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Results:

51. BIEG_windrose_2005-2014

N (Number of observations for wind direction) Icelandic Met Office 02. júl. 2015 778 5 1016 4 491 0 235 8 95 2 68 6 41 5 45 4 70 0 55 7 31 9 63 7 47 6 51 1 146 2 162 3 242 3 505 1 345 2 459 6 494 2 417 2 371 5 220 7 73 2 45 3 66 2 32 4 27 5 53 0 40 6 63 8 106 0 90 7 97 1 277 8 Wind rose BIEG January 2005−2014 90 80 70 60 50 40 30 /media/vedur/BIEG_windrose_2005-2014.pdf
52. VI_2019_009

are shown in appendix. Table 1 shows the equivalence between some of them, yet the original codes will be used in the figures. Table 1. Present weather codes from the automatic station during this period of time mapped to the codes from the manual station. Automatic Manual Automatic Manual 0 0,1,2,3 61 60,61 10 10 62 62,63 20 42,43 64 66 21 14,15,16,50,51, 67 68 60,61,70,71 23 21, 60, 61 71 70,71 24 /media/vedurstofan-utgafa-2019/VI_2019_009.pdf
53. IMO_AnnualReport2014

and Oceanography 66, Article No: 25421; DOI: 10.3402/tellusa.v66.25421. Jonassen, M. O., Hálfdán Ágústsson & Haraldur Ólafsson (2014). Im- pact of surface characteristics on flow over a mesoscale mountain. Quarterly Journal of the Royal Meteorological Society 140(684), 2330-2341; DOI: 10.1002/qj.2302. Muri, H., Jón Egill Kristjánsson, T. Storelvmo & Melissa Anne Pfe?er (2014). The climatic e?ects /media/vedurstofan/utgafa/skyrslur/2015/IMO_AnnualReport2014.pdf
54. VI_2020_004

/m2 (Katla) ............................ 65 Figure 38 Seasonal analysis for tephra probability exceeding 1 kg/m2 (Katla) ....................... 66 Figure 39 Seasonal analysis for tephra probability exceeding 10 kg/m2 (Katla) ..................... 67 Figure 40 Seasonal analysis for tephra probability exceeding 100 kg/m2 (Katla) ................... 68 Figure 41 Impact map for road network in case /media/vedurstofan-utgafa-2020/VI_2020_004.pdf
55. VI_2015_009

= 66 IFM cross−validation l l l l l l l ll l ll 0 400 800 1200 0 50 0 100 0 150 0 Pred. (m³/s) R ef . (m ³/s ) µ(D)=(θ0)(AP)(θ1) Rel. RMSE= 0.54 NS= 0.95 MAE= 52 l l l l l l l ll l ll 0 500 1000 0 50 0 100 0 200 0 Pred. (m³/s) R ef . (m ³/s ) µ(D)=(θ0)(AP Z)(θ1) Rel. RMSE= 1.1 NS= 0.71 MAE= 111 l l l l l l l ll l ll 0 400 800 1200 0 50 0 100 0 150 0 Pred. (m³/s) R ef . (m ³/s ) µ(D)=(θ0)(AP L)(θ1 /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_009.pdf
56. Kok_et_al._TFSC_published_2011

17 24 64 Sustainability Eventually 5 3 30 28 66 Fortress Europe 18 11 30 23 72 Policy Rules 6 5 13 17 41 Total 44 27 80 92 243 844 K. Kok et al. / Technological Forecasting & Social Change 78 (2011) 835–851 Author's personal copy sector. The presence of various climate-related strategies is a consequence of the presence of climate-related obstacles and opportunities. 3.4.6. Robust elements Results /media/loftslag/Kok_et_al._TFSC_published_2011.pdf
57. IPPC-2007-ar4_syr

judgment and statistical analysis of a body of evidence (e.g. observations or model results), then the following likelihood ranges are used to express the assessed probability of occurrence: virtually certain >99%; extremely likely >95%; very likely >90%; likely >66%; more likely than not > 50%; about as likely as not 33% to 66%; unlikely <33%; very unlikely <10%; extremely unlikely <5 /media/loftslag/IPPC-2007-ar4_syr.pdf
58. VI2010-006_web

18 árið 1990 og aurblandað vatnsflóð sem stórskemmdi Aðalstræti 66 árið 1974 eru dæmi um alvarlegri skriður sem fallið hafa á svæðinu. Tafla 5: Yfirlit yfir þekkt skriðuföll og leysingaflóð úr Akureyrarbrekkum. Númer Tími Lýsing – 19. öld Á gömlu málverki frá því um miðja 19. öld (1857), sem sjá má í I. bindi Sögu Akureyrar (Jón Hjaltason, 1990), sést greinilegt skriðuör neðarlega í brekkunni ofan /media/vedurstofan/utgafa/skyrslur/2010/VI2010-006_web.pdf
59. Gudmundsson-etal-2011-PR-7282-26519-1-PB

2009. Simila- rities and differences in the response of two ice caps in Iceland to climate warming. Hydrology Research 40, 495502. Gudmundsson M.T., Ho¨gnado´ttir T., Kristinsson A.B. & Gudbjo¨rnsson S. 2007. Geothermal activity in the subglacial Katla caldera, Iceland, 19992005, studied with radar altimetry. Annals of Glaciology 45, 6672. Gudmundsson M.T., Pedersen R., Vogfjo¨rd K /media/ces/Gudmundsson-etal-2011-PR-7282-26519-1-PB.pdf
60. 2013_001_Nawri_et_al

. . . . . . . . . . . . 65 36 Seasonal mean wind power density within the Skagi region . . . . . . . . . . . . . 66 37 Directional mean wind power density within the Snæfellsnes region . . . . . . . . 67 38 Seasonal mean wind power density within the Snæfellsnes region . . . . . . . . . . 68 39 Directional mean wind power density within the Þorlákshöfn region . . . . . . . . 69 40 Seasonal mean wind /media/vedurstofan/utgafa/skyrslur/2013/2013_001_Nawri_et_al.pdf