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Results:

• 41. Bárðarbunga 2014 - August events

  likely produce a flood in Jökulsá á Fjöllum and perhaps explosive, ash-producing activity. At 10:00 UTC, IMO changed the Aviation Colour Code for Bárðarbunga to ‘orange', signifying that significant emission of ash into the atmosphere is unlikely. The aviation colour-code for the Askja volcano remains at ‘yellow'. Other scenarios cannot be excluded. For example, an eruption inside the Bárdarbunga /earthquakes-and-volcanism/articles/nr/3000

• 42. Bárðarbunga 2014 - August events

  likely produce a flood in Jökulsá á Fjöllum and perhaps explosive, ash-producing activity. At 10:00 UTC, IMO changed the Aviation Colour Code for Bárðarbunga to ‘orange', signifying that significant emission of ash into the atmosphere is unlikely. The aviation colour-code for the Askja volcano remains at ‘yellow'. Other scenarios cannot be excluded. For example, an eruption inside the Bárdarbunga /earthquakes-and-volcanism/articles/nr/3000/

• 43. 2010_017

  .................................................................................................................. 10 Figure 4. Elevation distribution for Sandá í Þistilfirði (vhm 26, blue curve) and Austari- Jökulsá (vhm 144, red broken curve). .................................................................................... 16 Figure 5. Comparison of mean yearly temperature 1961–2005 for Sandá í Þistilfirði (vhm 26); an interpolation /media/ces/2010_017.pdf

• 44. Observations - Þverfjall II

  Observations - Þverfjall II | Observations | Icelandic Meteorological office Observations - Þverfjall II Mon 1.05 14 GMT E 10 Max wind : 10 / 12 13 GMT E 9 Max wind : 10 / 11 12 GMT E 9 Max wind : 9 / 10 11 GMT E 8 Max wind : 10 / 12 10 GMT ENE 9 Max wind : 10 / 12 09 GMT ENE 8 Max wind /m/observations/areas

• 45. Daniell_etal-2010

  in the Dhuenn process for various reasons. While the Wupperverband aimed at initiating a participatory process in order to step into an emerging field of power (participatory water management on the way towards WFD implementation) [1; 10; 4; 6], it lacked procedural knowledge on how to design and conduct a participatory process, as well as financial and human resources in this field [1; 5]. The researchers /media/loftslag/Daniell_etal-2010.pdf

• 46. VI_2020_005

  (Quante and Colijn, 2016). Work on risk analysis and adaptation is in different stages in the countries of the world. Coastal floods have caused problems in Iceland in the past (Jóhannsdóttir, 2017) and are likely to do so in the future as well. Large coastal floods can be expected in Iceland every 10 - 20 years and the probability of such events can rise with climate change (Almannavarnir, 2011 /media/vedurstofan-utgafa-2020/VI_2020_005.pdf

• 47. NONAM_1st_workshop_summary_v3

  List of participants ............................................................................................... 28  NONAM Workshop Reykjavik 26 & 27 August 2010 – Summary 3 Introduction NONAM stands for NOrdic Network on Adaptive Management in relation to climate change. The NONAM network is one of the 10 networks funded by the Nordic Council of Ministers as part of the Top /media/vedurstofan/NONAM_1st_workshop_summary_v3.pdf

• 48. Henriksen_Barlebo-2008-AWM_BBN-Journ_Env_Management

  networks for t i Christiansen Barlebo r Voldgade 10, DK-1350 Copenhagen K, Denmark form 3 May 2007; accepted 11 May 2007 29 June 2007 www.elsevier.com/locate/jenvman  Mak manage ARTICLE IN PRESS brought together to find a solution that is adequate from multiple perspectives. This, not only requires coping with various sources and types of uncertainty, but also with the ambiguity produced /media/loftslag/Henriksen_Barlebo-2008-AWM_BBN-Journ_Env_Management.pdf

• 49. VI_2009_006_tt

  236 1992 09 167 124 167 98 1995 07 1994 1759 599 368 1995 10 96 62 73 37 1997 07 921 728 330 184 2000 08 1240 1083 365 221 2002 09 689 582 267 160 2003 11 241 207 139 98 2006 04 1370 1340 300 270 2008 10 1350 1290 300 265 The origin of the 1957, 1960, 1964 and 1966 jökulhlaups is not certain but is most likely the eastern cauldron. The discharge and volume for the 1995 jökulhlaup are a sum from /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_006_tt.pdf

• 50. Session program Thursday 13. October

  08:30 – 10:10 Oral session - Chair: Martin Hensch 08:30 – 08:50 Ambient noise tomography of Eyjafjallajökull Ásdís Benediktsdóttir, Ólafur Guðmundsson, Bryndís Brandsdóttir 08:50 – 09:10 Long-period earthquakes recorded on a dense seismic array during the 2014 Bárðarbunga rifting event Bryndís /norsem/norsem2016/program/thursday