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• 21. Adalgeirsdottir-etal-tc-5-961-2011

  1Institute of Earth Sciences, University of Iceland, 101 Reykjavík, Iceland 2Danish Meteorological Institute, Lyngbyvej 100, 2100 Copenhagen, Denmark 3Icelandic Meteorological Office, Bústaðavegi 150, 105 Reykjavík, Iceland 4Department of Computer Science, University of Iceland, 107 Reykjavík, Iceland 5CNRS; Université de Toulouse, Laboratoire d’Etudes en Géophysique et Océanographie Spatiales (LEGOS); 14 /media/ces/Adalgeirsdottir-etal-tc-5-961-2011.pdf

• 22. Refsgaard_etal-2007-Uncertainty-EMS

  :// www.harmoniqua.org), be decomposed into five major steps (Fig. 1), which again are decomposed into 48 tasks (not de- tailed here). The contents of the five steps are:  STEP1 (model study plan). This step aims to agree on a Model Study Plan comprising answers to the questions: Why is modelling required for this particular model study? What is the overall modelling approach and which work should be carried /media/loftslag/Refsgaard_etal-2007-Uncertainty-EMS.pdf

• 23. Staff members

  Weather observer Service and Research Division Marcel de Vries Meteorologist Service /about-imo/employees/

• 24. CES_D2.4_VMGO

  size. References 1. Meehl, G.A., C. Covey, T. Delworth, M. Latif, B. McAvaney, J.F.B. Mitchell, R.J. Stouffer and K.E. Taylor, 2007: The WCRP CMIP3 Multimodel Dataset: A New Era in Climate Change Research, BAMS, 88, 1383-1394, DOI: 10.1175/BAMS-88-9-1383. 2. Naki �enovi � N., J. Alcamo, G. Davis, B. de Vries, J Fenhann, S. Gaffin, K. Gregory, A.Grübler, T.Y. Jung, T. Kram, E.L. La Rovere /media/ces/CES_D2.4_VMGO.pdf

• 25. ces_geus_paakitsoq_full_report

  perturbations is higher for the degree-day model used by Ahlstrøm et al. (2008a) than for an energy balance model as applied in the present study (e.g. Van de Wal, 1996). 8 Conclusions and Outlook A workflow to calculate future scenario surface mass balance for the Paakitsoq area has been presented. On the example of the present-day runs it was shown that RCM biases exhibit a large influence /media/ces/ces_geus_paakitsoq_full_report.pdf

• 26. Publications

  (1991-2004) and Langjökull (1996-2004) ice caps, Iceland. Presented at the European Geosciences Union, General Assembly, Vienna, Austria, Apr 24-29. [Poster] de Woul, M., & Hock, R. (2005). Static mass balance sensitivity of Arctic glaciers and ice caps using a degree-day approach. Annals of Glaciology, 42 , 217-224. de Woul, M., Hock, R., Braun, M., Thorsteinsson, T., Jóhannesson, T /climatology/research/ce/publications/

• 27. 2012-Refsgaard_etal-uncertainty_climate-change-adaptation-MITI343

  in ty N at ur e o f u n ce rta in ty Inp ut dat a Mo de l Co ntex t Multi pl e knowl edg e fra m es Ambi guit y Ep istemi c un certaint y (re du cib le) Aleator y u n ce rta in ty (ir red uc ibl e) Pa ramete r val ue s Mode l techni ca l as pe ct s Mo de l st ru ct ur e G re en ho us e ga s em iss io ns X X X X X X X X X X Socio -econo m ic scena rio s X X X X X X X X X XX X X X Fu tu re cl im /media/loftslag/2012-Refsgaard_etal-uncertainty_climate-change-adaptation-MITI343.pdf

• 28. glacier_mass_balance_poster

  750-1170 AAR of the warm year of 2004 - digitized using the October 2004 SPOT 5 HRS images Ice cap E: Eyjafjallajökull To: Torfajökull Ti: Tindfjallajökull AAR (%) 20-25 <5 0 Method References Berthier E., Arnaud Y., Baratoux D., Vincent C. and Rémy F. 2004. Recent rapid thinning of the "Mer de Glace" glacier derived from satellite optical images. Geophys. Res. Lett., 31, L17401, doi:10.1029 /media/ces/glacier_mass_balance_poster.pdf

• 29. 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

• 30. Journal_of_Hydrology_Veijalainen_etal

  Directive has been to produce flood extent or inundation maps, which are already carried out in 23 European countries (de Moel et al., 2009). In Nordic climatic conditions, where snow plays an important role in hydrology, climate change may either increase or decrease floods (Vehviläinen and Huttunen, 1997; Beldring et al., 2006). Floods could become more severe, since annual precipitation is ex- pected /media/ces/Journal_of_Hydrology_Veijalainen_etal.pdf