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• 11. VI_2020_005

  2000-3000 years with variations of 25 cm at most over timescales of several centuries. The few pre-1900 tide gauge records, evidence from paleo coastal sediments and reconstructed mean sea levels modelled using combined tide gauge data and satellite altimetry suggest an acceleration in global mean sea level rise in the late 19th and early 20th century (figure 4) (Church, Clark, et al., 2013 /media/vedurstofan-utgafa-2020/VI_2020_005.pdf

• 12. VI_2020_004

  49 Probabilistic hazard map for a load ≥1000 kg/m2 (Öræfajökull) ............................ 78 Figure 50 Seasonal analysis for 1 kg/m2 (~1mm) tephra ground load (Öræfajökull). ............ 79 Figure 51 Seasonal analysis for 10 kg/m2 (~1 cm) tephra ground load (Öræfajökull). ........... 80 Figure 52 Impact map for roads in case of an eruption like 1362 at Öræfajökull ................... 81 /media/vedurstofan-utgafa-2020/VI_2020_004.pdf

• 13. Bardarbunga_kafli20140825

  characteristics: Type of products: Airborne tephra, water transported tephra Volcanic Explosivity Index Max: VEI 4; most freq: VEI 3-4; min: VEI 0 Column heights: No information Duration of eruptions: Weeks to months Bulk volume tephra (km3): Max: no information, aver: 0.1, min: no information Fallout beyond 1000 km: No information Tephra <63µm at 30 km No information Bulk volume lava /media/jar/Bardarbunga_kafli20140825.pdf

• 14. VI_2015_009

  (m³/s) R ef . (m ³/s ) µ(D)=(θ0) + (θ1)(AWm) Rel. RMSE= 0.79 NS= 0.73 MAE= 86 l l l l l l l ll l 0 1000 2000 0 100 0 200 0 300 0 Pred. (m³/s) R ef . (m ³/s ) µ(D)=(θ0) + (θ1)(AWm Z) Rel. RMSE= 1.3 NS= −0.84 MAE= 191 Figure II.2. As Fig II-1 but considering a linear relationship: dµ(D) = q0 + q1V . Models 13–24. 30 /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_009.pdf

• 15. Alam_Ashraful_CES_2010

  growth Carbon dioxide concentration at th t h Regeneration distribution, growth rate of different species Different tree e a mosp ere Mortality 10 Input data  Finnish NFI data • total 2816 permanent sample plots for the whole of Finland (south: 1855; north: 961)  FMI - Climatic data • Current climate (1971-2000) • Changing climate during 2010-2099 (2010-2039; 2040-2069; 2070-2099) A2 /media/ces/Alam_Ashraful_CES_2010.pdf

• 16. VI_2009_006_tt

  that is lost from the main river course as further discussed in the main text. from the eastern cauldron are normally larger. They most often rise in one to two days reaching maximum discharge in excess of 1000 m3 s 1. Maximum discharge of nearly 2000 m3 s 1 has been measured. This discharge peak, which is much higher than the normal discharge of Skaftá, lasts for three to four days (Zóphóníasson /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_006_tt.pdf

• 17. VI_2016_006_rs

  wide and 1000 m long shelf called Þófi, terminating at 80–100 m a.s.l., see Map 4. The inclination of the shelf is 15 on average. The surface of Þófi is covered with unconsolidated glacial till and landslide deposits and marked with five gullies. The brook called Þófalækur near the middle of the shelf divides it into an inner and outer part. On the outermost part of the shelf, there is a small /media/vedurstofan-utgafa-2016/VI_2016_006_rs.pdf

• 18. Group3-Road-scenarios

  in five-year basis  Current state of the road network affects the possible decisions to be made at the moment Political adaptation Management structures have to be more flexible and ready to apply adaptive management Technological adaptation 0 1000 2000 3000 4000 5000 6000 1985199019952000200520102015202020252030 vans (mln. tonkm) lorries (mln. tonkm) 0 10000 20000 30000 /media/loftslag/Group3-Road-scenarios.pdf

• 19. Refsgaard_etal-2007-Uncertainty-EMS

  and possibly the stake- holders at different phases of the modelling project. Many QA guidelines exist such as Middlemis (2000) and Van Waveren et al. (1999). The HarmoniQuA project (Schol- ten et al., 2007; Refsgaard et al., 2005a) has developed a com- prehensive set of QA guidelines for multiple modelling domains combined with a supporting software tool, MoST (downloadable via http /media/loftslag/Refsgaard_etal-2007-Uncertainty-EMS.pdf

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

  point is the seminal paper by Ostrom et al. (1961), which introduced the concept of a “polycentric political system,” now more frequently referred to as polycentricity (McGinnis 2000). The basic idea is that any group of individuals facing collective problems should be able to address that problem in whatever way they best see fit. To do so, they might work through the existing system of public /media/loftslag/Public-Choice-2012---McGuiness-and-Walker---Foundations-of-the-Ostrom-workshop---institutional-analysis,-polycentricity,-and-self-governance-of-the-commons.pdf