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Results:

• 61. Hare-2011-ParticipatoryModelling

  are labelled according to the geographical area of application. Examples such as Zürich and Hase II have already been reviewed and categorized in Hare et al. (2003) and Bots and van Daalen (2008), respectively. The entire Iskar process, of which Iskar (Phase I) is a part, has been categorized by Barreteau et al. (2010). All are included in this review to provide alternative analytical perspectives /media/loftslag/Hare-2011-ParticipatoryModelling.pdf

• 62. VI_2015_006

  m 2 or less, compared with losses of 80 W m 2 or more over neigh- bouring cloud-free regions. The conditions around midnight, off the southeast coast on 27 July, and along the north coast on 3 September, clearly show the limited ability (in the model) of even a complete high-level cloud cover to affect the longwave radiation balance at the surface. Mid- level clouds are usually simulated together /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_006.pdf

• 63. The eruption continues with little changes

  well away from the eruption now; all access is restricted. The weather forecast is as follows: Increasing northeast wind and intermittent snow and blowing snow, 18 to 23 m/s by afternoon. Rather slighter northwest wind tomorrow and snow showers. Air temperatures -1°C down to -6°C. Calmer weather is expected on Wednesday. On April 4th, lava flowing to the west encountered some patches of glacial ice /about-imo/news/nr/1860

• 64. 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/

• 65. The eruption continues with little changes

  At around 7 pm on March 31st, magma started degassing from the lava field, northeast of the main crater. Lava fountains have since then been active both there and in the old crater. This change was not accompanied by any detectable seismic activity, neither tremor nor micro earthquakes. Most of the lava seems to accumulate near the vents, but there are intermittent flows into the gullies of Hruná /about-imo/news/nr/1860/

• 66. Poster presentations

  on Intraplate Seismicity in Central Fennoscandia Annakaisa Korja, Uski, M., Lund, B., Grigull, S., Nironen, M., E., Högdahl, K. Relative earthquake location in Southern Iceland Bergþóra S. Þorbjarnardóttir and Ingi Þ. Bjarnason This year's update on the Burträsk fault seismicity Darina Buhcheva and Björn LundThe SIL-system from an operational standpointJón Söring Communication between /norsem/norsem2016/program/poster

• 67. 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 '/

• 68. 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 '/

• 69. 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 '/

• 70. 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 '/' link '/