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Results:

• 61. norsem_schmidt

  will occasionally have to deal with spurious events. At SNSN we are therefore investigating the feasibility to construct an event verifier. The basic idea is to emulate the decision made by a seismologist viewing a section of recorded traces, sorted by epicentral distance, and expecting to see direct P-phase arrivals on most traces out to the most distant phase pick. Here we will report /media/norsem/norsem_schmidt.pdf

• 62. VI_2015_009

  by rescaling a dimensionless regional flood frequency distribution or growth curve, qR(D;T ), com- mon to all sites of the homogeneous region, with the so-called index flood, µi(D), of the target site: bQi(D;T ) = µi(D)qR(D;T ); (1) where bQi(D;T ) is the estimated flood quantile, i.e. the T -year flood peak discharge averaged over duration D, at site i. The regional growth curve, qR(D;T /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_009.pdf

• 63. VI_2009_013

  ...................................... 18  Figure 7. Temporal/spatial evolution of seismicity between 1996 and 2007. .................. 19  Figure 8. Temporal/spatial evolution during the latter intrusion swarm and until 2006. . 19  Figure 9. Mechanisms in selected depth intervals for the three main swarms. ................ 21  Figure 10. Distribution of P- and T-axis for events /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_013.pdf

• 64. programme2---PhD-Workshop-preceding-Adaptation-Research-Conference

  inty in decision making linking pluriform uncertainty combining certified and tacit knowledge Tommy Chan Mich el Laiho Patrick Driscoll Kare Lundgren Hector Guin a Barrientos Eivind Junker Jussi Ylhäisi Athanasios Votsis Karoliina Pilli-Sihvola Yuang Zheng Väi ö Nurmi Jiao Xi nj Wejs a p p l i c a n t n o . a b s t r a c t n o . n a m e c o u n t r y d i s c i p l i n e ( M S c . ) 1 3 /media/loftslag/programme2---PhD-Workshop-preceding-Adaptation-Research-Conference.pdf

• 65. 2010_005_

  which are significantly lower com- pared with similar beginning and end years. Consequently, for the 2004–50 period, the average RCM warming rates of 0.29 K per decade over the ocean, and 0.35 K per decade over the land are somewhat larger than for the reduced IPCC ensemble mean. Additionally, the tabulated values of SAT differences between the 1961–90 control period and either the 2021–50 /media/ces/2010_005_.pdf

• 66. Climate and Modeling Scenarios

  & Ólafsson, H. (2010). Validation of numerical simulations of precipitation in complex terrain at high temporal resolution. Hydrology Research, 41 (3-4), 164-170. Christensen, J.H., Boberg, F., Christensen, O.B. & Lucas-Picher, P. (2008), On the need for bias correction of regional climate change projections of temperature and precipitation, Geophys. Res. Lett., 35, L20709, doi:10.1029/2008GL035694 /ces/publications/nr/1680

• 67. Lettenmaier_Dennis_CES_2010pdf

  Dennis P. Lettenmaier Department of Civil and Environmental Engineering University of Washington Conference on Future Climate and Renewable Energy: Impacts, Risks, and Adaptation Oslo June, 1, 2010 Runoff projections and impacts on water resources Outline of this talk 1) Projected runoff changes over the next century – the global and continental picture 2) Downscaling to the regional /media/ces/Lettenmaier_Dennis_CES_2010pdf.pdf

• 68. VanderKeur_etal-2008-Uncertainty_IWRM-WARM

  Identification of Major Sources of Uncertainty in Current IWRM Practice. Illustrated for the Rhine Basin P. van der Keur & H. J. Henriksen & J. C. Refsgaard & M. Brugnach & C. Pahl-Wostl & A. Dewulf & H. Buiteveld Received: 13 December 2006 / Accepted: 10 January 2008 # Springer Science + Business Media B.V. 2008 Abstract Integrated Water Resources Management (IWRM) can be viewed as a complex /media/loftslag/VanderKeur_etal-2008-Uncertainty_IWRM-WARM.pdf

• 69. Kok_and_Veldkamp_editorial_ES-2011-4160

  Tengö, D. Timmer, and M. Zurek. 2007. Linking futures across scales: a dialog on multiscale scenarios. Ecology and Society 12(1): 17. [online] URL: http://www.ecolog yandsociety.org/vol12/iss1/art17/. Borgatti, S. P., and P. C. Foster. 2003. The network paradigm in organizational research: a review and typology. Journal of Management 29(6):991-1013. Brenner, N. 2001. The limits to scale /media/loftslag/Kok_and_Veldkamp_editorial_ES-2011-4160.pdf

• 70. Cradden_Lucy_CES_2010

  Capacity (A) F r e q u e n c y control future +0.4std dev (as % of mean) -0.68max -8.32min -1.74mean % change June 2010 15 Time series 450 500 550 600 650 700 Hour C a p a c i t y ( A ) Typical year of control period Seasonal average rating Calculated capacity 450 500 550 600 650 700 Hour C a p a c i t y ( A ) Typical year under future scenario Calculated capacity Seasonal average /media/ces/Cradden_Lucy_CES_2010.pdf