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Results:

• 21. 2010_016

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

• 22. 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

• 23. 2010_017

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

• 24. NONAM_1st_workshop_summary_v3

  ........................................................................................................................... 3  Summary ............................................................................................................................... 4  Summary of the break-out sessions on road infrastructure ................................................... 6  Summary of the break-out sessions on Horsens case /media/vedurstofan/NONAM_1st_workshop_summary_v3.pdf

• 25. 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

• 26. VI_2020_005

  /media/vedurstofan-utgafa-2020/VI_2020_005.pdf

• 27. Bárðarbunga 2014 - August events

  automatically detected from midnight until now are 400. 27 August 2014 20:50 - info from a surveillance flight Scientists from IES and IMO on a flight to Vatnajökull tonight discovered a row of 10-15 m deep cauldrons south of the Bárðarbunga caldera. They form a 6-4 km long line. The cauldrons have been formed as a result of melting, possibly a sub-glacial eruption, uncertain when. Heightened /earthquakes-and-volcanism/articles/nr/3000

• 28. Bardarbunga-2014_August-events

  of 10-15 m deep cauldrons south of the Bárðarbunga caldera. They form a 6-4 km long line. The cauldrons have been formed as a result of melting, possibly a sub-glacial eruption, uncertain when. Heightened tremor level/volcanic tremor has not been observed on IMO's seismometers at the moment. The new data is being examined. A field trip earlier today A new GPS station being mounted near /media/jar/Bardarbunga-2014_August-events.pdf

• 29. Bárðarbunga 2014 - August events

  automatically detected from midnight until now are 400. 27 August 2014 20:50 - info from a surveillance flight Scientists from IES and IMO on a flight to Vatnajökull tonight discovered a row of 10-15 m deep cauldrons south of the Bárðarbunga caldera. They form a 6-4 km long line. The cauldrons have been formed as a result of melting, possibly a sub-glacial eruption, uncertain when. Heightened /earthquakes-and-volcanism/articles/nr/3000/

• 30. VI_2022_006_extreme

  for the hydropower catchments ............................................ 36 6 CONCLUSIONS .................................................................................................................. 41 BIBLIOGRAPHY ...................................................................................................................... 42 APPENDIX I. MELT SEASON ANALYSIS /media/vedurstofan-utgafa-2022/VI_2022_006_extreme.pdf