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  • 51. VI_2017_009

  • 52. BIHN_windrose_2005-2014

    ) Icelandic Met Office 02. júl. 2015 32 2 3 30 10 9 15 1 0 27 39 1 9 6 6 1 1 2 3 1 2 7 9 17 1 1 1 3 1 5 6 3 92 7 3 63 BIHN gusts exceeding 50 knots (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 2 4 6 8 10 Frequency of wind direction (%) Aerodrome Total observations: 135 Calm /media/vedur/BIHN_windrose_2005-2014.pdf
  • 53. BITN_windrose_2005-2014

    210 200 190 180 170 160 150 140 130 120 110 100 1 2 3 4 5 Frequency of wind direction (%) Aerodrome Total observations: 868 Calm: 5.2% Variable winds: 5.4% Average wind speed for wind direction Wind direction (°) Wind speed (knots ) 0 5 10 15 0 45 90 135 180 225 270 315 360 N E S W N (Number of observations for wind direction) Icelandic Met Office 02. júl. 2015 17 39 42 41 32 17 22 17 26 32 11 /media/vedur/BITN_windrose_2005-2014.pdf
  • 54. VanderKeur_etal-2008-Uncertainty_IWRM-WARM

  • 55. VI2010-006_web

    úrkoma á skömmum tíma skiptir oft meira máli varðandi hættu á ofanflóðum en meðaltal úrkomunnar yfir lengri tímabil. Tafla 3 sýnir niðurstöður greiningar á aftakaúrkomu yfir 1, 2, 3 12 Tafla 2. Meðaltöl ýmissa veðurþátta fyrir veðurstöðina á Akureyri (stöð nr. 422) fyrir tímabilið 1961–1990. Stærð jan feb mar apr maí jún júl ágú sep okt nóv des ár Úrkoma (mm) 55 42 43 29 19 28 33 34 39 58 54 53 /media/vedurstofan/utgafa/skyrslur/2010/VI2010-006_web.pdf
  • 56. GA_2009_91A_4_Andreassen

    : bs modelled using modelled bw (bw-m1) as snow depth, bs-m2: bs modelled using measured bw as snow depth, bn-m1: bn=bw-m1+bs- m2, bn-m2: bn=bw+bs-m2. Notes: n: number of years. Period n bw-m1 bw-m2 bs-m1 bs-m2 bn-m1 bn-m2 1949–2006 58 0.84 0.86 0.83 0.87 0.87 0.94 r 1949–1968 19 0.85 0.89 0.89 0.92 0.92 0.951968–2006 39 0.86 0.87 0.87 0.88 0.90 0.94 rmse 1949–2006 58 0.25 0.22 0.28 0.24 0.30 0.22 /media/ces/GA_2009_91A_4_Andreassen.pdf
  • 57. VI_2015_006

    ................................................................... 36 19 Differences in mean sea level air pressure.................................................... 38 20 Differences in the meridional wind component at 10 mAGL............................ 39 6 1 Introduction The goal of this study is to establish the sensitivity of the HARMONIE mesoscale weather prediction model to changes in snow and cloud cover /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_006.pdf
  • 58. BIRK_windrose_2005-2014

    41 8 20 4 10 5 6 4 8 0 10 9 31 2 48 4 52 7 39 0 29 2 30 5 22 6 24 7 18 1 17 6 20 0 18 0 19 5 22 7 21 9 19 2 16 4 15 0 13 5 13 4 9 9 8 5 11 9 12 6 7 9 14 3 14 2 15 4 20 1 Wind rose BIRK May 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 Frequency of wind direction (%) Aerodrome Total /media/vedur/BIRK_windrose_2005-2014.pdf
  • 59. BIVM_windrose_2005-2014

    Office 02. júl. 2015 8 3 9 8 3 9 1 8 1 3 3 7 2 6 7 7 19 3 39 9 27 1 15 3 12 1 7 8 10 0 7 1 6 8 7 9 4 6 6 3 5 1 7 2 9 3 7 2 8 3 7 7 6 3 8 3 7 3 6 1 4 6 2 1 3 3 4 6 10 5 Wind rose BIVM May 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 7 8 9 Frequency of wind /media/vedur/BIVM_windrose_2005-2014.pdf
  • 60. 2013_001_Nawri_et_al

    . . . . . . . . . . . . 65 36 Seasonal mean wind power density within the Skagi region . . . . . . . . . . . . . 66 37 Directional mean wind power density within the Snæfellsnes region . . . . . . . . 67 38 Seasonal mean wind power density within the Snæfellsnes region . . . . . . . . . . 68 39 Directional mean wind power density within the Þorlákshöfn region . . . . . . . . 69 40 Seasonal mean wind /media/vedurstofan/utgafa/skyrslur/2013/2013_001_Nawri_et_al.pdf

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