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  • 51. Twenty years of multinational earthquake prediction research in Iceland, and the future

    for an alert system. The alert system has been in operation for almost two decades and is in further development. The SIL system also provides a basis for all the later prediction research projects. The PRENLAB and PRENLAB-2 projects of several European countries, 1996-2000 (EC supported projects) were a direct continuation of the SIL project, but with a more multidisciplinary approach. PRENLAB /earthquakes-and-volcanism/conferences/jsr-2009/earthquake-prediction/
  • 52. Earthquakes

    most active volcanoes. Earthquake activity in the vicinity of Hekla is usually quite low, but seems to increase abruptly before an eruption. Before the eruption in Hekla in 2000, increased earthquake activity was measured in the area and a seismic swarm occurred just about an hour before the eruption. In addition to the earthquake activity, there were some significant changes in nearby strain /volcanoes/volcanic-hazards/earthquakes/
  • 53. Dyrrdal_Anita_CES_2010

    • Analyse future snow scenarios Introduction Data & Methods Results 0 50 100 150 200 250 300 350 400 450 0-100 100- 200 200- 300 300- 400 400- 500 500- 600 600- 700 700- 800 800- 900 900- 1000 1000- 1100 1100- 1200 1200- 1300 1300- 1400 1400- 1500 1500- 1600 1600- 1700 1700- 1800 1800- 1900 1900- 2000 2000- 2100 2100- 2200 Høyde (m o.h.) A n t a l l v æ r s t a s j o n e r Elevation of met.no /media/ces/Dyrrdal_Anita_CES_2010.pdf
  • 54. Linnet_Ulfar_CES_2010

    °C/100y 1975-2000 • 2.35 °C/100y 2000- •Change in precipitation • Average increase 4.8% / 100 y • Range 3.3 – 7.2 % •Glaciers • Results from CES • 25% decrease in volume from 2000 to 2050 Temperature transformation Com parison of series 10000 12000 14000 16000 18000 20000 22000 1 9 5 0 1 9 5 2 1 9 5 4 1 9 5 6 1 9 5 8 1 9 6 0 1 9 6 2 1 9 6 4 1 9 6 6 1 9 6 8 1 9 7 0 1 9 7 2 1 9 7 4 1 9 7 6 1 9 7 8 1 /media/ces/Linnet_Ulfar_CES_2010.pdf
  • 55. Savolainen_Ilkka_CES_2010

    ) and other gases A wide spectrum of measures needed in order to reach deep enough emission reductions 503/02/2010 Global greenhouse gas emissions by sectors in 2005 The emissions sum up to approximately 46,000 MtCO2eq. Data source: CAIT, cait.wri.org. *) The estimated effect of land use change & forestry, 8,000 MtCO2, is for the year 2000. 603/02/2010 Raupach et al 2007; Le Quere et al. 2009 /media/ces/Savolainen_Ilkka_CES_2010.pdf
  • 56. 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
  • 57. Final Conference of the SVALI project

    News The western cauldron in Vatnajökull, Iceland, on 19 August 2000, view towards southeast /about-imo/news/nr/3142
  • 58. Increased seismic activity between Krýsuvík and Ölfus

    News Earthquakes over 1 in size at the Reykjanes peninsula, from Jan 2000 to June 2015 /about-imo/news/nr/3150
  • 59. 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/
  • 60. Hekla

    on the Eastern Volcanic zone and consists of a central volcano rising to 1490 m.a.s.l. and is about 60 km long fissure swarm. The volcano has been highly active during Holocene and has erupted 23 times in historical time, with its last eruption occurring in 2000. It is considered the third most active volcano in Iceland. About 100 eruptions are known from the system in the past 9000 years, both effusive /volcanoes/about-volcanoes/hekla/

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