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Results:

• 21. Hazard zoning

  in the legend (left part of the map) and in the figure caption (the phrase below the map). The colour scale reports different values of likelihood (under 1% has no colour). The maps have been made considering 10 years of meteorological data and computing the ground concentration each hour with the CALPUFF gas dispersion model. The results have been plotted considering the wind variability across /pollution-and-radiation/volcanic-gas/hazard-zoning

• 22. Henriksen_Barlebo-2008-AWM_BBN-Journ_Env_Management

  and provide a narrative approach for tool enhancement. r 2007 Elsevier Ltd. All rights reserved. Keywords: Groundwater management; Bayesian belief networks; Qualitative interview; Adaptive management; IWRM; Tool enhancement; Participatory integrated assessment; Social learning; Newater; Organizational complexity 1. Introduction and indexes are available e.g. poverty index, water stress index etc /media/loftslag/Henriksen_Barlebo-2008-AWM_BBN-Journ_Env_Management.pdf

• 23. VI_2020_005

  flooding, sea level, sea level rise, risk assessment, natural hazard This work was carried out for the Icelandic Meteorological Office and is a part of Masters Thesis ISSN 1650-6553 No. 470, published by the Department of Earth Sciences at Uppsala University in 2019. The Masters Thesis is available as a whole at www.diva-portal.org. Copyright c Guðrún Elín Jóhannsdóttir Contents 1 Introduction /media/vedurstofan-utgafa-2020/VI_2020_005.pdf

• 24. ECONOMIC_EFFECTS_OF_CLIMATE_CHANGE_ON_THE_TOURISM_SECTOR_IN_SPAIN

  changes in many natural systems. Moreover, it also presents, in a greater or lesser extent, economical effects in nearly every sector of activity. In this context, the tourism will be particularly affected [1; 2]. There will be regional and seasonal shifts in global tourist flows, leaving some countries more vulnerable to shifting climatic conditions [3]. European Mediterranean countries /media/loftslag/ECONOMIC_EFFECTS_OF_CLIMATE_CHANGE_ON_THE_TOURISM_SECTOR_IN_SPAIN.pdf

• 25. Perrels-CBA

  26.8.2011Adriaan Perrels/IL 6 Review of climate change effects in built-up areas (1) Source: IPCC 4AR_2 Source: IPCC 4AR_2 26.8.2011Adriaan Perrels/IL 7 Source: IPCC 4AR_2 Review of climate change effects in built-up areas (2) 26.8.2011Adriaan Perrels/IL 8 Cost-benefit analysis – the basics 1 • CBA: • assess for the estimated lifetime of a project the annual expenditures (investment funding cost /media/loftslag/Perrels-CBA.pdf

• 26. askja_minnisblad_ens

  are photographs, maps and graphs that show the main results of measurements and analyses that are available, now two weeks after the event.  Width of fracture line: 800 m  Vertical drop: 350 m  Runout length beyond the lake shore: ~1000 m  Volume: ~30–50 million m³  Estimated duration of the slide: 20 seconds according to seismographs  Travel time of tsunami across the lake: 1–2 minutes /media/ofanflod/myndasafn/frodleikur/askja_minnisblad_ens.pdf

• 27. Mo_Birger_CES_2010

  Introduction Electricity system model Simulation results Summary and concluding remarks Energy systems Quantitative analysis of the NordPool electricity system Birger Mo, Ove Wolfgang, Joar Styve Sintef Energy Research 02.06.2010 Sintef Energy Research Quantitative system analysis 1 of 21 Introduction Electricity system model Simulation results Summary and concluding remarks Outline Methodology 1 /media/ces/Mo_Birger_CES_2010.pdf

• 28. VI_2009_006_tt

  the discharge in Skaftá and the temperature of the flood water close to the glacier margin were measured. The dis- charge from the subglacial lake during the jökulhlaup was calculated using a hypso- metric curve for the subglacial lake, estimated from the form of the surface cauldron after jökulhlaups. The maximum outflow from the lake during the jökulhlaup is esti- mated as 123 m3 s 1 while /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_006_tt.pdf

• 29. Rockslide in Askja, July 21 2014 - Preliminary results of observations

  plume rise up above Askja at 23:27. The steam plume was created when the slide exposed shallow geothermal areas in the release area. In addition, a dust cloud created by the rock slide may have contributed to the plume. The release area of the rockslide is approximately 800 m wide and 350 m above the lake surface. It may have been a "rotational slide movement", which means that the failure surface /avalanches/articles/nr/2929

• 30. VI_2020_004

  ....................................................................................................................................... 9 Ágrip ......................................................................................................................................... 11 1 General introduction ........................................................................................................... 13 1.1 Main aim of the project /media/vedurstofan-utgafa-2020/VI_2020_004.pdf