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• 41. CES_D2.4_VMGO

  is the world’s coldest country with its annual mean area averaged temperature of -4.1ºC. Projections with the global climate models provide a physically consistent quantitative picture of climate change through the 21st century. The model projected mean warming will plausibly be accompanied by changes in the extremes that exhibit considerable interregional differences. The extremes at limited /media/ces/CES_D2.4_VMGO.pdf

• 42. Group2-report

   1 orange, Society 2 green, Society 3 purple).   The combinations of climate conditions and socio economic conditions are frames which are used for back  casting, i.e. the goal of good water quality is achieved by measures which are consistent with the frame.  This study is limited to three frames, consisting of the combinations listed in Table 2.    The scenario  consists of a set of measures /media/loftslag/Group2-report.pdf

• 43. Lorenzoni_Pidgeon_2006

  weather events with the potential to influence people’s views. Opinion polls have also investigated people’s knowledge of the causes of cli- mate change. Generally, individuals are found to have a limited understanding of the human contributions to a changing climate. Research mainly in developed na- tions during the mid to late 1990s has shown that most citizens do not have a clear understanding /media/loftslag/Lorenzoni_Pidgeon_2006.pdf

• 44. Bárðarbunga 2014 - August events

  ) The migration of magma could stop, attended by a gradual reduction in seismic activity. 2) The dike could reach the surface of the crust, starting an eruption. In this scenario, it is most likely that the eruption would be near the northern tip of the dike. This would most likely produce an effusive lava eruption with limited explosive, ash-producing activity. 3) An alternate scenario would be the dike /earthquakes-and-volcanism/articles/nr/3000

• 45. Bardarbunga-2014_August-events

  In this scenario, it is most likely that the eruption would be near the northern tip of the dike. This would most likely produce an effusive lava eruption with limited explosive, ash-producing activity. 3) An alternate scenario would be the dike reaching the surface where a significant part, or all, of the fissure is beneath the glacier. This would most likely produce a flood in Jökulsá á Fjöllum /media/jar/Bardarbunga-2014_August-events.pdf

• 46. VI_2021_008

  or for the audio alarm. • Silence audio: The audio alarm can be silenced for the ALERT module if this variable is changed from “False” to “True.” This is useful if the ALERT module is desired to be used for research instead of monitoring purposes. • Max audio per hour: The number of audio alarms triggered per hour can be limited within this variable. This is especially useful if there is an ongoing /media/vedurstofan-utgafa-2021/VI_2021_008.pdf

• 47. Bárðarbunga 2014 - August events

  ) The migration of magma could stop, attended by a gradual reduction in seismic activity. 2) The dike could reach the surface of the crust, starting an eruption. In this scenario, it is most likely that the eruption would be near the northern tip of the dike. This would most likely produce an effusive lava eruption with limited explosive, ash-producing activity. 3) An alternate scenario would be the dike /earthquakes-and-volcanism/articles/nr/3000/

• 48. Kok_1-scenarios-lecture-1

  – intuitive vs formal: VI. Data: qualitative vs quantitative VII. Method of data collection: participatory vs desk research VIII. Resources: extensive vs limited IX. Institutional conditions: open vs constrained Scenarios - types HOW? C Scenario content - complex vs simple: X. Temporal nature: chain vs snapshot XI. Variables: heterogeneous vs homogenous XII. Dynamics: peripheral vs trend XIII. Level /media/loftslag/Kok_1-scenarios-lecture-1.pdf

• 49. Public-Choice-2012---McGuiness-and-Walker---Foundations-of-the-Ostrom-workshop---institutional-analysis,-polycentricity,-and-self-governance-of-the-commons

  into distinct units of private property. Slowly, a growing number of field researchers documented the geographical and histor- ical prevalence of successful systems of management through which communities of user groups effectively limited access to a resource and thereby avoided the supposedly inevitable tragedy of the commons (e.g., Bromley et al. 1992; Berkes et al. 1989; Feeny et al. 1990; Netting /media/loftslag/Public-Choice-2012---McGuiness-and-Walker---Foundations-of-the-Ostrom-workshop---institutional-analysis,-polycentricity,-and-self-governance-of-the-commons.pdf

• 50. 2010_005_

  periods of time and over smaller spatial scales. In general, regional climate projections are derived either directly from one or more general cir- culation model (GCM) runs, or through additional numerical or statistical downscaling of these large-scale fields. Numerical downscaling uses higher-resolution regional climate models (RCMs) over a limited area to refine global GCM simulations. Problems /media/ces/2010_005_.pdf