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Results:

• 31. AnneFleig_May2010_CES

  E l b e i n D r e s d e n , A p r i l 2 0 0 7 CES conference, Oslo, Norway, 31 May - 2 June 2010 Typical features • develop slowly, • become severe when they cover a large region and persist for an extended period. E l b e i n D r e s d e n , A p r i l 2 0 0 7 ( s p i e g e l . d e ) Anne K. Fleig et al. “Regional hydrological droughts and weather types in north /media/ces/AnneFleig_May2010_CES.pdf

• 32. Hare-2011-ParticipatoryModelling

  25 26 27 28 29 30 31 32 33 34 35 36 37 38 39 40 41 42 43 44 45 46 47 48 49 50 51 52 53 54 55 56 57 Fr am ew o rk Cr ite ria u se d M ain pu rp o se o fframewor k Participator y m od ell in g purpos e Particip ator y structur e Contro lo f
  ow of in for m a tio n betwee n stakeholder s Timin g of event s Participatio n mod e Mo de l typ e Participator y m et ho ds use d Actor sinvolve d (at eac h /media/loftslag/Hare-2011-ParticipatoryModelling.pdf

• 33. Lawrence_Deborah_CES_2010

  
  
                                !  !   0 20 40 60 80 100 120 140 jan feb mar apr mai jun jul aug sep okt nov des m m / m å n e d 55550 Hafslo 60 80 100 120 140 jan feb ar apr ai j j l t m m / m å n e d 55550 Hafslo 54130 Lærdal Ensemble approach for probabilistic hydrological projections Catchment /media/ces/Lawrence_Deborah_CES_2010.pdf

• 34. Guidelines2-for-rapporteurs

  ). This can be helpful with respect to finding a common structure in presenting as well in session reporting (for which angles mentioned in the opening session statements of the Workshop participants can provide checkpoints).” Session rapporteur allocation M o n d a y 2 9 . 8 Y u a n g Z h e n g A t h a n a s i o s V o t s i s E i v i n d J u n k e r M i c h a e l L a i h o H e c to r /media/loftslag/Guidelines2-for-rapporteurs.pdf

• 35. VI_2016_006_rs

  that occur in Botnabrún or at the rim of Þófinn are debris slides. The size of the slides varies depending on the source area. C Mudslides or mudflows occur where there is an abundance of soils. They normally occur in areas where the vegetation cover has been breached. Common occurrences in Seyðis- fjörður are in the mountain Bjólfur and in the valley west of the settlement. D Rockfalls are a common /media/vedurstofan-utgafa-2016/VI_2016_006_rs.pdf

• 36. ces_risk_flyer

  and distribution network are all identified a section at a time. In some cases, however, it might be more valuable to focus only on a certain part of functional model. Fig.1. Functional Model. The results of the risk analysis are represented visually in a fourfold table. (Fig.2) The main idea of the table is to provide a readily interpretable overview of h hi hli h d i k d i i i l i Having already been /media/ces/ces_risk_flyer.pdf

• 37. Hydropower, Hydrology

  Hydrological Sciences Journal, 53, 100-111. Kriauciuniené, J., Meilutyté-Barauskiené, D., Rimkus, E., Kays, J., Vincevicius, A. (2008). Climate change impact on hydrological processes in Lithuanian Nemunas river basin. Baltica, Vol. 21 (1-2), pp. 1-61. Vilnius. ISSN 3067-3064. Lawrence, D., Haddeland, I. (2010). Uncertainty in hydrological modelling of climate change impacts in four Norwegian /ces/publications/nr/1938

• 38. TietavainenHanna_CES_2010

  versa • Very large range within the simulations • Larger number of observation stations in the study area leads to • better compatibility between different observational data sets • smaller bias in the model simulations CES Conference, Oslo 31.5.-2.6.2010 References • Haylock, M. R., Hofstra, N., Klein Tank, A. M. G., Klok, E. J., Jones, P. D. and New, M. 2008. A European daily high-resolution /media/ces/TietavainenHanna_CES_2010.pdf

• 39. Case_B___Road_transport_operation_and_infrastructure_planning

  on the Shifts of climatic zones from cooler or wetter to warmer or drier (a) 1971-2000 (b) 2010-39 A1B observational data set (0.25º grid) from Haylock et al. (2008) (b-d) Based on CMIP3 GCM runs for A1B & the delta-change method (c) 2040-69 A1B (d) 2070-99 A1B Jylhä et al. (2010) Uncertainties in climate change schematically Observed climate Future climate Natural /media/loftslag/Case_B___Road_transport_operation_and_infrastructure_planning.pdf

• 40. Climatological data

  /climatology/data/