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  • 31. BITN_windrose_2005-2014

    15 22 32 21 3 12 3 8 4 6 6 2 1 10 5 20 29 27 24 38 37 16 52 Wind rose BITN August 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 observations: 836 Calm: 7.9% Variable winds: 8.1% Average wind speed for wind direction Wind direction /media/vedur/BITN_windrose_2005-2014.pdf
  • 32. AnneFleig_May2010_CES

    (all) common atmospheric situations over a region. CES conference, Oslo, Norway, 31 May - 2 June 2010 Advantages • simple, • consider the whole region, • strongly correlated with several, local meteorological variables, • if based on air pressure data only: - better represented in climate models than precipitation. Anne K. Fleig et al. “Regional hydrological droughts and weather types /media/ces/AnneFleig_May2010_CES.pdf
  • 33. The weather in Iceland 2014

    prec.days >=1.0 mm Reykjavík 963.1 121 112 37.6 223 160 Stafholtsey 829.4 97 28.0 182 144 Bláfeldur 1460.7 97 32.0 272 195 Stykkishólmur 678.8 96 87 20.0 218 136 Litla-Ávík 835.0 96 34.1 267 164 Bergstaðir 458.2 98 22.6 177 92 Sauðanesviti 1017.5 115 28.2 239 158 Akureyri 743.7 152 133 23.0 225 133 Grímsstaðir 514.8 /about-imo/news/nr/3082
  • 34. ved-eng-2014

    24-hr mm prec.days >=1.0 mm Reykjavík 963.1 121 112 37.6 223 160 Stafholtsey 829.4 97 28.0 182 144 Bláfeldur 1460.7 97 32.0 272 195 Stykkishólmur 678.8 96 87 20.0 218 136 Litla-Ávík 835.0 96 34.1 267 164 Bergstaðir 458.2 98 22.6 177 92 Sauðanesviti 1017.5 115 28.2 239 158 Akureyri 743.7 152 133 23.0 225 133 Grímsstaðir 514.8 146 128 22.5 228 133 Miðfjarðarnes 765.0 120 36.4 233 /media/vedurstofan/utgafa/skylduskil/ved-eng-2014.pdf
  • 35. 2011_005

    in Appendix III. 4.2 Preferred layout of the network The Iceland CGPS network has been installed mostly through research grants of different projects with various collaborators. As a result the network coverage is uneven around the country. Areas outside of the active plate boundary have hardly any GPS stations and the network coverage is lacking for large part of the plate boundary, many /media/vedurstofan/utgafa/skyrslur/2011/2011_005.pdf
  • 36. Bárðarbunga 2014 - November events

    water Large quantities of gases are emitted to the atmosphere associated with the Holuhraun eruption. Among the gases are SO2 that can convert to sulfuric acid causing acid rain. Since 19th September 2014, rainwater samples have been collected and analysed at weekly bases at 18 locations across all the country. The sampling and analysis have been carried out by Veðurstofan and Háskóli Íslands /earthquakes-and-volcanism/articles/nr/3023
  • 37. Bardarbunga-2014_November-events

    all below M1.0. A slight increase of seismicity in the dyke during the first hours after M>5 earthquakes at the caldera rim has also been observed in several previous cases since the onset of the activity. No obvious changes in the volcanic activity at the eruption site in Holuhraun, based on camera observation. 22 November 2014 12:00 - from geoscientist on duty Seismic activity around /media/jar/Bardarbunga-2014_November-events.pdf
  • 38. Bárðarbunga 2014 - November events

    water Large quantities of gases are emitted to the atmosphere associated with the Holuhraun eruption. Among the gases are SO2 that can convert to sulfuric acid causing acid rain. Since 19th September 2014, rainwater samples have been collected and analysed at weekly bases at 18 locations across all the country. The sampling and analysis have been carried out by Veðurstofan and Háskóli Íslands /earthquakes-and-volcanism/articles/nr/3023/
  • 39. The weather in Iceland in 2022

    was particularly cold; the temperature was 5 °C below average in both places. It hasn't been this cold in Reykjavík in December for over 100 year. Precipitation The year 2022 was unusually wet in Reykjavík. It was relatively wet in the capital in the beginning of the year, with March exceptionally wet. It was the wettest March on record, with total precipitation almost triple the average precipitation /about-imo/news/the-weather-in-iceland-in-2022
  • 40. Bárðarbunga 2014 - October events

    The lowest layers had a cloud ceiling of 2000 feet, the second layer between 6000-9000 and a third layer at flight level around 19000 feet. The clouds slowly dissipated to the south. The flight was directed to the northeast from Reykjavik airport, north towards Hofsjokull and Askja. A large circle was then flown around the Bárðarbunga caldera and Holuhraun. In the later part of the flight the area /earthquakes-and-volcanism/articles/nr/3011

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