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• 61. GA_2009_91A_4_Andreassen

  to highly negative summer balances, but also lower bw than the average for 1949–2006. Calculated change in specific mass balance for a ±1°C change in air tem- perature was ±0.55 m w.e., whereas a ±10 % in- crease in precipitation represented a change of ± 0.20 m w.e. Model results further indicated that for a 2°C warming, the ablation season will be extend- ed by c. 30 days and that the period /media/ces/GA_2009_91A_4_Andreassen.pdf

• 62. VI_Arsskyrsla_2018_vef

  ÁRSSKÝRSL A 2018 2 Á R S S K Ý R S L A 2 0 1 8 3 Frá forstjóra 4 Veðurstofan 2009–2019 12 Náttúrufar 18 Rannsóknir 20 Fjármál og rekstur 22 Ritaskrá starfsmanna ?Veðurstofa Íslands 2019 Bústaðavegi 7–9, 108 Reykjavík ISSN 2251-5607 Efni ársskýrslunnar var unnið af starfsmönnum Veðurstofu Íslands Ritstjórn: Sigurlaug Gunnlaugsdóttir Hönnun og umbrot: Hvíta húsið Prentun: Prentmet /media/vedurstofan/utgafa/arsskyrslur/VI_Arsskyrsla_2018_vef.pdf

• 63. BIEG_windrose_2005-2014

  33 7 22 5 26 5 31 4 28 3 30 1 16 8 3 9 3 3 6 3 2 6 3 4 4 3 2 6 6 3 8 9 8 0 8 0 29 0 Wind rose BIEG June 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 12 14 16 Frequency of wind direction (%) Aerodrome Total observations: 7053 Calm: 11% Variable winds: 2.4% Average /media/vedur/BIEG_windrose_2005-2014.pdf

• 64. Jökulhlaup from Grímsvötn subsides

  their measurements are shown in Figure 2. Figure 2. Discharge (m³/s) measurements at Gígjukvísl bridge: From the curve the total amount of floodwater is estimated 0.45 km³. The discharge curve is typical for jökulhlaups from Grímsvötn that do not result from volcanic activity: Over the course of several days, the amount of water flowing through an ice tunnel at the glacier bed steadily increases. Loss /about-imo/news/2010/nr/2042

• 65. Jökulhlaup from Grímsvötn subsides

  their measurements are shown in Figure 2. Figure 2. Discharge (m³/s) measurements at Gígjukvísl bridge: From the curve the total amount of floodwater is estimated 0.45 km³. The discharge curve is typical for jökulhlaups from Grímsvötn that do not result from volcanic activity: Over the course of several days, the amount of water flowing through an ice tunnel at the glacier bed steadily increases. Loss /about-imo/news/nr/2042

• 66. Bad weather is expected

  23.2.2017 The Icelandic Meteorological Office wants to emphasize the extremely bad weather that is expected tomorrow Friday 24th of February. Windspeed is expected to be 20 - 28 m/s (45 - 62 miles/hour) in the south and west part after noon, tomorrow with strong gusts up to 40 m/s /about-imo/news/bad-weather-is-expected-1

• 67. Consultation meeting

  Consultation meeting Nordic Meteorological Institutes 3.9.2013 The Director General of the Icelandic Meteorological Office invited his colleagues of the other Nordic Meteorological Institutes to the northern town of Ísafjörður 26 – 28 August /about-imo/news/nr/2736

• 68. The eruption has come to an end

  The eruption has come to an end The volcanic eruption in Holuhraun lasted six months 15.3.2015 The volcanic eruption in Holuhraun has come to an END, see a declaration from the Scientific Advisory Board, 28 February 2015. For the first time in six months /about-imo/news/nr/3097

• 69. Warning - strong or severe gale

  - strong or severe gale Forecast for Tuesday 10 March 9.3.2015 Icelandic Meteorological Office wishes to emphasize the following weather forecast: Warning A strong gale or severe gale warning (average wind velocity 20 to 28 m/s) is in effect for all parts /about-imo/news/nr/3104

• 70. Weather warning - violent storm

  Weather warning - violent storm 4.12.2015 A strong gale warning (average windspeed above 20 m/s) is in effect in Iceland this afternoon and for most of tomorrow. A violent storm (average wind speed, above 28 m/s) is expected /about-imo/news/nr/3245