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Results:

• 11. BIKF_windrose_2005-2014

  68 8 62 2 41 8 52 9 54 4 56 8 45 5 50 3 46 5 46 3 56 7 61 0 57 4 52 8 43 6 45 4 45 0 38 8 37 5 41 5 45 4 43 3 35 7 39 8 36 4 29 2 17 4 12 3 8 9 9 5 8 4 9 4 18 7 Wind rose BIKF February 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 Frequency of wind direction (%) Aerodrome Total /media/vedur/BIKF_windrose_2005-2014.pdf

• 12. Karlsdottir-Risk_analysis_IMO_SK

  Earth quakes Volcanic eruptions ash cloud detection – threat to aviation ash dispersion – threat to live stock and human health. Meteorological monitoring and forecast IMO monitors and issues forecast for land and sea large airspace IMO is a State Volcano Observatory Pre - eruption activity Eruption monitoring Airborne volcanic ash 62 seismic stations ~70 GPS stations ~25 ISGPS ~45 other /media/loftslag/Karlsdottir-Risk_analysis_IMO_SK.pdf

• 13. VI_2022_006_extreme

  -year return period, based on the complete ICRA dataset. Timeseries were extracted using the average value of all the grid-points within the catchment. 1M5 value is shown in red. Hálslón 2 years 5 years 10 years 25 years 50 years 100 years 3 hours 8 11 13 15 18 20 6 hours 18 23 27 31 36 39 12 hours 35 43 49 54 62 67 24 hours 60 70 78 85 94 101 48 hours 91 105 115 125 137 147 /media/vedurstofan-utgafa-2022/VI_2022_006_extreme.pdf

• 14. Isskyrsla_20100407

  W025°52.01' 49. N66°26.74' W025°51.74' 50. N66°27.25' W025°54.19' 51. N66°29.92' W025°55.49' 52. N66°30.60' W025°57.10' 53. N66°34.18' W025°54.30' 54. N66°36.46' W025°49.24' 55. N66°35.91' W025°45.72' 56. N66°37.65' W025°49.39' 57. N66°37.94' W025°53.33' 58. N66°40.72' W025°53.00' 59. N66°43.26' W025°48.84' 60. N66°43.01' W025°43.68' 61. N66°39.79' W025°42.75' 62. N66°38.95' W025°41.76' 63. N66 /media/hafis/skyrslur_lhg/Isskyrsla_20100407.pdf

• 15. Bárðarbunga 2015 - March, April, May

  obtained are: The depth of the caldera subsidence is the same as obtained with the BARC GPS station until contact was lost in March, the maximum being 62 m. The volume of the subsidence bowl is now 1.9 km³. This is an increase of about 0.1 km³ since 3rd February. It is likely that most of this volume increase occurred in Febuary. Geothermal activity: Ice cauldrons at the SE rim /earthquakes-and-volcanism/articles/nr/3122

• 16. Bárðarbunga 2015 - March, April, May

  obtained are: The depth of the caldera subsidence is the same as obtained with the BARC GPS station until contact was lost in March, the maximum being 62 m. The volume of the subsidence bowl is now 1.9 km³. This is an increase of about 0.1 km³ since 3rd February. It is likely that most of this volume increase occurred in Febuary. Geothermal activity: Ice cauldrons at the SE rim /earthquakes-and-volcanism/articles/nr/3122/

• 17. Bardarbunga-2015_MarchAprMay-events

  surveys were conducted from TF-FMS over Bárðarbunga, after six weeks of waiting for the right weather. The results obtained are:  The depth of the caldera subsidence is the same as obtained with the BARC GPS station until contact was lost in March, the maximum being 62 m.  The volume of the subsidence bowl is now 1.9 km³. This is an increase of about 0.1 km³ since 3rd February. It is likely /media/jar/Bardarbunga-2015_MarchAprMay-events.pdf

• 18. BIGJ_windrose_2005-2014

  W N (Number of observations for wind direction) Icelandic Met Office 02. júl. 2015 35 62 48 77 8 4 83 63 64 22 19 14 7 4 11 11 14 41 1 5 24 25 18 45 64 41 3 2 93 35 11 17 7 11 47 16 24 67 36 Wind rose BIGJ January 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 Frequency of wind /media/vedur/BIGJ_windrose_2005-2014.pdf

• 19. VI_2020_008

  /media/vedurstofan-utgafa-2020/VI_2020_008.pdf

• 20. Climatic-Change-2012---Personality-type-differences-between-Ph.D.-climate-experts-and-general-public---implications-for-communication

  geoscientists, microbiologists, plant scientists and statisticians (Schaubhut and Thompson 2008). Symposia participants exhibited a strong preference (82%) for taking in information through Intuition (Fig. 1). Overall, 62% of the college or university faculty in Schaubhut and Thompson (2008) indicated a preference for Intuition, as did the majority of biochemists, biologists, chemists, economists /media/loftslag/Climatic-Change-2012---Personality-type-differences-between-Ph.D.-climate-experts-and-general-public---implications-for-communication.pdf