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  • 31. 2010_012rs

  • 32. QA on the eruption in Eyjafjallajökull 2010

    amount of ice is melted and, accordingly, little danger of large jökulhlaups. The floods are monitored by online gauges in several rivers around the volcanoes Katla and Eyjafjallajökull. Large or damaging jökulhlaups are not expected in connection to this event unless changes occur in the eruption pattern. How is the eruption monitored? The Icelandic Meteorological Office monitors earth /earthquakes-and-volcanism/articles/nr/1880
  • 33. VI_2020_008

  • 34. Isskyrsla_20100407

    °37.30' W025°43.12' 64. N66°37.07' W025°42.88' 65. N66°35.83' W025°39.58' 66. N66°35.98' W025°38.09' 67. N66°36.72' W025°37.63' 68. N66°36.12' W025°30.75' 69. N66°40.29' W025°23.43' 70. N66°41.64' W025°22.00' 71. N66°42.18' W025°18.30' 72. N66°41.81' W025°14.49' 73. N66°43.06' W025°13.71' 74. N66°43.73' W025°15.62' 75. N66°44.26' W025°18.19' 76. N66°46.05' W025°17.16' 77. N66°45.77' W025°10.95' 78 /media/hafis/skyrslur_lhg/Isskyrsla_20100407.pdf
  • 35. Traffc-maintenance_expenditures

    602 1985 69 162 268 854 21 519 287 550 - 8 390 17 755 26 574 8 767 - - - 708 572 1 444 484 1984 63 220 239 096 17 569 274 379 - 6 561 17 510 21 630 7 314 - - - 646 775 1 373 444 1983 58 155 225 692 22 930 273 852 - 7 658 15 811 17 982 7 433 - - - 629 513 1 410 203 1982 52 712 189 383 15 822 262 412 - 8 974 15 974 17 509 10 038 - - - 572 824 1 385 993 1981 48 251 172 997 14 874 234 817 - 6 526 20 /media/loftslag/Traffc-maintenance_expenditures.pdf
  • 36. BIKF_windrose_2005-2014

    observations: 13639 Calm: 1.9% Variable winds: 0.22% Average wind speed for wind direction Wind direction (°) Wind speed (knots ) 0 5 10 15 20 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 25 3 43 7 55 9 69 3 58 3 49 1 74 0 82 8 70 5 47 8 44 2 40 7 41 1 52 4 51 1 41 7 38 2 36 7 32 1 29 7 29 3 29 9 37 0 39 9 44 1 35 8 32 3 21 3 /media/vedur/BIKF_windrose_2005-2014.pdf
  • 37. VI_2022_006_extreme

    77 91 109 Hraunaveita 132 116 136 159 117 140 169 Kvíslaveita 48 42 49 58 42 51 61 Sultartangi 66 57 68 80 58 69 84 Þingvallavatn 96 84 99 117 85 102 123 Þórisvatn 47 41 49 57 42 50 60 Tungnaá 76 67 79 92 67 80 98 Ufsarlón 104 92 108 126 93 112 134 36 Figure 19 – 1M5 maps for catchment Hálslón based on the ICRA dataset without projection (top left), with RCP 2.6 and 10th percentile /media/vedurstofan-utgafa-2022/VI_2022_006_extreme.pdf
  • 38. Hydropower - Glacier, Snow and Ice

    of Storbreen, Norway. Journal of Glaciology, 54 (185), 245-258. (Available online at IGS: http://www.igsoc.org/journal/54/185/j07j058.pdf.). Crochet, P. (2007). A study of regional precipitation trends in Iceland using a high quality gauge network and ERA-40. J. Climate, 20(18), 4659-4677, doi: 10.1175/JCLI4255.1. Crochet P., Jóhannesson T., Jónsson T., Sigurðsson O., Björnsson H., Pálsson F. & Barstad I /ces/publications/nr/1940
  • 39. PhD_course-Programme_26Aug2011-final

    of a large-scale agricultural catchment. WATER RESOURCES RESEARCH, VOL. 45, W00A15, doi:10.1029/2007WR006760 Kok K, Veldkamp TA (2011) Scale and governance: conceptual considerations and practical implications. Guest editorial special feature Scale and Governance. Ecology and Society 16(2): 23. [online] URL: http://www.ecologyandsociety.org/vol16/iss2/art23/ Kok K, van Vliet M, Bärlund I /media/vedurstofan/PhD_course-Programme_26Aug2011-final.pdf
  • 40. ces-oslo2010_proceedings

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