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Results:

• 41. VI_2019_009

  26 36 40 41 46 50 51 52 53 54 58 60 61 62 63 64 65 68 70 71 72 73 74 80 81 83 84 85 86 87 92 Present weather (Manual) Present weather ( Automatic ) Number of records a71 a71 a71 250 500 750 250 500 750 Number of records Figure 15. Automatic station as a function of manual station. a71 a71a71a71a71a71 a71a71 a71a71a71 a71a71 a71 a71 a71a71 a71 a71 a71 a71 a71 a71 a71 a71 a71 a71 a71 a71 a71a71a71 /media/vedurstofan-utgafa-2019/VI_2019_009.pdf

• 42. VI_2015_006

  August 2012 at 12 UTC (local time). Top panel: large- scale analysis based on ERA-Interim reanalysis data, with mean sea level air pressure (black contours), temperature at 850 hPa (dashed red contours), and 6-hourly accumu- lated precipitation (coloured contours). Bottom panel: manned and automated surface observations over Iceland. 11 3 September 2012 Weather conditions on that day were determined /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_006.pdf

• 43. 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

• 44. Moellenkampetal_etal-2010

  Acteurs et Usages (UMR G-EAU), Cemagref, 4University of Architecture, Civil Engineering and Geodesy, 5Hornsby Shire Council, 6Lisode, 7UN-Water Decade Programme on Capacity Development (UNW-DPC), United Nations University, 8School of Natural and Rural Systems Management, University of Queensland, 9College of Asia and the Pacific, The Australian National University, 10Marine and Atmospheric Research /media/loftslag/Moellenkampetal_etal-2010.pdf

• 45. vhmkerfi_mars_2012

  W W W W W W W D DD DD DD CB CA CB CA CA CB CB CB CA CA CB CA CA CA CBCB CB CA CB CB CB CBCBCB CB CB CA CA CACA CA CA CACACB CA CA CA CA CB CA CA CA CA CA CB CA CA CA CACA CA CB CA CA CA CA CA CA CB CA CA CA CBCA CA CACA CA CA CA CA CA CA CA CB CA CA CA CBCB CB C CA CA CB CB CA CA CB CA CB CA CA CB CA CA CA CACA CA CB B CA CA CA CA CA CB CA CA CA CA CB CA CA CAC CACB CA CBCB CB CB CB CACA CBCA C B /media/vatnafar/maelar/vhmkerfi_mars_2012.pdf

• 46. IMO_AnnualReport2014

  used to produce probabilistic hazard maps for SO2 concentration at ground. The maps have been produced using a wind statistics based on 10 years. The final prod- ucts have been adopted by the Civil Protection for the definition of the restricted area around the eruption site. Baldur Bergsson, Árni Snorrason and Amy Donovan measuring gas at Holuhraun. Photo: Hermann Arngrímsson. Bárðarbunga /media/vedurstofan/utgafa/skyrslur/2015/IMO_AnnualReport2014.pdf

• 47. 2013_001_Nawri_et_al

  and a pressure of 1013.25 hPa. In the case of Iceland, the climate deviates significantly from these standard atmospheric conditions. Additionally, terrain elevation varies considerably across the island. Therefore, seasonal and annual differences in air density from the standard value, as well as spatial variability, need to be taken into account. Approximate air density can be calculated by assuming /media/vedurstofan/utgafa/skyrslur/2013/2013_001_Nawri_et_al.pdf

• 48. Kok_et_al._TFSC_published_2011

  ]. There is ample experience with backcasting, and consequently much has been said about the underlying principles (e.g. [20]), the methodological 838 K. Kok et al. / Technological Forecasting & Social Change 78 (2011) 835–851 Author's personal copy framework (e.g. [8,30–32]), and practical applications (e.g. [33–35]). Also the combination between backcasting and other types of scenarios has been /media/loftslag/Kok_et_al._TFSC_published_2011.pdf

• 49. VI_2020_004

  vedur@vedur.is Veðurstofa Íslands Bústaðavegur 7–9 108 Reykjavík Sara Barsotti, Veðurstofa Íslands Sigrún Karlsdóttir, Veðursstofa Íslands Anna María Ágústsdóttir, Landgræðslan Björn Oddsson, Almannavarnadeild Ríkislögreglustjóra Íris Marelsdóttir, Embætti landlæknis Þorvaldur Þórðarson, Jarðvísindastofnun H áskólans Þórólfur Guðnason, Embætti landlæknis Bogi B. Björnsson, Veðurstofa Íslands /media/vedurstofan-utgafa-2020/VI_2020_004.pdf

• 50. Observations - Ingólfsfjall

  Observations - Ingólfsfjall | Observations | Icelandic Meteorological office Observations - Ingólfsfjall Mon 1.05 14 GMT 5.6° E 3 Max wind : 5 / 7 13 GMT 5.4° ENE 5 Max wind : 7 / 9 12 GMT 4.3° ENE 8 Max wind : 9 / 13 11 GMT 3.5° ENE 9 Max wind : 10 / 13 10 GMT 2.2° ENE 10 Max wind : 11 /m/observations/areas