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• 41. 2010_012rs

  Gudmundsson, Icelandic Met Office Hjörleifur Sveinbjörnsson, Icelandic Met Office Sigþrúdur Ármannsdóttir, Icelandic Met Office Bergþóra Thorbjarnardóttir, Icelandic Met Office Steinunn S. Jakobsdóttir, Icelandic Met Office 4 5 Contents 1. Development and implementation of near-real time automatic fault mapping in SW-Iceland /media/vedurstofan/utgafa/skyrslur/2010/2010_012rs.pdf

• 42. A strong earthquake

  A strong earthquake 29.5.2008 Today, Thursday 29 May 2008 at 15:45, an earthquake of the size 6.1 on the Richter scale occurred in Southwest Iceland. It was found in Reykjavík and elsewhere. Its origin was near mountain Ingólfsfjall, 5 km northwest /about-imo/news/nr/1305

• 43. The crater at Grímsvötn

  GMT explosive activity increased again and the plume rose to about 7.5 km height. The increased activity was observed for about 20 minutes, then the activity dropped down at 21:15 GMT and increased again at 21:45 GMT. This pulsating activity is also clearly seen on tremor plots (click to enlarge) from near seismic stations, i.e. at Grímsfjall, located 5 km east of the eruption site /about-imo/news/nr/2188

• 44. The crater at Grímsvötn

  stations, i.e. at Grímsfjall, located 5 km east of the eruption site, and at Skrokkalda located 50 west of the eruption. Water is clearly seen in the fissure (photo below). The eruptive activity is now concentrated at two small vents surrounded by a thin circle of tephra. The eruption plume drifted slowly southwards but ash fell down from the plume into a brownish layer of ash which spread out over /about-imo/news/nr/2188/

• 45. norsem_palli

  Oblique spreading leads to extensive volcanism and large earthquakes, a combination that is otherwise uncommon in Iceland. The fissure swarms of individual volcanic systems contain normal faults and fissures, with a NE-trend, also quite oblique to the plate boundary. The fissure swarms fade out towards the NE and SW as they extend into the plates on either side. Overprinting this pattern /media/norsem/norsem_palli.pdf

• 46. The ice cap Snæfellsjökull is thinning rapidly

  in recent years according to people living in the neighbourhood of the glacier and travellers in the area, which is among the most popular tourists' destinations in Iceland. By comparing airborne lidar measurements of the glacier surface, that were carried out in September 2008, with a digital terrain model by the mapping company Loftmyndir ehf from 1999, the average lowering of the ice surface /weather/articles/nr/1618

• 47. The ice cap Snæfellsjökull is thinning rapidly

  in recent years according to people living in the neighbourhood of the glacier and travellers in the area, which is among the most popular tourists' destinations in Iceland. By comparing airborne lidar measurements of the glacier surface, that were carried out in September 2008, with a digital terrain model by the mapping company Loftmyndir ehf from 1999, the average lowering of the ice surface /weather/articles/nr/1618/

• 48. Kok_2-scenarios-lecture-2

  ) Establish scenario team and scenario panel (2) Team proposes goals and outline (3) Panel drafts narrative storylines (6) Panel revises storylines (5) Modelling groups quantify scenarios (4) Team quantifies driving forces (8) General review of scenarios (9) Team & Panel make final revision of scenarios (10) Publication and distribution (7) Repeat step 4-6 Story-And-Simulation approach /media/loftslag/Kok_2-scenarios-lecture-2.pdf

• 49. norsem_slunga

  stiff machines) but also brittle stable slip. Cook studied the slip behaviour at different pressures and temperatures. He found that at shallow depths one expect in general brittle and stable slip (not unstable slip, earthquakes). This prevailed for the top 5 km of granitic crust. Between 5 and 20 km depth one got brittle unstable slip and when temperature and depth increased one got eventually /media/norsem/norsem_slunga.pdf

• 50. NONAM_1st_workshop_summary_v3

  of adaptive management (as synthesized in the ‘double loop model’) – see figure 2. The first session started with an introduction to the sector / case considered, followed by a brief general discussion on the outlined features of the sector. The rest of that session was used to deliberate on questions 1 to 4. In the second break-out session the rest of the questions 5 to 7 were addressed. The third /media/vedurstofan/NONAM_1st_workshop_summary_v3.pdf