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  • 21. BIKF_windrose_2005-2014

    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: 14605 Calm: 1.4% Variable winds: 0.38% 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 46 6 76 6 /media/vedur/BIKF_windrose_2005-2014.pdf
  • 22. VI_arsskyrsla2020

  • 23. ces-oslo2010_proceedings

    ...................................................................................................................................................................... 74 Nawri, N. and Björnsson, H. Surface Air Temperature and Total Precipitation Trends for Iceland in the 21st Century ..................................... 76 Räisänen, J. Probabilistic projections of temperature and precipitation change for the period 2021-2050 ............................... 78 HYDROLOGICAL PROJECTIONS, RUNOFF Beldring, S /media/ces/ces-oslo2010_proceedings.pdf
  • 24. GA_2009_91A_4_Andreassen

    net balances are wellcorrelated and (obviously) best modelled as the sum of bw measured and bs modelled (bs-m2). Thebest obtained correlations of modelled bw (0.86), bs(0.87) and bn (0.94) for 1949–2006, show that themodel could explain 73, 76 and 88% of the variance over this period.From each year we also extracted the day with maximum bw (bwd) and minimum bs (bsd, mini-mum values as bs is negative /media/ces/GA_2009_91A_4_Andreassen.pdf
  • 25. Lorenzoni_Pidgeon_2006

    felt it was a “fairly good thing” or a “very good thing”). Two UK surveys undertaken in 2004 indi- cated that although most people have heard of global warming, and rate it as the most important environmental issue for the world today, they see terrorism and domestic issues as having a higher priority (Norton and Leaman, 2004; Kirby, 76 I. LORENZONI AND N. F. PIDGEON 2004). These findings contrast /media/loftslag/Lorenzoni_Pidgeon_2006.pdf
  • 26. VI_2020_004

    ................................................................................................................ 72 5.4.1 Input parameters and synthetic scenario .......................................................... 72 5.4.2 Validating model results with real deposit map ............................................... 73 5.4.3 Probabilistic hazard maps ................................................................................ 76 5.4.4 Towards Impact /media/vedurstofan-utgafa-2020/VI_2020_004.pdf
  • 27. VI_2009_013

    stress and the spectra of seismic shear waves from earthquakes. J. Geophys. Res., 75, no 26, 4997–5009. Brune, J. N. (1971). Correction. J. of Geophys. Res., 76, No. 20, 5002. Dahm, Thorsten, B. Brandsdóttir (1997). Moment tensors of microearthquakes from the Eyjafjallajökull volcano in South Iceland. Geophys. J. Int, 130, 183–192. Einarsson, P., S. Björnsson, G. Foulger, R. Stefánsson and Th /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_013.pdf
  • 28. 2010_012rs

    teleseismic event; a total of 76 estimates of τmax. Of these 19 events, four local events on Reykjanes peninsula (yellow stars in Figure 1), in the magnitude range 3.3–4.2 have provided reliable estimates of dominant period, consistent between stations and events (see Figure 2). The estimates from a M5.4 event at 15º distance in Svalbard are contaminated by S-waves, because the driver did /media/vedurstofan/utgafa/skyrslur/2010/2010_012rs.pdf
  • 29. 2010_003rs

  • 30. VI_2017_009

    % Kirkjubæjarklaustur 45% 5% - Reykjavík 29% 1% - Selfoss 43% 3% - 2081-2100 RCP8.5 Akureyri 32% 10% 1% Egilsstaðir 48% 15% 2.5% Kirkjubæjarklaustur 73% 12% 0.5% Reykjavík 44% 3% - Selfoss 76% 10% - To determine the frequency of cold days the three cases mentioned above are considered, namely days with frost at some point, days with frost all day, and days with extreme frost. To look /media/vedurstofan-utgafa-2017/VI_2017_009.pdf

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