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Results:

• 41. VI_2014_001

  WaSiM-ETH (Schulla and Jasper, 2007; Atladóttir et al., 2011; Þórarinsdóttir, 2012) was calibrated on 4 gauged catchments (vhm19, vhm38, vhm51 and vhm52). A semi-automatic multi-objective optimization based on the analysis of discharge information was used to assist in the selection of best model parameters for each catchment (Crochet, 2012d). The model was then used to simulate daily streamflow /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_001.pdf

• 42. VI_2014_006

  in a historical archive, according to certain atmospheric variables and some analogy criteria. Then, the dates of the N best analogues, i.e. the N closest matches to the target situation are extracted and sorted, and a meteorological ensemble pre- diction is formed, with the precipitation and temperature sample, observed on these days (N members): P(i; t) = P(ui) (1) T2m(i; t) = T2m(ui) (2) where t = t0 /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_006.pdf

• 43. Henriksen-AM

  greater demands on stakeholders, because they must monitor decisions and the decision-making process over the time of the life of the project – Because decisions are always tentative, it may also increase or extend controversy and conflict – It may require trading the anticipated best outcome in the short term for long-term learning and improvement Discussion (2) When is adaptive management /media/loftslag/Henriksen-AM.pdf

• 44. Kok_and_Veldkamp_editorial_ES-2011-4160

  agreement on use of terminology. Third, all scoping papers stress that there is no silver bullet solution, with a different view on both scale and governance being appropriate depending on the specific case. Buizer et al. (2011) are strongest on this view by presenting and discussing a framework. Termeer et al. (2010) confirm that there is no best governance approach, drawing an analogue /media/loftslag/Kok_and_Veldkamp_editorial_ES-2011-4160.pdf

• 45. IPPC-2007-ar4_syr

  the respective WG reports. Unless otherwise stated, numerical ranges given in square brackets in this report indicate 90% uncertainty intervals (i.e. there is an estimated 5% likelihood that the value could be above the range given in square brackets and 5% likelihood that the value could be below that range). Uncertainty intervals are not necessarily symmetric around the best estimate. 1 Observed changes /media/loftslag/IPPC-2007-ar4_syr.pdf

• 46. Refsgaard_etal-2007-Uncertainty-EMS

  in what terms uncertainty can best be scribed. The vertical axis identifies the location or source external economic, environmental, political, social and technological circumstances that form the context of the problem.  Input uncertainty in terms of external driving forces (within or outside the control of the water manager) and system data that drive the model such as land use maps, Certainty /media/loftslag/Refsgaard_etal-2007-Uncertainty-EMS.pdf

• 47. glacier_mass_balance_poster

  point measurements and surface profiles surveyed by kinematic GPS, and further corrected with airborne radar altimetry profiles from October 2004. Autumn aerial photographs: 20 m contour lines digitized using the best available aerial photographs from: 1979 for Torfajökull, 1980 for Tindfjallajökull and 1984 for Eyjafjallajökull. Regular 40x40 m DEMs created by a kriging method. Maps of annual /media/ces/glacier_mass_balance_poster.pdf

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

  with expectations of predictability, indiscrimination etc. But is this compatible with the best strategies for handling uncertainty? What if new knowledge prescribes a decision contrary to one that has already been made? Should the need for legal certainty and predictability prevail? 2) What is the best way to distribute roles and responsibilities between scientists, politicians /media/loftslag/programme2---PhD-Workshop-preceding-Adaptation-Research-Conference.pdf

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

  are developing plans for their local communities to adapt to climate change will not be best served by a model whose horizontal grid has divisions measured in hundreds of kilome- ters. To facilitate information transfer in both directions between climate science and water management, the climate models need to include more explicit and faithful representa- tion of surface- and ground-water processes /media/loftslag/Milly_etal-2008-Stationarity-dead-Science.pdf

• 50. 2010_012rs

  to a subset of near-by events from the event library via cross-correlation of P and S waveforms. The relative times are inverted for best location, resulting in a high-precision automatic location for the new event available within minutes. As more waveforms arrive, the process is repeated to improve the location. The location accuracy that can be achieved is from tens of meters to a few hundred meters /media/vedurstofan/utgafa/skyrslur/2010/2010_012rs.pdf