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Results:

• 31. Daniell_etal-2010

  artificial and determined by reservoir management. According to its recent assessment pursuant to Art. 5 WFD, the Dhuenn basin does not attain the good status required by the WFD (MUNLV 2005). Downstream of the dam, the ecomorphological quality of the river is mediocre compared to the upper part of the basin (MUNLV 2005). Shortcomings are linked mainly to the ecological status, especially /media/loftslag/Daniell_etal-2010.pdf

• 32. Observations - Húsafell

  Observations - Húsafell | Observations | Icelandic Meteorological office Observations - Húsafell Mon 1.05 14 GMT 7.9° NE 5 Max wind : 5 / 8 13 GMT 6.0° NNE 4 Max wind : 6 / 9 12 GMT 4.2° NNE 5 Max wind : 6 / 10 11 GMT 3.2° NNE 5 Max wind : 6 / 11 10 GMT 2.5° NNE 5 Max wind : 6 / 10 /m/observations/areas

• 33. 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

• 34. 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

• 35. 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

• 36. VI_2014_006

  ................................................................................. 47 5 Summary .................................................................................................... 54 6 Acknowledgements....................................................................................... 55 7 References /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_006.pdf

• 37. 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

• 38. Forecasts - Seltjarnarnes - Suðurnes

  Forecasts - Seltjarnarnes - Suðurnes | Station forecasts | Icelandic Meteorological office Forecasts - Seltjarnarnes - Suðurnes Mon 1.05 14 GMT 6° NE 2 Cloud cover: 100% 15 GMT 6° ENE 6 Cloud cover: 100% 16 GMT 7° E 4 Cloud cover: 100% 17 GMT 7° SE 6 Cloud cover: 100% 18 GMT 6° SE 5 /m/forecasts/areas

• 39. VI_2009_006_tt

  viii Contents Abstract ii Ágrip v Acknowledgements vii List of Figures xi List of Tables xiii 1 Introduction 1 2 Overview of jökulhlaups 3 2.1 Jökulhlaups from marginal lakes . . . . . . . . . . . . . . . . . . . . 3 2.2 Jökulhlaups due to volcanic eruptions . . . . . . . . . . . . . . . . . 4 2.3 Grímsvötn and the Skaftá cauldrons . . . . . . . . . . . . . . . . . . 5 2.4 Jökulhlaups in Iceland /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_006_tt.pdf

• 40. BIHN_windrose_2005-2014

  Wind rose BIHN 2005 − 2014 90 80 70 60 50 40 30 2010360350340 330 320 310 300 290 280 270 260 250 240 230 220 210 200 190 180 170 160 150 140 130 120 110 100 1 2 3 4 5 6 Frequency of wind direction (%) Aerodrome Total observations: 28301 Calm: 5.3% Variable winds: 1.6% Average wind speed for wind direction Wind direction (°) Wind speed (knots ) 0 2 4 6 8 10 0 45 90 135 180 225 270 315 360 N E S /media/vedur/BIHN_windrose_2005-2014.pdf