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• 31. ESC-IASPEI-statement-LAquila-2012-1

  of IASPEI's most brilliant scientists, who dedicated their lives to the reduction of seismic risk and to whom go our sympathy and support. , on behalf of the world community of seismologists, expresses its deepest concern for the L’Aquila verdict and prison sentence, that condemns for involuntary manslaughter seven prominent Italian scientists and members of the Great Risks Commission /media/vedurstofan/utgafa/hlidarefni/ESC-IASPEI-statement-LAquila-2012-1.pdf

• 32. Moberg_Anders_CES_2010

  1500 years and IPCC future temperature scenarios • Significant climate changes have occurred in the last millennium – affecting both temperature and hydrology • Future changes in this century will likely go substantially beyond what we have seen in the recent past IPCC 2007, SPM Fig. 5Mann et al. Science 2009, 326, p.1257, Fig. 1 /media/ces/Moberg_Anders_CES_2010.pdf

• 33. norsem_slunga

  are as large as the friction allows) directly leads to boundaries on the k-values and that these curves not only has a simple physical meaning, they also show a significant difference from the numerical fitting. This encouraged me to later go on and use the same assumptions to put boundaries on the pore pressure within wet crust which then was the base for the QuakeLook complete stress /media/norsem/norsem_slunga.pdf

• 34. Hare_2-participation

  and groups come and go frrom processes (how do you keep them turning up year after year?) • Participatory burn-out – legislators want it everywhere – too often with not enough results 5. Overselling of participation the tyranny of participation? Cooke & Kothari (2000) • Experiences in Cooperation and Development projects – Ignorance of existing power structures in local communities • Which /media/loftslag/Hare_2-participation.pdf

• 35. Update on the earthquake swarm in Geldingadalir

  there were around 1300 earthquakes detected in the Reykjanes peninsula as a whole. This is a lot less than the day before when around 2300 earthquakes were detected. The scientific Advisory board for the civil protection services met on the 27th of December to go over the situation near Fagradalsfjall. GPS instruments and satellite interferograms show that the magmatic intrusion is limited /about-imo/news/update-on-the-eruption-in-geldingadalir

• 36. Update on the earthquake swarm in Geldingadalir

  there were around 1300 earthquakes detected in the Reykjanes peninsula as a whole. This is a lot less than the day before when around 2300 earthquakes were detected. The scientific Advisory board for the civil protection services met on the 27th of December to go over the situation near Fagradalsfjall. GPS instruments and satellite interferograms show that the magmatic intrusion is limited /about-imo/news/update-on-the-eruption-in-geldingadalir/

• 37. Factsheet_Bardarbunga_20141208

  continues until the subsidence of the Bardarbunga caldera stops. The eruption can still go on for many months.  The volcanic fissure may lengthen southwards under Dyngjujokull, resulting in a jokulhlaup and an ash-producing eruption. It is also possible that eruptive fissures could develop in another location under the glacier. If such an eruption would be prolonged it could eventually produce /media/jar/Factsheet_Bardarbunga_20141208.pdf

• 38. Factsheet_Bardarbunga_20141210

  scenarios are considered most likely:  The eruption in Holuhraun continues until the subsidence of the Bardarbunga caldera stops. The eruption can still go on for many months.  The volcanic fissure may lengthen southwards under Dyngjujokull, resulting in a jokulhlaup and an ash- producing eruption. It is also possible that eruptive fissures could develop in another location under the glacier /media/jar/Factsheet_Bardarbunga_20141210.pdf

• 39. Factsheet_Bardarbunga_20141212

  scenarios are considered most likely:  The eruption in Holuhraun continues until the subsidence of the Bardarbunga caldera stops. The eruption can still go on for many months.  The volcanic fissure may lengthen southwards under Dyngjujokull, resulting in a jokulhlaup and an ash- producing eruption. It is also possible that eruptive fissures could develop in another location under the glacier /media/jar/Factsheet_Bardarbunga_20141212.pdf

• 40. Factsheet_Bardarbunga_20141216

  of the Bardarbunga caldera stops. The eruption can still go on for many months.  The volcanic fissure may lengthen southwards under Dyngjujokull, resulting in a jokulhlaup and an ash- producing eruption. It is also possible that eruptive fissures could develop in another location under the glacier. If such an eruption would be prolonged it could eventually produce a lava flow.  Volcanic eruption /media/jar/Factsheet_Bardarbunga_20141216.pdf