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Results:

• 61. GA_2009_91A_4_Andreassen

  and bs of 0.22–0.25 and0.24–0.28 m w.e. respectively in the period 1949–2006 are acceptable considering the uncertaintiesin both modelled and measured values. Althoughdiscrepancies occurred in some years, the mass bal- ance model was able to reproduce the main char-acteristics of annual and seasonal mass balance ofStorbreen. Close agreement between modelledmelt using a detailed energy balance model /media/ces/GA_2009_91A_4_Andreassen.pdf

• 62. Markarfljót outwash plain and Öræfajökull

  was funded mainly by the National Avalanche and Landslide Fund, with additional financial contributions from the Icelandic Road and Coastal Administration and the National Power Company. Published material Under the link below, each of the chapters can be downloaded or short summaries read. Pagneux, E., Gudmundsson, M. T., Karlsdóttir, S., & Roberts, M. J. (Eds.) (2015). Volcanogenic floods /hydrology/hazard-risk-assessments/glacial-outburst-floods/markarfljotsaurar-oraefajokull/

• 63. Journal_of_Hydrology_Veijalainen_etal

  A second, but usually smaller, increase in runoff oc- curs in the autumn. In northern Finland more than 95% of annual maximum floods are caused by spring snowmelt (cf. Fig. 7a). Also the small upstream lakes in the northern part of the lake area and the northernmost of the coastal rivers fall mainly into this cat- egory. In most coastal rivers the major floods can be caused by either snowmelt /media/ces/Journal_of_Hydrology_Veijalainen_etal.pdf

• 64. Avalanche danger scale

  was introduced late last winter (early 2012). It is important to understand that more avalanches are likely to have fallen without being reported; most notices come from regions where avalanche observers work. On the main page is a button (below left) for reporting avalanches. Another link invites comments on avalanches. Back /avalanches/articles/nr/2619

• 65. EUROVOLC – a networking project kick-off meeting

  established European volcanological supersites, FUTUREVOLC and MedSUV.Examples of networking activities in EUROVOLC include collaboration and networking between Volcano Observatories, Volcano Research Institutions and civil protection agencies, networking of atmospheric gas and aerosol observations as well as observations of subsurface processes, and initiation of access to multidisciplinary /about-imo/news/eurovolc-a-networking-project-kick-off-meeting

• 66. Focus of the Hydropower-Hydrology group of CES

  of climate change on the floods computed according to the national guidelines for design studies are analysed. Comparative studies of design floods in a changing climate with different national guidelines will also be carried out in border rivers between Norway and Finland and between Norway and Sweden. The rules for the regulation of lakes and rivers may become obsolete in a changing climate /ces/project/hydropower/

• 67. Factsheet_Bardarbunga_20140918

  University of Iceland along with representatives from the Icelandic Civil Protection, the Environmental Agency of Iceland and Directorate of Health. Main points  Volcanic eruption in Holuhraun  Air quality  Scenarios Notes  The volcanic eruption in Holuhraun continues with similar rate as yesterday.  The subsidence of the Bardarbunga caldera continues.  Seismic activity has /media/jar/Factsheet_Bardarbunga_20140918.pdf

• 68. Factsheet_Bardarbunga_20140919

  of the caldera. Such an eruption would melt large quantities of ice, leading to a major jokulhlaup, accompanied by ashfall. Other scenarios cannot be excluded. From the Icelandic Met Office: The Aviation Colour Code for Bardarbunga remains at ‘orange’. The National Commissioner of the Icelandic Police, Department of Civil Protection and Emergency Management www.almannavarnir.is /media/jar/Factsheet_Bardarbunga_20140919.pdf

• 69. Factsheet_Bardarbunga_20140920

  University of Iceland along with representatives from the Icelandic Civil Protection and the Environmental Agency of Iceland. Main points  Volcanic eruption in Holuhraun  Air quality  Scenarios Notes  The volcanic eruption in Holuhraun continues with similar rate as last few days.  The subsidence of the Bardarbunga caldera continues with same rate as before.  Big earthquakes /media/jar/Factsheet_Bardarbunga_20140920.pdf

• 70. Factsheet_Bardarbunga_20140921

  as before.  Big earthquakes are still detected in the Bardarbunga caldera. Since noon yesterday there have been 18 earthquakes bigger the M3,0. The biggest one was measured M5,0 at 17:11 yesterday afternoon. Smaller earthquakes were detected in north part of the dyke and around the eruption site.  No change was detected in water monitoring that cannot be explained with changing weather /media/jar/Factsheet_Bardarbunga_20140921.pdf