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• 11. Climate Report

  fields.The glacial retreat has led to significant changes in hydrological conditions as the course of glacial rivers has been altered, new pro-glacial lakes have been formed, while existing ones have become more extensive or, in some cases, dried up. In 2009, the river Skeiðará altered its course and joined with the river Gígjukvísl, leaving an 880 m long bridge running over mostly dry riverbed /climatology/iceland/climate-report

• 12. Climate Report

  fields.The glacial retreat has led to significant changes in hydrological conditions as the course of glacial rivers has been altered, new pro-glacial lakes have been formed, while existing ones have become more extensive or, in some cases, dried up. In 2009, the river Skeiðará altered its course and joined with the river Gígjukvísl, leaving an 880 m long bridge running over mostly dry riverbed /climatology/iceland/climate-report/

• 13. VED_AnnualReport-2013_screen

  in the field of volcanology have been employed to work on improving the infrastructure and services for volcano monitoring. We have actively participated in international research projects in collaboration with the Univer- sity of Iceland, the Icelandic Civil Protection Agency and several Icelandic companies. We have received considerable international funding for these pro- jects. As part /media/vedurstofan/utgafa/arsskyrslur/VED_AnnualReport-2013_screen.pdf

• 14. Paper-Olafur-Rognvaldsson_91

  of such an approach is that it is relatively inexpensive in terms of computer resources used for simulations of the atmospheric flow at relatively high spatial and temporal resolutions. As resolution is increased, pro- cesses governed by the interaction of the large scale flow and topography be- come better resolved by the models. One drawback of this approach which is not present in global /media/ces/Paper-Olafur-Rognvaldsson_91.pdf

• 15. Keranen_Jaana_CES_2010

  tance ◊ energy losses hot w e ather decre ase s the lifetim e of tra nsform ers increas ing w ater capa city V ery like ly, the pro bability tha t the next decad e is w arm er is 90%. Phe nom ena 1.1 - higher te m peratures, espe cially during winter Sc en ario 1. war mer clim ate Conseque nce categ ory acc ording to own ra nking Lik elihood according to own rank in g Th e op /media/ces/Keranen_Jaana_CES_2010.pdf

• 16. Group4

  is that the future transport system will have to adapt. In 2012, transport planners adopted a pro-active approach to the future, seeking to embrace uncertainty to enable society to move toward a low-impact mobility system. “What happens tomorrow depends less on prevailing trends and more on individual and collective decisions taken in the face of these trends” (Godet, 2005, p. 9 /media/loftslag/Group4.pdf

• 17. IMO_AnnualReport2014

  and surveillance of earth, water and air showed its strength and was in particular very helpful in the pro vision of gas-distribution forecasts for the public. All divi- sions of IMO contributed to the e?ort which was carried out in close co-operation with the University of Iceland and the Civil Protection in Iceland, with great backing from our ministry and the government. It is not enough /media/vedurstofan/utgafa/skyrslur/2015/IMO_AnnualReport2014.pdf

• 18. IPPC-2007-ar4_syr

  2000 to 2100 in the absence of additional climate policies Global GHG emissions (Gt C O 2 -eq / yr ) post-SRES (max) post-SRES (min) Purchasing Power Parity, PPP) does not appreciably affect the pro- jected emissions, when used consistently.11 The differences, if any, are small compared to the uncertainties caused by assumptions on other parameters in the scenarios, e.g. technological change /media/loftslag/IPPC-2007-ar4_syr.pdf

• 19. Paper-Olafur-Rognvaldsson_92

  can, to some extent, be explained by the fact that precipitation falls on porous post- glacial lava in some areas and flows through groundwater aquifers to the ocean without participating in surface runoff. Earlier research (Tómasson, 1982) have estimated this flow to be on the order of 33–62mm y−1. This comparison of total accumulated scaled and non-scaled precipitation indicates that MM5 pro /media/ces/Paper-Olafur-Rognvaldsson_92.pdf

• 20. Refsgaard_etal-2007-Uncertainty-EMS

  to arrive at a robust deci- sion. As with the other steps, the quality of the results needs to be assessed through internal and external reviews that also provide platforms for dialogues between water man- ager, modeller, reviewer and, often, stakeholders/public. Fig. 1 shows the key actors in the water management pro- cess and the above five steps in the modelling process. The interactions between /media/loftslag/Refsgaard_etal-2007-Uncertainty-EMS.pdf