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  • 31. Hare-2011-ParticipatoryModelling

    : 10.1002/eet 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17 18 19 20 21 22 23 24 25 26 27 28 29 30 31 32 33 34 35 36 37 38 39 40 41 42 43 44 45 46 47 48 49 50 51 52 53 54 55 56 57 Example 5: Nîmes (Etienne et al., 2008b). This process sought to support social learning and develop collective management ideas for urban re prevention, whilst developing conceptual and simulation models. It is an uncommon /media/loftslag/Hare-2011-ParticipatoryModelling.pdf
  • 32. Henriksen_Barlebo-2008-AWM_BBN-Journ_Env_Management

    in the data used in making the decision and the factors are interlinked, all of which makes the problem highly complex. The part of the net defined by variables and links is relatively easily communicated to stakeholders (Henriksen et al., 2007b). However the tal Management 88 (2008) 1025–1036 quantitative part, with the conditional probability tables (CPTs), the numbers, is the step where /media/loftslag/Henriksen_Barlebo-2008-AWM_BBN-Journ_Env_Management.pdf
  • 33. High resolution precipitation maps for Iceland

    using an orographic precipitation model. This model retains the essential physics and dynamics of orographic precipitation such as airflow dynamics, hydrometeor formation and fallout times as well as lee-side evaporation. This procedure makes it possible to simulate the distribution of precipitation in much more detail than has been done until now in Iceland and opens up new possibilities /weather/articles/nr/1625
  • 34. norsem_palli

    boundaries are frequently characterized by complicated fault patterns, which makes their seismogenic potential and seismic hazard difficult to assess. The Reykjanes Peninsula oblique rift has an over-all trend of 70°, highly oblique with respect to the spreading direction, 101° in this region. It contains both volcanic systems and seismogenic strike-slip faults /media/norsem/norsem_palli.pdf
  • 35. Group1-Adaptive_Management_in_a_relation_to_climate_change2

    -Community training Low taxation Scenario building Risk Perception Socio Economic Development H ig h Lo w Scenario 1 Scenario 2 Present time 2030 2020 Scenario 1 Scenario 1opt. Flood Warning System • The operator, based on analysis of the received weather data and other information from the Internet makes the decision whether to warn inhabitants • A computer /media/loftslag/Group1-Adaptive_Management_in_a_relation_to_climate_change2.pdf
  • 36. NONAM

    to adaptation policy development and related investments, notably regarding infrastructures of various kinds (energy, transport, water & sanitation, communication) and the overarching planning and management systems that create the context in which these systems are designed and operated (urban and coastal zone management e.g. planning and disaster prevention & -relief and rescue) comparability /nonam
  • 37. NONAM

    to adaptation policy development and related investments, notably regarding infrastructures of various kinds (energy, transport, water & sanitation, communication) and the overarching planning and management systems that create the context in which these systems are designed and operated (urban and coastal zone management e.g. planning and disaster prevention & -relief and rescue) comparability /nonam/
  • 38. VanderKeur_etal-2008-Uncertainty_IWRM-WARM

    strategies with existing policies or practices under alternative scenarios, including uncertainty. This leads not to direct problem solving, but rather to increasing the adaptive capacity of the system and raising increased awareness among water managers that a substantial part of the information they use is highly uncertain. Within the IWRM system, depicted in Fig. 2, uncertainty emerges at every /media/loftslag/VanderKeur_etal-2008-Uncertainty_IWRM-WARM.pdf
  • 39. Map of the Glaciers of Iceland

    This is the reason that the Icelandic Meteorological Office published the map, to show all of the glaciers of Iceland and the changes to them which took place during the last century. On the Map of the Glaciers of Iceland the outlines of all the glaciers are shown together, thus it is easy to see their distribution and the comprehensive record of the changes to them. The map shows the greatest extent /about-imo/news/nr/2712
  • 40. Factsheet_Bardarbunga-140910

    repeatedly as concentrations of gas reached dangerous levels due to sudden changes in wind conditions. o At the eruption site, local wind anomalies can occur due to thermal convection from the hot lava. This makes the conditions on site extremely dangerous as winds can change suddenly and unpredictably.  Around 80 earthquakes have been recorded since midnight. The largest two /media/jar/myndsafn/Factsheet_Bardarbunga-140910.pdf

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