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• 21. VI_2020_008

  Figure 8. Stations ranked according to their average CC for the 20 highest rainfall daily events. ................................................................................................................................................... 33 Figure 9. Ranked values of the 50 highest 24-hour accumulated precipitation events plotted against ranked values of the 50 highest daily precipitation /media/vedurstofan-utgafa-2020/VI_2020_008.pdf

• 22. CES_D2.4_solar_CMIP3

  %, for several months less than 2%. The good accordance encourages utilization of the models to construct future pro- jections. Admittedly, there is quite a large scatter among the various models, and conse- quently one is more justified to base the projections on the entire ensemble of the models rather than on any individual model. 2 ESTABLISHMENT OF THE PROJECTIONS The output of the model simulations /media/ces/CES_D2.4_solar_CMIP3.pdf

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

  hedged against small climate changes. Additionally, climate projec- tions were not considered credible (12, 14). Recent developments have led us to the opinion that the time has come to move beyond the wait-and-see approach. Pro- jections of runoff changes are bolstered by the recently demonstrated retrodictive skill of cli- mate models. The global pattern of observed annual streamflow trends /media/loftslag/Milly_etal-2008-Stationarity-dead-Science.pdf

• 24. 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

• 25. 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/

• 26. 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

• 27. 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

• 28. Perrels-CBA

  enhanced weather effects on road infrastructure • traffic safety • road maintenance • traffic capacity • Assessing flood risks in cities • TOLERATE: From climate modeling to appraisal of counter measures • IRTORISKI: Extended event-tree analysis Next pages (EWENT) 26.8.2011Adriaan Perrels/IL 26 Road capacity effects of weather & CC Changes in the supply curve caused by extreme weather conditions /media/loftslag/Perrels-CBA.pdf

• 29. 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

• 30. 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