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Results:

• 1. Public-Choice-2012---Teyssier---Inequity-and-risk-aversion-in-sequential-public-good-games

  Public Choice (2012) 151:91–119 DOI 10.1007/s11127-010-9735-1 Inequity and risk aversion in sequential public good games Sabrina Teyssier Received: 5 January 2010 / Accepted: 12 October 2010 / Published online: 3 November 2010 ³ Springer Science+Business Media, LLC 2010 Abstract Behavioral hypotheses have recently been introduced into public-choice theory (Ostrom in American Political Science /media/loftslag/Public-Choice-2012---Teyssier---Inequity-and-risk-aversion-in-sequential-public-good-games.pdf

• 2. VI_2020_008

  Figure 8. Stations ranked according to their average CC for the 20 highest rainfall daily events. ................................................................................................................................................... 33 Figure 9. Ranked values of the 50 highest 24-hour accumulated precipitation events plotted against ranked values of the 50 highest daily precipitation /media/vedurstofan-utgafa-2020/VI_2020_008.pdf

• 3. The

  2017, 66 above the 1961 to 1990 mean, but 91 fewer than the mean of the last ten years (2007 to 2016). In Akureyri the total was 932.8, 112 below the 1961 to 1990 average and 137 fewer than the mean of the last ten years (2007 to 2016). August was sunny in Reykjavík, but in most of the other months the sunshine duration was around normal. There was particularly little sunshine /about-imo/news/the-weather-in-iceland-in-2017

• 4. Hydropower - Glacier, Snow and Ice

  Guðmundsson, S., Björnsson, H., Pálsson, F., Jóhannesson, T., Hannesdóttir, H. o.fl. (2011). Modelling the 20th and 21st century evolution of Hoffellsjökull glacier, SE-Vatnajökull, Iceland. The Cryosphere, 5, 961-975, doi:10.5194/tc-5-961-2011. Andreassen, L. M., & Oerlemans, J. (2009). Modelling long-term summer and winter balances and the climate sensitivity of Storbreen, Norway. Geogr. Ann., 91 /ces/publications/nr/1940

• 5. Isskyrsla_20100407

  N66°44.92' W025°08.94' 79. N66°45.01' W025°08.50' 80. N66°46.32' W025°10.27' 81. N66°46.73' W025°07.19' 82. N66°46.01' W025°04.86' 83. N66°46.22' W025°04.33' 84. N66°47.12' W025°06.45' 85. N66°47.26' W025°04.36' 86. N66°48.44' W025°03.60' 87. N66°49.10' W025°04.45' 88. N66°51.68' W025°03.27' 89. N66°53.36' W024°59.25' 90. N66°55.39' W024°58.89' 91. N66°55.82' W024°58.13' 92. N66°56.15' W025°01.15 /media/hafis/skyrslur_lhg/Isskyrsla_20100407.pdf

• 6. Helle_Katrine_Andersen_(DANVA,_Dk)

  Vision for Proactive Climate Change Adaptation in the Danish Water Sector Speaker: Helle Katrine Andersen, DANVA hka@danva.dk To inspire water utilities to develop climate change adaptation strategies and to implement CC adaptation solutions The Danish Water and Waste Water Association (DANVA) has developed a vision for Proactive Climate Change Adaptation in the Water Sector /media/loftslag/Helle_Katrine_Andersen_(DANVA,_Dk).pdf

• 7. The weather in Iceland in 2018

  in Reykjavík in June was only 70, 91 below the 1961 to 1990 and have not been as few since 1914. Precipitation was heavy in those parts of the country and it was relatively cold. Meanwhile it was warm and sunny in the East, with several days with temperature reaching over 20 degrees. South- and southwesterly winds were prevailing. July July was warm and sunny in the East but cool /about-imo/news/the-weather-in-iceland-in-2018

• 8. 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

• 9. BIHN_windrose_2005-2014

  W N (Number of observations for wind direction) Icelandic Met Office 02. júl. 2015 68 0 62 9 111 2 167 0 117 5 70 6 26 7 25 4 58 7 47 3 36 6 101 3 91 1 53 1 117 0 73 6 44 2 72 7 38 7 60 4 113 6 70 0 109 3 130 5 26 1 12 5 30 0 14 4 10 5 34 6 17 0 29 4 114 3 158 0 146 5 172 7 Wind rose BIHN January 2005−2014 90 80 70 60 50 40 30 2010360350340 330 320 310 300 290 280 270 /media/vedur/BIHN_windrose_2005-2014.pdf

• 10. VI_2020_004

  ) ................. 89 Figure 61 Tephra accumulation rate on the ground on 8 October 1982 (Öræfajökull) ............ 90 Figure 62 Tephra accumulation rate on the ground in Skaftafell (Öræfajökull) ...................... 91 Figure 63 Preliminary intersectional map ................................................................................ 93 Figure 65 Initial user-interface of the public web-site /media/vedurstofan-utgafa-2020/VI_2020_004.pdf