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• 31. What is Bárðarbunga?

  in northwestern Vatnajökull ice cap and therefore covered with ice. The enormous size and nature of Bárðarbunga was not fully recognized until it was observed in 1973 on an image from a satellite, 800 km above Earth (see below). A caldera in the volcano's crown, 11 km long on the longer side, is covered with approximately 850 m thick glacial ice. Eruptions related to the central volcano can occur /about-imo/news/nr/2968

• 32. Tornado_Impacts_-_FMI_Presentation

  -Scale Category R a t i o N i g h t t o O t h e r T i m e s Fatalities Injuries Casualties and Month 80 100 120 140 I n d e x V a l u e Fatalities 0 20 40 60 Jan ua ry Feb rua ry Ma rch Apr il Ma y Jun e Jul y Au gus t Sep tem ber Oct obe r No ve mb er De ce mb er I n d e x V a l u e Injuries Casualties: Weekends vs. Weekdays 140.0739064 107.8746803 120 140 160 0 20 40 60 80 100 Index /media/loftslag/Tornado_Impacts_-_FMI_Presentation.pdf

• 33. ces_geus_paakitsoq_full_report

  Observational Data Data from four weather stations is used to validate the RCMs : Illulisat and Station 437 are coastal stations being operated by the Danish Meteorological Institute (DMI) and Asiaq, 1 Figure 1: Overview of the study site. The location of the four weather stations is indicated and in the background mean annual accumu- lation distribution (1980–2006) according to Burgess et al. (2010 /media/ces/ces_geus_paakitsoq_full_report.pdf

• 34. VI_2015_006

  depth is determined by placing 50 cm of snow water equivalent (SWE) (or 500 kg m 2 of snow) on top of the permanent snow regions, as defined by the model glacier mask. The “snow on glaciers” runs are used for most of the analysis presented here, whereas the “no snow” runs are used in the last section, to determine the impact of glaciers on the thermodynamic properties of the boundary-layer /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_006.pdf

• 35. VED_AnnualReport-2013_screen

  the accumulation and preservation of data and knowledge regarding the long-term de- velopment of natural processes such as climate, glacier changes, crustal movements and other environmental matters that fall under IMO‘s responsibility, including trans-boundary air pollu- tion • Undertaking of risk assessments for natural haz- ards at the request of the government • Deciding on evacuation plans /media/vedurstofan/utgafa/arsskyrslur/VED_AnnualReport-2013_screen.pdf

• 36. Lettenmaier_Dennis_CES_2010pdf

  21 15% 55 26 5% 5546% of world's GDP 2233% of world’s population 10%0%Runoff decreases by Continental U.S. and Alaska All scenarios Top 200 basins Precipitation change per degree T change vs evaporation change per degree T All scenarios Top 200 basins Precipitation change per degree T change vs runoff change per degree T A1B scenario Top 200 basins Precipitation change per Degree T change /media/ces/Lettenmaier_Dennis_CES_2010pdf.pdf

• 37. 2010_016

  /media/ces/2010_016.pdf

• 38. Staff members

  Staff members Marcel de Vries Job title: Meteorologist Email: Marcel (hjá) vedur.is /about-imo/employees/persona/314/fyrirtaeki/2

• 39. Kok_1-scenarios-lecture-1

  Columbia University Press. O'Neill, R.V., D. DeAngelis, J. Waide and T. F. H. Allen. 1986. A hierarchical concept of ecosystems. Princeton University Press. Log time (years) Log space (meters) Leaf Crown days Tree Stand Forest Branch Landscape months year century decade cm m 100m 100km Examples of functional scales Log time (years /media/loftslag/Kok_1-scenarios-lecture-1.pdf

• 40. Milly_etal-2008-Stationarity-dead-Science

  ), S. Solomon et al., Eds. (Cambridge Univ. Press, New York, 2007), pp. 1–18; www.ipcc.ch/press/index.htm. 5. IPCC, in Climate Change 2007: Climate Change Impacts, Adaptation and Vulnerability, Contribution of WG2 to AR4, M. L. Parry et al., Eds. (Cambridge Univ. Press, New York, 2007), pp. 1–16. 6. I. M. Held, B. J. Soden, J. Clim. 19, 5686 (2006). 7. T. P. Barnett, J. C. Adam, D. P. Lettenmaier /media/loftslag/Milly_etal-2008-Stationarity-dead-Science.pdf