91 results were found for Y アイリス〈ωωω,RTЗЗ,TOP〉コード:B77〉ミップスロット༿トラットfc🤞サッカートトサイト💛マカオベネシアン╜ソマリアの国家戦㍁パワーボールピクスター∿ジョージアサッカー␇プロトライブスコア∔.adq/.

Results:

• 81. GA_2009_91A_4_Andreassen

  andEnergy Directorate (NVE), Oslo, Norway2Department of Geosciences, University of Oslo, Norway3Institute for Marine and Atmospheric Research, Utrecht University, Utrecht, the Netherlands Andreassen, L. and Oerlemans, J., 2009: Modelling long-term summer and winter balances and the climate sensitivity of Stor-breen, Norway. Geogr. Ann. 91 A (4): 233–251. ABSTRACT. Measurements of winter balance (bw /media/ces/GA_2009_91A_4_Andreassen.pdf

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

  are also optimal for individuals (Ahn et al. 2001, 2003; Ostrom 1998). However, empirical analysis is required to specify which types of social S. Teyssier () INRA, UR1303 ALISS, 94200 Ivry-sur-Seine, France e-mail: Sabrina.Teyssier@ivry.inra.fr 92 Public Choice (2012) 151:91–119 preference are relevant for public-choice theory. This kind of work is still only rare in the literature, even though /media/loftslag/Public-Choice-2012---Teyssier---Inequity-and-risk-aversion-in-sequential-public-good-games.pdf

• 83. Kok_JGEC658_2009

  that such a system can potentially be in equilibrium. It is more Fig. 4. Output of various Fuzzy Cognitive Maps. X-axis: number of iteration steps; Y-axis: value of selected concepts. K. Kok / Global Environmental Change 19 (2009) 122–133128 Author's personal copy significant that it can be maintained without any policy incentive (C12 < 0.05 after 20 iterations). In terms of the Fuzzy Cognitive Map, using /media/loftslag/Kok_JGEC658_2009.pdf

• 84. Lorenzoni_Pidgeon_2006

  their lifestyles for this purpose. Of those who would be prepared to change their way of living, most (92% to 96%) favoured options that could be easily undertaken in the home, and that would cost almost nothing, like recycling and using less energy. Fewer favoured reducing their private transport (68% would use the car less; 62% would take fewer flights), whilst price increases were not popular (only 37 /media/loftslag/Lorenzoni_Pidgeon_2006.pdf

• 85. VI_2020_008

  Lykilorð: Undirskrift framkvæmdastjóra sviðs: úrkoma, endurkomutími, aftakagreining, þröskuldsaðferðin, 1M5 kort, IDF ferlar precipitation, rainfall, extreme value analysis, return periods, 1M5 map, IDF curves Undirskrift verkefnisstjóra: Yfirfarið af: SG, TóJ, TJ, EBJ Lykilsíða 5 Contents GLOSSARY /media/vedurstofan-utgafa-2020/VI_2020_008.pdf

• 86. VI_2016_006_rs

  wide and 1000 m long shelf called Þófi, terminating at 80–100 m a.s.l., see Map 4. The inclination of the shelf is 15 on average. The surface of Þófi is covered with unconsolidated glacial till and landslide deposits and marked with five gullies. The brook called Þófalækur near the middle of the shelf divides it into an inner and outer part. On the outermost part of the shelf, there is a small /media/vedurstofan-utgafa-2016/VI_2016_006_rs.pdf

• 87. 2010_012rs

  Processes in South-West Iceland VÍ 2010- 012 ISSN 1670- 8261 Report +354 522 60 00 +354 522 60 06 vedur@vedur. is Veðurst of a Íslands Bústaðaveg ur 9 150 Reyk j avík Kristín S. Vogfjörd, Icelandic Met Office Einar Kjartansson, Icelandic Met Office Ragnar Slunga, QuakeLook AB Stockholm Páll Halldórsson, Icelandic Met Office Sigurlaug Hjaltadóttir, Icelandic Met Office Gunnar B /media/vedurstofan/utgafa/skyrslur/2010/2010_012rs.pdf

• 88. vanRoosmalen_etal-2009-WRR_2007WR006760

  and Relative Changes When Comparing the A2 and B2 Scenarios to the Current Climatea Scenario Net Recharge Horizontal Boundary Outflow Drain Flow Base Flow Water Supply Irrigation Simulations Not Including Abstractions and Irrigation Current climate 550 23 279 252 A2 scenario + 67 (12%) + 1 (4%) + 56 (20%) + 13 (5%) B2 scenario + 113 (21%) + 1 (4%) + 92 (33%) + 22 (9%) Simulations Including Abstractions /media/loftslag/vanRoosmalen_etal-2009-WRR_2007WR006760.pdf

• 89. VI_2013_008

  Forecast skill evaluation over the period 01/09/2001–31/08/2005. No rescaling (Eqs. 6 and 10). All units are in m3=s Forecast range T=1 day T=2 days T=3 days Statistics ME RMSE Q95–Q5 ME RMSE Q95–Q5 ME RMSE Q95–Q5 vhm 64 – method 1 –20 103 302 –19 99 297 –20 103 298 vhm 64 – method 2 –11 44 132 –15 64 162 –18 87 201 vhm 64 – method 3 –24 64 206 –24 72 221 –25 87 241 vhm 64 – method 4 –16 47 132 /media/vedurstofan/utgafa/skyrslur/2013/VI_2013_008.pdf

• 90. VI_2020_011_en

  –8% likelihood that a vent will open on Heimaey. In other words, there is a 92–97% likelihood that the next eruption within the volcanic system will not be on Heimaey. The most densely populated parts of Heimaey in the north and around the harbor are the most vulnerable to Moderate and Large lava flows originating on the island. Almost all infrastructure on the island is vulnerable to lava /media/vedurstofan-utgafa-2020/VI_2020_011_en.pdf