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Results:

• 21. NONAM_1st_workshop_summary_v3

  NONAM Nordic Network on Adaptive Management in relation to climate change Risk Assessment and Stakeholder Involvement Multidisciplinary Workshop in Reykjavík 26 - 27 August 2010 Final report NONAM Workshop Reykjavik 26 & 27 August 2010 – Summary 2 Contents Introduction /media/vedurstofan/NONAM_1st_workshop_summary_v3.pdf

• 22. 2010_017

  ............................................................................................................................... 5 TABLES ................................................................................................................................. 6 1 ABSTRACT ..................................................................................................................... 7 2 INTRODUCTION /media/ces/2010_017.pdf

• 23. VI_2014_005

  Evaluation of HARMONIE reanalyses of surface air temperature and wind speed over Iceland Nikolai Nawri VÍ 2014-005 Skýrsla 2 Evaluation of HARMONIE reanalyses of surface air temperature and wind speed over Iceland VÍ 2014- 005 ISSN 1670- 8261 Skýrsla +354 522 60 00 vedur @vedur . is Veður st of a Íslands Búst aðaveg ur 7 – 9 108 Reyk j avík Nik olai Nawr i /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_005.pdf

• 24. 2010_016

  .................................................................................................................... 7 2 INTRODUCTION ........................................................................................................... 8 3 METHODS .................................................................................................................... 10 4 DATA /media/ces/2010_016.pdf

• 25. Henriksen_Barlebo-2008-AWM_BBN-Journ_Env_Management

  ) Use this model to identify policies that are likely to succeed or that probe key uncertainties; (2) being to (1) Work with stakeholders to develop a shared under- standing of the system to be managed and the desirable outcomes, by developing a system model that can be used for policy screening; Wal as a d e social and political values in water resource ment. ters and Holling (1990) describe /media/loftslag/Henriksen_Barlebo-2008-AWM_BBN-Journ_Env_Management.pdf

• 26. VI_2020_005

  . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 9 2 Background . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 11 2.1 Factors affecting sea level . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 12 2.1.1 Main factors affecting sea level in Scandinavia, the UK and Iceland . . . . 13 2.2 Sea level data /media/vedurstofan-utgafa-2020/VI_2020_005.pdf

• 27. Bárðarbunga 2014 - August events

  at around midday. From the Icelandic Met Office: The Aviation Colour Code remains at the ‘orange' level for Bárðarbunga. 27 August 2014 06:30 - from geoscientist on duty The night started with a 5.3 event in Bardarbunga at 00:16 hours. Around half an hour later activity around the tip of the dyke started increasing and reached some kind of "high" around 2 o'clock and has continued at that level /earthquakes-and-volcanism/articles/nr/3000

• 28. Bardarbunga-2014_August-events

  The night started with a 5.3 event in Bardarbunga at 00:16 hours. Around half an hour later activity around the tip of the dyke started increasing and reached some kind of "high" around 2 o'clock and has continued at that level since with many events of magnitude 2-3. Just before 2 o'clock there was a magnitude 4.5 event just east of the Askja caldera. Few microearthquakes have been measured /media/jar/Bardarbunga-2014_August-events.pdf

• 29. Bárðarbunga 2014 - August events

  at around midday. From the Icelandic Met Office: The Aviation Colour Code remains at the ‘orange' level for Bárðarbunga. 27 August 2014 06:30 - from geoscientist on duty The night started with a 5.3 event in Bardarbunga at 00:16 hours. Around half an hour later activity around the tip of the dyke started increasing and reached some kind of "high" around 2 o'clock and has continued at that level /earthquakes-and-volcanism/articles/nr/3000/

• 30. VI_2022_006_extreme

  J. Roberts Tinna Þórarinsdóttir VÍ 2022-006 Skýrsla +3 5 4 522 6000 vedur@ve d u r.i s Veðursto f a Ísland s B ú sta ð a rve g u r 7–9 108 Reyk j a vík Contents 1 INTRODUCTION .................................................................................................................. 4 2 STUDY AREA /media/vedurstofan-utgafa-2022/VI_2022_006_extreme.pdf