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• 21. 2010_017

  Iceland VÍ 2010-017 ISSN 1670-8261 Report +354 522 60 00 +354 522 60 06 vedur@vedur.is Veðurstofa Íslands Bústaðavegur 9 150 Reykjavík Bergur Einarsson, Icelandic Meteorological Office Sveinbjörn Jónsson, Icelandic Meteorological Office   5 Contents FIGURES /media/ces/2010_017.pdf

• 22. 2010_016

  Sveinbjörn Jónsson, Icelandic Meteorological Office 4 5 Contents FIGURES .............................................................................................................................. 5 TABLES ................................................................................................................................ 6 1 ABSTRACT /media/ces/2010_016.pdf

• 23. Bardarbunga-2014_August-events

  Office, Institute of Earth Sciences and Cambridge University confirmed the location of the eruption.  The eruption occurred on an old volcanic fissure on the Holuhraun lava field, about 5 km north of the Dyngjujökull ice margin. The active fissure was about 600 m in length.  A small amount of lava drained from the fissure and by around 04:00 UTC, lava flow is thought to have stopped /media/jar/Bardarbunga-2014_August-events.pdf

• 24. Bárðarbunga 2014 - August events

  field, about 5 km north of the Dyngjujökull ice margin. The active fissure was about 600 m in length. A small amount of lava drained from the fissure and by around 04:00 UTC, lava flow is thought to have stopped. According to seismic data and web-camera imagery, the eruption peaked between 00:40 and 01:00 UTC. At the beginning of the eruption, seismic activity decreased, although seismicity has /earthquakes-and-volcanism/articles/nr/3000

• 25. Bárðarbunga 2014 - August events

  field, about 5 km north of the Dyngjujökull ice margin. The active fissure was about 600 m in length. A small amount of lava drained from the fissure and by around 04:00 UTC, lava flow is thought to have stopped. According to seismic data and web-camera imagery, the eruption peaked between 00:40 and 01:00 UTC. At the beginning of the eruption, seismic activity decreased, although seismicity has /earthquakes-and-volcanism/articles/nr/3000/

• 26. NONAM_1st_workshop_summary_v3

  NONAM Workshop Reykjavik 26 & 27 August 2010 – Summary 5 • Conflict resolution mechanisms. The water sector is characterised by many strong stakeholders, who have to compromise to allow a water management solution to be achieved, and often the stakeholders are directly involved in negotiating the management solutions. The national road sector decisions are more often made at the central /media/vedurstofan/NONAM_1st_workshop_summary_v3.pdf

• 27. VI_2014_005

  mode ................................................... 14 5 Errors associated with SURFEX .................................................................... 15 6 Statistical correction of model results .............................................................. 19 7 Original and corrected 2-m air temperature .................................................... 22 8 Original and corrected 10-m /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_005.pdf

• 28. Henriksen_Barlebo-2008-AWM_BBN-Journ_Env_Management

  in the data used in making the decision and the factors are interlinked, all of which makes the problem highly complex. The part of the net defined by variables and links is relatively easily communicated to stakeholders (Henriksen et al., 2007b). However the tal Management 88 (2008) 1025–1036 quantitative part, with the conditional probability tables (CPTs), the numbers, is the step where /media/loftslag/Henriksen_Barlebo-2008-AWM_BBN-Journ_Env_Management.pdf

• 29. VI_2020_005

  5 Conclusion . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 60 References . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 61 Appendix: Description of the usage of the ACER method to find return periods and an adopted Hunter method to calculate allowances in Norway . . . . . . . . . . . . . . 73 1 Introduction The dynamic /media/vedurstofan-utgafa-2020/VI_2020_005.pdf

• 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