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41. VI_Arsskyrsla_2018_vef
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42. 2010_005_
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43. VI_2015_009
Rist, S. (1990). Vatns er þörf. Bókaútgáfa Menningarsjóðs. 248 pp. (In Icelandic). Zaman, M.A., Rahman, A. & Haddad, K. (2012). Regional flood frequency analysis in arid regions. A case study for Australia. J. Hydrol., 475, 74-83. 25 Appendix I - Identification of homogeneous groups of catch- ments obtained with the ROI technique and associated growth curves −2 0 2 4 6 0 1 2 3 4 −ln(−ln(1−1/T)) q(T /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_009.pdf -
44. GA_2009_91A_4_Andreassen
and for the combination of +2°C and +10% P perturbationsthe length of the ice melt period is 83 days, slight-ly lower due to the 10% increase in P. DiscussionSelection of input dataThe good correlation between precipitation meas-ured west of the water divide and bw at Storbreenreveals that many stations are suitable to be used asinput data. The poor correlation with stations eastof the glacier /media/ces/GA_2009_91A_4_Andreassen.pdf -
45. Public-Choice-2012---Teyssier---Inequity-and-risk-aversion-in-sequential-public-good-games
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46. 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 -
47. 2010_012rs
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48. Journal_of_Hydrology_Veijalainen_etal
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49. VI_2020_011_en
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50. ces-oslo2010_proceedings
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