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  • 21. Paper-Olafur-Rognvaldsson_92

    a systematic com- parison of results to observed precipitation has been carried out. Un- dercatchment of solid precipitation is dealt with by looking only at days when precipitation is presumably liquid or by considering the occurrence and non-occurrence of precipitation. Away from non- resolved orography, the long term means (months, years) of observed and simulated precipitation are often /media/ces/Paper-Olafur-Rognvaldsson_92.pdf
  • 22. VI_2020_005

    and CNES, n.d.; National Center for Atmospheric Research Staff, 2016; Quante and Colijn, 2016). Now, additional altimeters at different orbits perform slightly less accurate measurements up to 82 N and S (Rhein et al., 2013). These records are used to estimate sea surface changes and calculate global mean sea level, a temporal average sea level averaged over the oceans (Church, Clark, et al., 2013 /media/vedurstofan-utgafa-2020/VI_2020_005.pdf
  • 23. Henriksen_Barlebo-2008-AWM_BBN-Journ_Env_Management

    and to list categories of stakeholders such as water users, potential groundwater pollution sources, and autho- rities in the area including: local waterworks; water consumers; farmers; industry; anglers; the local county; and three municipalities. The stakeholder involvement process and the extension of the organisation with new Define context Collect dat a Define states Identify factors, ac tion s /media/loftslag/Henriksen_Barlebo-2008-AWM_BBN-Journ_Env_Management.pdf
  • 24. Observations - Eskifjörður

    wind : 10 / 14Precip.: 0.0 mm / 1 h 22 GMT 0.0° S 8 Max wind : 8 / 12Precip.: 0.0 mm / 1 h 21 GMT 0.3° S 8 Max wind : 10 / 14Precip.: 0.0 mm / 1 h 20 GMT 0.6° S 9 Max wind : 9 / 14Precip.: 0.0 mm / 1 h 19 GMT 1.3° S 9 Max wind : 9 / 14Precip.: 0.0 mm / 1 h 18 GMT 1.9° S 7 Max wind : 8 / 13Precip.: 0.0 mm / 1 h 17 GMT 3.0° SW 7 Max wind : 8 /m/observations/areas
  • 25. VI_2014_005

    ] MAE [m s 1] Orig. Corr. Orig. Corr. Orig. Corr. Orig. Corr. January -1.03 -0.14 1.71 1.42 -1.23 -0.32 2.37 2.16 July -0.14 -0.10 1.16 1.16 -0.89 -0.30 1.62 1.50 20 Figure 11. Monthly averages (January blue; July red) of original or corrected SURFEX 2-m air temperature (top row) and 10-m wind speed (bottom row), in comparison with station measurements. 21 Figure 12. Average diurnal cycles of 2-m /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_005.pdf
  • 26. Traffc-maintenance_expenditures

    229 1 587 160 1970 18 591 42 413 2 166 86 101 - 892 5 131 2 310 201 - - - 157 805 1 652 904 1969 17 559 38 840 2 313 93 776 - 922 4 562 1 571 - - - - 159 543 1 832 354 1968 13 474 36 376 3 074 104 519 - 1 080 4 131 1 156 - - - - 163 811 1 964 368 1967 11 139 34 495 5 940 95 857 - 419 3 032 1 087 - - - - 151 968 1 936 249 1966 9 835 32 581 8 349 94 777 - 587 4 205 1 743 - - - - 152 077 2 032 936 /media/loftslag/Traffc-maintenance_expenditures.pdf
  • 27. VI_2019_009

    weather [SYNOP code] Number of obse rv ation s Station Manual Automatic Figure 13. Frequency of present weather (SYNOP codes) observed by both stations. 0 50 100 150 1 2 3 10 11 15 16 20 21 23 24 25 26 40 41 50 51 52 53 58 60 61 62 63 64 67 70 71 72 73 80 81 83 84 85 Present weather [SYNOP code] Number of obse rv ation s Station Manual Automatic Figure 14. Frequency of present weather (SYNOP /media/vedurstofan-utgafa-2019/VI_2019_009.pdf
  • 28. 2013_001_Nawri_et_al

    storm systems, whereby in many parts of the island low-level wind speeds in excess of 20 m s 1 in winter are not uncommon. Small-scale convective storm systems are less important in Iceland than at mid- and low-latitudes. Unlike over mid-latitudes continental regions, thunder- storms in Iceland are most common during the winter months (Dec – Feb) (Einarsson, 1976). They typically form when cold air /media/vedurstofan/utgafa/skyrslur/2013/2013_001_Nawri_et_al.pdf
  • 29. Lorenzoni_Pidgeon_2006

    level, surveys commissioned by the European Com- munity/the European Union provide an indication of trends in concern about cli- mate change. Since 1992, such surveys have been undertaken among representative samples of citizens in its Member States, and specifically on topics related to the environment (Special Eurobarometers (EB) in 1992, 1995, 2002; and a Flash EB in 2002). These have included /media/loftslag/Lorenzoni_Pidgeon_2006.pdf
  • 30. VI_2020_004

    Figure 53 Impact map for airports in case of an eruption like 1362 at Öræfajökull ................ 82 Figure 54 Impact map for power lines in case of an eruption like 1362 at Öræfajökull ......... 83 Figure 55 5% PM10 probability map for an eruption like 1362 at Öræfajökull. ...................... 84 Figure 56 25% PM10 probability map for an eruption like 1362 at Öræfajökull /media/vedurstofan-utgafa-2020/VI_2020_004.pdf

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