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  • 21. Bárðarbunga 2014 - August events

    do not allow overflight at this time. The opportunity to fly over the area will be assessed later today. From the Icelandic Met Office: The Aviation Colour Code for Bárðarbunga is at ‘red' and the code for Askja at ‘yellow'. 31 August 2014 08:40 - Eruption in Holuhraun observed 05:15 Observation from scientists in the field (05:15): It appears that the eruptive fissure is longer than /earthquakes-and-volcanism/articles/nr/3000/
  • 22. Group4

    ) intelligent roads (ITS). Temporal scale: The rationale for choosing 2050 as a starting point for the backcast is twofold: 1) 2100 is too far into the future, resulting in high levels of epistemic and ontologic uncertainty (time, values, knowledge, etc.), 2) road transportation investment lifetimes typically encompass 30-40 year spans. 3.0 Scenarios 3.1 Background Brief: Prior to initiating /media/loftslag/Group4.pdf
  • 23. NONAM_1st_workshop_summary_v3

    initiates and manages the adaptation planning and assessment process is working on the basis of a vision (e.g. objectives regarding function and quality of road infrastructure in 40 years10). Q3 / Q4 Also between questions 3 and 4 considerable overlap and interaction exists. The scanning, analysis and scenario outline(s) implied by questions 3 and 4 should be guided by a strategic view /media/vedurstofan/NONAM_1st_workshop_summary_v3.pdf
  • 24. VI_2020_005

    . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 25 2.4.1 Sea level projections for Scandinavia, the UK and Iceland . . . . . . . . . 29 2.5 Extreme sea level . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 34 2.5.1 Extreme sea levels in Scandinavia, the UK and Iceland . . . . . . . . . . . 36 3 Coastal flooding risk analysis . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 40 3.1 Coastal flooding risk /media/vedurstofan-utgafa-2020/VI_2020_005.pdf
  • 25. 2010_016

    and the groundwater module. The coupling between both modules was done by a net boundary flux between the unsaturated zone and the groundwater (Schulla & Jasper, 2007). Information on land use, soil type, elevation and other general properties of the watershed are given in static distributed grids while a number of parameters describing specific processes are adjusted to the properties of each /media/ces/2010_016.pdf
  • 26. 2010_017

    of radiation are added to a classic degree-day model. For infiltration, a methodology of Peschke, based on the approach of Green and Ampt, was used. To calculate the fluxes within the unsaturated soil zone, the Richards equation was used. The groundwater table was modelled in both the unsaturated zone module and the groundwater module. The coupling between both modules was done by a net /media/ces/2010_017.pdf
  • 27. 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
  • 28. VI_2022_006_extreme

    and documented in Björnsson et al. (2018) and Crochet et al. (2007). The study, based on the previous research of Jónas Elíasson (Elíasson, 2000; Elíasson et al., 2009) also presented intensity-duration-frequency curves for over 40 locations in Iceland. These curves describe the relationship between rainfall intensity, duration, and return periods, making them useful for flood warnings /media/vedurstofan-utgafa-2022/VI_2022_006_extreme.pdf
  • 29. Journal_of_Hydrology_Veijalainen_etal

    ) in Europe yield contradictory results on the changes in floods in many parts of Europe, including Finland. Dankers and Feyen (2008) reported a considerable reduction of 10–40% in 100-year discharges in Finland, much of northern Sweden and north-western Russia by the end of the century due to decrease in snow accumulation; however Lehner et al. (2006) evaluated that the 100-year floods in the same areas /media/ces/Journal_of_Hydrology_Veijalainen_etal.pdf
  • 30. Outline_for_the_case_Road_maintenance_in_a_changing_climate

    NONAM PhD course – Adaptive management in relation to climate change – Copenhagen 21-26/8/2011 …………………………………………………………………………………………………………………………………………………………………… 1 Outline for the case Road maintenance in a changing climate Introduction Roads and transport systems are vulnerable to climate change impacts (VTT 2011; Koetse and Rietveld, 2009; Regmi & Hanaoka, 2011; Road ERA-net 2009 & 2010 /media/loftslag/Outline_for_the_case_Road_maintenance_in_a_changing_climate.pdf

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