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Results:

• 61. Gode_Jenny_CES_2010

  positions: from fuel purchase, plant engineering and up to strategic level square4 Own experience and thoughts Viewpoints presented in this presentation do not claim to be general opinions! Stakeholder Relevance of the CES Project Jenny Gode, 31 May 2010 Communication CES Relevance Improvements Not widely known? Stronger focus on mitigation Uncertain Long-term Many scenarios Policy instru /media/ces/Gode_Jenny_CES_2010.pdf

• 62. Kriauciuniene_Jurate_CES_2010

  boxshadowdwnboxshadowdwn Geographical and hydrometeorological description of Baltic regions boxshadowdwnboxshadowdwn Data and methods boxshadowdwnboxshadowdwn Regional series - Temperature, precipitation, runoff boxshadowdwnboxshadowdwn Conclusions Purpose of the study To do comparison of the Baltic regional series of temperature, precipitation and river runoff for period of last years (1991 /media/ces/Kriauciuniene_Jurate_CES_2010.pdf

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

  calculations. When including explicit basal sliding in the model, a flow parameter that characterizes stiffer ice is required (e.g. Aðal- geirsdóttir, 2000). The available data do not allow the de- termination of the relative contributions of deformation and sliding velocities for the glacier. Many combinations of A and C will produce a satisfactory fit to observations. A se- ries of model runs /media/ces/Adalgeirsdottir-etal-tc-5-961-2011.pdf

• 64. ces_geus_paakitsoq_full_report

  (2007), Mass balance of the Amitsulôq ice cap, West Greenland, in Glacier Mass Balance Changes and Meltwater 15 Discharge (selected papers from sessions at the IAHS Assembly in Foz do Iguaçu, Brazil, 2005), no. 318 in IAHS Publication, pp. 107–115, IAHS Press: Wallingford. Burgess, E., R. Forster, J. Box, E. Mosley-Thompson, D. Bromwich, R. Bales, and L. Smith (2010), A spatially calibrated model /media/ces/ces_geus_paakitsoq_full_report.pdf

• 65. VI_2009_012

  A is similar to the present velocity-attenuation formula used at IMO to estimate local magnitude ML, which is given by: 8.4)(log1.2)(maxlog 1010 −+⋅−= Mrvelocity Date (yyyymmdd) Origin time (hhmmss.ms) Latitude (˚N) Longitude (˚W) MLw (M0 SIL) Mw (M0SIL) MLw (M0CMT) Mw (M0CMT) 20000621 005146.985 63.973 20.711 6.6*) 6.6 6.5 6.4 20000617 154040.998 63.973 20.367 6.4*) 6.2 6.5 6.5 /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_012.pdf

• 66. Eriksson_2-Acceptability-of-policy

  for behavioural responses to policy • Psychological models of behaviour change (e.g., TPB) Ajzen & Fishbein (1991) Subjective norm Specific attitudes Perceived behavioural control Intention Behaviour Normative beliefs Behavioural beliefs Control beliefs P O L I C Y (3) Factors important for behavioural responses to policy cont. • Cost-minimization principle (Loukopoulos et al. 2006) • Barriers /media/loftslag/Eriksson_2-Acceptability-of-policy.pdf

• 67. Daniell_etal-2010

  Copyright © 2010 by the author(s). Published here under license by the Resilience Alliance. Moellenkamp, S., M. Lamers, C. Huesmann, S. Rotter, C. Pahl-Wostl, K. Speil, and W. Pohl. 2010. Informal participatory platforms for adaptive management. insights into niche-finding, collaborative design and outcomes from a participatory process in the rhine basin. Ecology and Society 15(4): 41. [online /media/loftslag/Daniell_etal-2010.pdf

• 68. Refsgaard_2-uncertainty

  that there is something we do not know Total ignorance (=epistemic arrogance) • We do not know that there is something we do not know Statistical Uncertainty Scenario Uncertainty Regognized Ignorance Total ignorance Determinism Indeterminacy Qualitative Uncertainty Sources of uncertainty in Water Resources Management Data • physical, chemical, biological, etc. • scale problems (temporal and spatial /media/loftslag/Refsgaard_2-uncertainty.pdf

• 69. Journal_of_Hydrology_Veijalainen_etal

  24 July 2010 This manuscript was handled by K. Georgakakos, Editor-in-Chief, with the assistance of Ercan Kahya, Associate Editor Keywords: Climate change Flood Hydrological modelling Flood inundation area Hydraulic modelling Finland s u m m a r y This paper provides a general overview of changes in flooding caused by climate change in Finland for the periods 2010–2039 and 2070–2099. Changes /media/ces/Journal_of_Hydrology_Veijalainen_etal.pdf

• 70. Gudmundsson-etal-2011-PR-7282-26519-1-PB

  was used as a reference map for co-registration and correction of the vertical offset of the other DEMs. The average specific mass balance was estimated from the mean elevation difference between glaciated areas of the DEMs. The glacier mass balance declined significantly between the two periods: from 0.2 to 0.2 m yr1 w. eq. during the earlier period (1980s through 1998) to 1.8 to 1.5 m yr1 w /media/ces/Gudmundsson-etal-2011-PR-7282-26519-1-PB.pdf