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Results:

• 1. 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

• 2. 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

• 3. FAQ

  in mind. There are many hollows where the gas can accumulate and be dangerous to people. Volcanic gasses might as well absorb any amount of O2. The Icelandic Meteorological Office publishes a forecast of the likelihood of gas pollution at ground level, while the Environment Agency of Iceland monitors air quality in inhabited areas. We also recommend looking at the information /volcanoes/fagradalsfjall-eruption/faq/

• 4. Traffc-maintenance_expenditures

  229 1 587 160 1970 18 591 42 413 2 166 86 101 - 892 5 131 2 310 201 - - - 157 805 1 652 904 1969 17 559 38 840 2 313 93 776 - 922 4 562 1 571 - - - - 159 543 1 832 354 1968 13 474 36 376 3 074 104 519 - 1 080 4 131 1 156 - - - - 163 811 1 964 368 1967 11 139 34 495 5 940 95 857 - 419 3 032 1 087 - - - - 151 968 1 936 249 1966 9 835 32 581 8 349 94 777 - 587 4 205 1 743 - - - - 152 077 2 032 936 /media/loftslag/Traffc-maintenance_expenditures.pdf

• 5. Bardarbunga_kafli20140825

  have not been located it is not clear whether eruptions on the central part of the system belong to a central volcano or the ice covered fissure swarm. Both cases will generate jökulhlaups from rapidly melting ice. All explosive eruptions originating below ice are therefore described together. 4 4.1 Bárðarbunga central volcano and adjacent ice covered fissure swarm 1. Phreatomagmatic /media/jar/Bardarbunga_kafli20140825.pdf

• 6. IPPC-2007-ar4_syr

  Approximate CO2-eq concentrations corresponding to the computed radiative forcing due to anthropogenic GHGs and aerosols in 2100 (see p. 823 of the WGI TAR) for the SRES B1, AIT, B2, A1B, A2 and A1FI illustrative marker scenarios are about 600, 700, 800, 850, 1250 and 1550ppm, respectively. d) Temperature changes are expressed as the difference from the period 1980-1999. To express the change relative /media/loftslag/IPPC-2007-ar4_syr.pdf

• 7. News

  Search Search string Contact IMO © Veðurstofa Íslands | Bústaðavegi 7- 9 | 105 Reykjavík | Phone 522 6000 | Fax: 522 6001 Recording 902 0600 | SSN 630908-0350 Contact us | Employees | Terms and conditions | Sitemap /about-imo/news/bigimg/3727

• 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/

• 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 '/

• 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 '/