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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. 100 days of gas release at Holuhraun

  rich but not as Laki in the 18th century Sara Barsotti 11.12.2014 The ongoing eruption at Holuhraun, which began in at the end of August 2014, is very rich in gas. We have to go 150 years back to find an event (Trölladyngja) that had a comparable impact on Iceland and its /pollution-and-radiation/volcanic-gas/measurements/

• 4. 100 days of gas release at Holuhraun

  rich but not as Laki in the 18th century Sara Barsotti 11.12.2014 The ongoing eruption at Holuhraun, which began in at the end of August 2014, is very rich in gas. We have to go 150 years back to find an event (Trölladyngja) that had a comparable impact on Iceland and its /pollution-and-radiation/volcanic-gas/measurements

• 5. 100 days of gas release at Holuhraun

  rich but not as Laki in the 18th century Sara Barsotti 11.12.2014 The ongoing eruption at Holuhraun, which began in at the end of August 2014, is very rich in gas. We have to go 150 years back to find an event (Trölladyngja) that had a comparable impact on Iceland and its /pollution-and-radiation/volcanic-gas/measurements/nr/3036

• 6. Hazard zoning

  takes place on two vents along the fissure, the northernmost part of the rampart and from the central part of the rampart. These two sources merge into one plume. Downwind, dense volcanic gases separate and descend. Further downwind a second plume, rich in water vapour, reaches higher elevation than the first plume /pollution-and-radiation/volcanic-gas/hazard-zoning/bigimg/3042

• 7. VONA message

  with fountains reaching 100-150 m above the ground. These pulses are very apparent in the seismic tremor from stations in a wide area around the eruption site. Cloud height:The base of the volcanic cloud is discernible from the webcameras and it is assessed to be between 800-900 m asl. Other cloud information:The plume is gas rich and minor ash is observed. Remarks:Some gas /earthquakes-and-volcanism/volcanoes/vona-notifications/

• 8. VONA message

  with fountains reaching 100-150 m above the ground. These pulses are very apparent in the seismic tremor from stations in a wide area around the eruption site. Cloud height:The base of the volcanic cloud is discernible from the webcameras and it is assessed to be between 800-900 m asl. Other cloud information:The plume is gas rich and minor ash is observed. Remarks:Some gas /earthquakes-and-volcanism/volcanoes/vona-notifications/' link '/

• 9. VONA message

  with fountains reaching 100-150 m above the ground. These pulses are very apparent in the seismic tremor from stations in a wide area around the eruption site. Cloud height:The base of the volcanic cloud is discernible from the webcameras and it is assessed to be between 800-900 m asl. Other cloud information:The plume is gas rich and minor ash is observed. Remarks:Some gas /earthquakes-and-volcanism/volcanoes/vona-notifications/' link '/' link '/

• 10. VONA message

  with fountains reaching 100-150 m above the ground. These pulses are very apparent in the seismic tremor from stations in a wide area around the eruption site. Cloud height:The base of the volcanic cloud is discernible from the webcameras and it is assessed to be between 800-900 m asl. Other cloud information:The plume is gas rich and minor ash is observed. Remarks:Some gas /earthquakes-and-volcanism/volcanoes/vona-notifications/' link '/' link '/' link '/