Water Resources and Lake Regulation in the Vuoksi Watershed in Finland Noora Veijalainen · Tanja Dubrovin · Mika Marttunen · Bertel Vehviläinen Received: 12 July 2009 / Accepted: 22 February 2010 / Published online: 24 March 2010 ³ Springer Science+Business Media B.V. 2010 Abstract /media/ces/Water_resources_man_Veijalainen_etal.pdf

• 55. Grímsvötn 2010

  outburst flood in 2010 3.11.2010 Jökulhlaup from Grímsvötn subsides - 5 November 2010 The jökulhlaup (glacial outburst flood) from Grímsvötn that began near the end of October is now coming to an end. See thorough description in news on front page. Assessment - 5 /hydrology/articles/nr/2040

• 56. Grímsvötn 2010

  outburst flood in 2010 3.11.2010 Jökulhlaup from Grímsvötn subsides - 5 November 2010 The jökulhlaup (glacial outburst flood) from Grímsvötn that began near the end of October is now coming to an end. See thorough description in news on front page. Assessment - 5 /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

  a truck; destroy a small building or break a few trees. 1000 tonn 4 Could bury and destroy a railway car, large truck, several buildings or a piece of forest. 10.000 tonn 5 Could gouge the landscape; disastrous damage potential. 100.000 tonn It is not always easy or obvious how to classify the size of an avalanche, however, the destructive potential is the predominant /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

   The rate of the subsidence in Bárðarbunga caldera had decreased substantially. But that is not the whole story. Ice is subsiding into the caldera with the effect that the GPS station does not show any changes. The estimated depression of the rock foundation of the caldera, in the light of the ice subsidence, is about 5 cm per day. The flow of magma from under Bárðarbunga is believed /media/jar/Factsheet_Bardarbunga_20150220.pdf