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  • 21. VI_2009_006_tt

    lake in a volcanic caldera in the interior of the Vatnajökull ice cap (Björns- son, 1988). Jökulhlaups from Grímsvötn have been known since at least the fourteenth century (Þórarinsson, 1939, 1974). In the beginning of the twentieth century there were about ten years between outbursts but the floods diminished with time and became more frequent. After a catastrophic, rapidly rising flood caused /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_006_tt.pdf
  • 22. vanRoosmalen_etal-2009-WRR_2007WR006760

    and Irrigationa Scenario Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec Current 101 85 59 13 6 4 1 6 39 79 84 97 A2 145 132 73 10 10 7 6 8 4 75 92 123 B2 137 119 75 16 6 6 6 5 21 74 110 141 aValues are in millimeters. 10 of 18 W00A15 VAN ROOSMALEN ET AL.: CLIMATE AND LAND USE CHANGE W00A15 time and larger area where groundwater levels rise above the drain levels. Table 6 shows the mean discharges /media/loftslag/vanRoosmalen_etal-2009-WRR_2007WR006760.pdf
  • 23. ces-oslo2010_proceedings

    change over the North Atlantic and in some simulations also for Iceland. In all areas, including the North Atlantic and Iceland, a clear climate change signal compared to the spread between the simulations is seen. The standard deviation calculated from 17 of the simulations are less than 1°C in all areas apart from Iceland where it reaches between 1 and 2°C and in parts of the Barents Sea where /media/ces/ces-oslo2010_proceedings.pdf
  • 24. Windspeed

    Extreme wind, dangerous Top of page Comparison with Beaufort-values Windforce* Average windspeed** Median of average windspeed Beaufort Name m/s km/h knots m/s km/h knots 0 Calm 0-0,2 < 1 < 1 0,0 0,0 0,0 1 Light air 0.3-1.5 1-5 1-3 0.8 3.0 1.6 2 Light breeze 1.6-3.3 6-11 4-6 2.4 8.5 4.6 3 /weather/articles/nr/1283
  • 25. Windspeed

    Extreme wind, dangerous Top of page Comparison with Beaufort-values Windforce* Average windspeed** Median of average windspeed Beaufort Name m/s km/h knots m/s km/h knots 0 Calm 0-0,2 < 1 < 1 0,0 0,0 0,0 1 Light air 0.3-1.5 1-5 1-3 0.8 3.0 1.6 2 Light breeze 1.6-3.3 6-11 4-6 2.4 8.5 4.6 3 /weather/articles/nr/1283/
  • 26. VI_2020_011_en

    particles formed as the magmatic gases age (most notably, SO4 aerosol is formed from SO2 gas), and from tephra particles (the finest ash can be breathed in, and the acidic coatings on tephra particles can acidify and pollute fresh water). One person died due to CO2 accumulation in a basement during the 1973 Eldfell eruption. During the eruption, rescue 22 workers needed to be aware of escape /media/vedurstofan-utgafa-2020/VI_2020_011_en.pdf
  • 27. 2010_012rs

    ) closest stations, respectively. The 40 highest correlating events are then inverted for the best location. For comparison the manual locations, obtained by an analyst are shown in yellow. The final locations of the events are all within an approximately 1 km2 area, even though their original, automatic locations are up to 5 km away. They are also within a few hundred meters from the manual /media/vedurstofan/utgafa/skyrslur/2010/2010_012rs.pdf
  • 28. BIAR_windrose_2005-2014

    1 8 1 7 1 9 4 1 7 5 21 5 27 2 32 5 48 9 68 4 82 1 Wind rose BIAR September 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 Frequency of wind direction (%) Aerodrome Total observations: 7233 Calm: 3.5% Variable winds: 8.7% Average wind speed for wind direction Wind direction (°) Wind /media/vedur/BIAR_windrose_2005-2014.pdf
  • 29. Past temperature conditions in Iceland

    cold period lasting to 1920. The overall warming trend is about 0.7°C per century. A short spell of cold springs also occured around 1950. The ice years (1965 to 1971) were also bad and a few very cold springs occurred around 1980, 1979 being the worst. The spring in 1812 and 1859 are the worst of the 19th century. Back to top Autumn temperature in Stykkishólmur Figure /climatology/articles/nr/1213
  • 30. Past temperature conditions in Iceland

    cold period lasting to 1920. The overall warming trend is about 0.7°C per century. A short spell of cold springs also occured around 1950. The ice years (1965 to 1971) were also bad and a few very cold springs occurred around 1980, 1979 being the worst. The spring in 1812 and 1859 are the worst of the 19th century. Back to top Autumn temperature in Stykkishólmur Figure /climatology/articles/nr/1213/

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