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• 61. Milly_etal-2008-Stationarity-dead-Science

  ), S. Solomon et al., Eds. (Cambridge Univ. Press, New York, 2007), pp. 1–18; www.ipcc.ch/press/index.htm. 5. IPCC, in Climate Change 2007: Climate Change Impacts, Adaptation and Vulnerability, Contribution of WG2 to AR4, M. L. Parry et al., Eds. (Cambridge Univ. Press, New York, 2007), pp. 1–16. 6. I. M. Held, B. J. Soden, J. Clim. 19, 5686 (2006). 7. T. P. Barnett, J. C. Adam, D. P. Lettenmaier /media/loftslag/Milly_etal-2008-Stationarity-dead-Science.pdf

• 62. Kok_et_al._TFSC_published_2011

  ]. There is ample experience with backcasting, and consequently much has been said about the underlying principles (e.g. [20]), the methodological 838 K. Kok et al. / Technological Forecasting & Social Change 78 (2011) 835–851 Author's personal copy framework (e.g. [8,30–32]), and practical applications (e.g. [33–35]). Also the combination between backcasting and other types of scenarios has been /media/loftslag/Kok_et_al._TFSC_published_2011.pdf

• 63. 2013_001_Nawri_et_al

  and a pressure of 1013.25 hPa. In the case of Iceland, the climate deviates significantly from these standard atmospheric conditions. Additionally, terrain elevation varies considerably across the island. Therefore, seasonal and annual differences in air density from the standard value, as well as spatial variability, need to be taken into account. Approximate air density can be calculated by assuming /media/vedurstofan/utgafa/skyrslur/2013/2013_001_Nawri_et_al.pdf

• 64. Eriksson_Garvill_Nordlund_2006

  and infringement on freedom, and indirectly associated with the acceptability of road pricing. In addition, relations between beliefs about effectiveness and acceptability of TDM measures have been shown. More specifically, the more effective a measure is perceived to be, the more acceptable it is (e.g. Bamberg & Ro¨lle, 2003; Nordlund & Garvill, 2006; Rienstra et al., 1999). For coercive measures /media/loftslag/Eriksson_Garvill_Nordlund_2006.pdf

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

  individuals act like homo-œconomicus agents (see for example Andreoni 1988; Berg et al. 1995; Camerer 2003; Forsythe et al. 1994; Isaac et al. 1984). Recent developments in public-choice theory have taken a behavioral approach to broaden the analysis of collective action. The introduction of social preferences, such as altruism, inequity aversion or trust, may mean that optimal collective choices /media/loftslag/Public-Choice-2012---Teyssier---Inequity-and-risk-aversion-in-sequential-public-good-games.pdf

• 66. 2010_005_

  that during the summer by about half a degree. Adding the calculated warming for the 2 CO2 equilibrium to the observations at Stykkishólmur, resulted in predicted temperatures close to those at Bergen, Norway during the summer, and to those at Lerwick, Shetland Islands during the winter. The study also examined projected changes in precipitation and found that on an annual basis precipitation /media/ces/2010_005_.pdf

• 67. Instructions for weather radar pages

  : It is possible to click the bar anywhere. It is possible to click on a day above the bar to view the noon forecast for that specific day. It is possible to click on a specific time below the bar. It is possible to click on the arrows to both sides of the bar to view a previous or newer time range. It is possible to use the left and right arrows on the keyboard to view a previous or newer /weather/articles/nr/1221

• 68. IMO at the Arctic Circle Assembly 2017

  the USA, the European Space Agency (ESA) and China.Ingvar Kristinsson, managing director at IMO, participated in a session on the potential effects of volcanic ash clouds from Icelandic volcanoes on aviation in the Arctic airspace. In a special session on issues related to Arctic Freshwater, Halldór Björnsson and Þorsteinn Þorsteinsson contributed to a discussion on freshwater fluxes /about-imo/news/imo-at-the-arctic-circle-assembly-2017

• 69. The segmented dyke intrusion explained

  to time of occurrence and the colour code is shown at the top of the map. The earthquake locations delineate the track of the dyke intrusion from Bárðarbunga volcano to the eruption site at Holuhraun. Vertical cross sections through the crust are also shown; looking from the south (below) and east (to the right). Triangles mark the locations of seismic stations in and around the glacier. Data /about-imo/news/nr/3038

• 70. Bardarbunga_kafli20140825

  have not been located it is not clear whether eruptions on the central part of the system belong to a central volcano or the ice covered fissure swarm. Both cases will generate jökulhlaups from rapidly melting ice. All explosive eruptions originating below ice are therefore described together. 4 4.1 Bárðarbunga central volcano and adjacent ice covered fissure swarm 1. Phreatomagmatic /media/jar/Bardarbunga_kafli20140825.pdf