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• 21. VI_2016_006_rs

  of 100–140 m a.s.l. Several debris flows are recorded in Búðará since the beginning of the 20th century. It is not clear whether the upper or lower area is the main source for these debris flows. The return time for sizeable debris flows in Búðará is around 20 years. It appears that the land- slide activity has been more frequent in the last 30 years than earlier in the 20th century. 4.5 Areas 7 /media/vedurstofan-utgafa-2016/VI_2016_006_rs.pdf

• 22. Moellenkampetal_etal-2010

  Acteurs et Usages (UMR G-EAU), Cemagref, 4University of Architecture, Civil Engineering and Geodesy, 5Hornsby Shire Council, 6Lisode, 7UN-Water Decade Programme on Capacity Development (UNW-DPC), United Nations University, 8School of Natural and Rural Systems Management, University of Queensland, 9College of Asia and the Pacific, The Australian National University, 10Marine and Atmospheric Research /media/loftslag/Moellenkampetal_etal-2010.pdf

• 23. Refsgaard_etal-2007-Uncertainty-EMS

  The advantage of Monte Carlo analysis is its general appli- cability and that it does not impose many assumptions on prob- ability distributions and correlations and that it can be linked to any model code. The key limitation is the large run times for computationally intensive models and the huge amount of outputs that are not always straightforward to analyse. 4.8. Multiple model simulation Multiple model /media/loftslag/Refsgaard_etal-2007-Uncertainty-EMS.pdf

• 24. VI_2020_005

  and CNES, n.d.; National Center for Atmospheric Research Staff, 2016; Quante and Colijn, 2016). Now, additional altimeters at different orbits perform slightly less accurate measurements up to 82 N and S (Rhein et al., 2013). These records are used to estimate sea surface changes and calculate global mean sea level, a temporal average sea level averaged over the oceans (Church, Clark, et al., 2013 /media/vedurstofan-utgafa-2020/VI_2020_005.pdf

• 25. 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/

• 26. 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 '/

• 27. 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 '/

• 28. 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 '/

• 29. 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 '/

• 30. 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 '/' link '/