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Results:

• 11. Traffc-maintenance_expenditures

  010 35 826 31 995 14 697 - - 11 565 965 240 1 534 288 1989 99 043 344 975 25 658 417 254 - 6 616 27 444 37 107 11 469 - - - 969 568 1 626 822 1988 89 553 316 711 32 055 370 248 - 4 552 24 027 41 360 9 665 - - - 888 171 1 609 435 1987 95 558 294 548 31 938 366 374 - 7 647 22 013 38 900 11 006 - - - 867 984 1 656 504 1986 70 968 273 286 26 725 324 820 - 7 254 19 103 29 614 11 425 - - - 763 193 1 521 /media/loftslag/Traffc-maintenance_expenditures.pdf

• 12. BIIS_windrose_2005-2014

  (Number of observations for wind direction) Icelandic Met Office 02. júl. 2015 28 6 85 3 223 1 339 5 367 0 315 2 161 9 89 4 34 6 11 7 18 7 9 7 7 7 15 9 8 7 7 2 14 9 7 4 22 6 36 9 69 6 148 3 183 1 148 5 96 9 45 1 21 1 9 3 7 8 2 0 1 7 2 4 1 2 1 6 7 3 11 6 Wind rose BIIS January 2005−2014 90 80 70 60 50 40 30 2010360350340 330 320 310 300 290 280 270 260 /media/vedur/BIIS_windrose_2005-2014.pdf

• 13. VI_2022_006_extreme

  /media/vedurstofan-utgafa-2022/VI_2022_006_extreme.pdf

• 14. VI_2020_008

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

• 15. VI_2009_013

  T., and T. C. Wallace, 1995. Modern Global Seismology, Academic Press. McNutt, S. R. (2005). Volcanic Seismology. Annu. Rev. Earth Planet. Sci., 32, 15.1– 15.31. doi: 10.1146/annurev.earth.33.092203.122459. Meissner, R. and J. Strehlau (1982). Limits of stresses in continental crusts and their relation to the depth-frequency distribution of shallow earthquakes, Tectonics, 1, 73– 89. Pedersen /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_013.pdf

• 16. BIKF_windrose_2005-2014

  89 7 72 0 47 7 29 7 32 3 43 8 40 2 40 2 40 5 44 3 52 3 79 1 67 4 51 3 43 9 34 6 31 1 28 3 29 9 40 5 45 3 45 8 39 1 25 2 29 0 20 1 18 0 19 6 22 4 19 2 19 6 21 8 17 3 29 4 Wind rose BIKF May 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 Frequency of wind direction (%) Aerodrome Total /media/vedur/BIKF_windrose_2005-2014.pdf

• 17. 2010_012rs

  and dips 89°. The strike deviates only 4° from the strike defined by the relocated aftershock distribution on the Ingólfsfjall fault, which shows an 11 km long and an 8 km deep fault, striking N181°E and dipping 89°. The mechanism of the earthquake on the Ingólfsfjall fault could therefore have been immediately inferred. However, there were only three foreshocks 25 on the (second) Kross fault /media/vedurstofan/utgafa/skyrslur/2010/2010_012rs.pdf

• 18. VI_2017_009

  - Interim (which gives 3% cover in February). Reject: Variables which show a significant difference between models and on which bases a certain GCM is rejected. The time period is 1981-2000. GCM Tavg (°C) Ptot (mm/yr) SI (%) Febr. Reject CNRM-CM5 -3.1 -419 +17 SI, Tavg, Ptot IHCEC-EC-Earth -3.2 +89 +19 SI, Tavg HadGEM2 -1.1 +107 +8 - MPI-ESM-LR +0.5 +11 0 - 3.4 Quality control: RCMs /media/vedurstofan-utgafa-2017/VI_2017_009.pdf

• 19. 2010_005_

  /media/ces/2010_005_.pdf

• 20. Lorenzoni_Pidgeon_2006

  very/somewhat worried about the greenhouse effect (of these, 43% were very worried); in 19924 the percentage had increased to 89% (of these, 62% were very worried) (INRA (Europe), 1992). In 19955 public concern was similar: 84% declared to be very/quite worried about climate change as a global environmental threat (INRA (Europe)-ECO, 1995). By 2002 another survey (EORG, 2002) suggested /media/loftslag/Lorenzoni_Pidgeon_2006.pdf