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  • 1. programme2---PhD-Workshop-preceding-Adaptation-Research-Conference

    During the conference all of you are requested to act as rapporteur in two or three sessions. A preliminary allocation of rapporteur sessions has been made (see below), while accounting for your expertise in certain areas. Participants can suggest changes in the rapporteur session allocation, on the condition a convincing argumentation is provided as well as a confirmed alternative rapporteur /media/loftslag/programme2---PhD-Workshop-preceding-Adaptation-Research-Conference.pdf
  • 2. Refsgaard_1-Welcome

    – Print yourselves • Case descriptions and tasks/questions • Lecturers’ presentations – Handouts during the week – Pdfs will be uploaded at website afterwards Practicalities • PC login – Internet access • Printing • Lunch • Coffee – tea • Posters Monday afternoon + refreshments • Dinner Tuesday at 19:00 Students • Brief presentation round – now • 2-minutes presentation of research topics /media/loftslag/Refsgaard_1-Welcome.pdf
  • 3. Bárðarbunga earthquakes - interactive model

    (central mouse scroll), pan (right click), turn over (left click) choose speed 1x, 2x, 10x (available in some browsers (e.g. Chrome but not Firefox) coloured patches on/off (ring icon) choose landscape map (mountain icon) or satellite image (bell icon) for the surface Tryggvi Hjörvar, specialist at the Icelandic Met Office, created this model. An easier presentation - demo In a video /earthquakes-and-volcanism/articles/nr/2971
  • 4. Bárðarbunga earthquakes - interactive model

    (central mouse scroll), pan (right click), turn over (left click) choose speed 1x, 2x, 10x (available in some browsers (e.g. Chrome but not Firefox) coloured patches on/off (ring icon) choose landscape map (mountain icon) or satellite image (bell icon) for the surface Tryggvi Hjörvar, specialist at the Icelandic Met Office, created this model. An easier presentation - demo In a video /earthquakes-and-volcanism/articles/nr/2971/
  • 5. norsem_begga

    shock mag. ~3.0 and aftershocks). The DD relocation gives tighter clustering of earthquakes in all three areas, and the strike of a fault segment, unclear in the catalog data, becomes clearly visible after relocation. Relocation shifts the centroids of the clusters by ~300 m from catalog locations, but relative distances between clusters do not change significantly. Our next step is to extend /media/norsem/norsem_begga.pdf
  • 6. Bárðarbunga 2014 - December events

    (pdf 0.4 Mb). The Scientific Advisory Board of the Icelandic Civil Protection has held 80 meetings since the seismic activity started on the 16th of August. The Scientific Advisory Boards wishes all its' dedicated readers a Merry Christmas. 22 December 2014 10:00 - from geoscientist on duty Bárðarbunga: The largest earthquake measured the last 24 hours was M4.5 and occurred at 16:12 yesterday /earthquakes-and-volcanism/articles/nr/3055
  • 7. Bárðarbunga 2014 - December events

    (pdf 0.4 Mb). The Scientific Advisory Board of the Icelandic Civil Protection has held 80 meetings since the seismic activity started on the 16th of August. The Scientific Advisory Boards wishes all its' dedicated readers a Merry Christmas. 22 December 2014 10:00 - from geoscientist on duty Bárðarbunga: The largest earthquake measured the last 24 hours was M4.5 and occurred at 16:12 yesterday /earthquakes-and-volcanism/articles/nr/3055/
  • 8. Bardarbunga-2014_December-events

    the crater. Lava is also running to the north. Notes from the meeting of the Scientific Advisory Board (pdf 0.4 Mb). The Scientific Advisory Board of the Icelandic Civil Protection has held 80 meetings since the seismic activity started on the 16th of August. The Scientific Advisory Boards wishes all its' dedicated readers a Merry Christmas. 22 December 2014 10:00 - from geoscientist /media/jar/Bardarbunga-2014_December-events.pdf
  • 9. Bárðarbunga 2014 - October events

    The lowest layers had a cloud ceiling of 2000 feet, the second layer between 6000-9000 and a third layer at flight level around 19000 feet. The clouds slowly dissipated to the south. The flight was directed to the northeast from Reykjavik airport, north towards Hofsjokull and Askja. A large circle was then flown around the Bárðarbunga caldera and Holuhraun. In the later part of the flight the area /earthquakes-and-volcanism/articles/nr/3011
  • 10. Bardarbunga-2014_October-events

    previously been observed for several M>5 events and can not be interpreted as a decrease of the overall activity. The subsidence rate of the caldera had shortly increased around one hour after the M5.3 and is now again back to normal rates, see graph, which also is a frequent observation associated with M>5 earthquakes in Bárðarbunga. Around 20 events have been detected in the northern part /media/jar/Bardarbunga-2014_October-events.pdf

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