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Results:

• 41. 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

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

  were carried out to obtain the flow and sliding parameters for Hoffellsjökull that resulted in a good simulation of the observed 20th century evolution of the glacier geometry. The obtained values for the rate factor and the sliding parameter are A= 4.6× 10−15 s−1 kPa−3 and C = 10× 10−15 m a−1 Pa−3, respectively. The ice divide is kept at a fixed location in the model com- putations presented here /media/ces/Adalgeirsdottir-etal-tc-5-961-2011.pdf

• 43. vonKorff_etal-2010

  Copyright © 2010 by the author(s). Published here under license by the Resilience Alliance. Von Korff, Y., P. d'Aquino, K. A. Daniell, and R. Bijlsma. 2010. Designing participation processes for water management and beyond. Ecology and Society 15(3): 1. [online] URL: http://www. ecologyandsociety.org/vol15/iss3/art1/ Synthesis, part of a Special Feature on Implementing Participatory Water /media/loftslag/vonKorff_etal-2010.pdf

• 44. VI_2014_005

  in an overall cold bias, compared with station measurements. To test, whether this is due to the HARMONIE model core or the external surface scheme, biases of 2-m temperature from SURFEX are com- pared with biases of temperature projected from the lowest two model levels to 2 mAGL. It is found that the negative temperature biases are due to shallow inversion layers near the ground, which are introduced /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_005.pdf

• 45. Henriksen_Barlebo-2008-AWM_BBN-Journ_Env_Management

  improving management policies and practices by learning from the outcomes of implemented management strategies. Partici- patory integrated assessment is here a form of problem structuring for identification of gaps, ambiguity and multiple frames, confrontation, and integration of the most divergent views with respect to a given problem situation. Additional methods and tools that AM require com /media/loftslag/Henriksen_Barlebo-2008-AWM_BBN-Journ_Env_Management.pdf

• 46. Refsgaard_2-uncertainty

  - nitrate reduction in underground medium medium large large large Model technical uncertainty - numerical approximation small small medium small - bugs in software medium medium small SUM: Importance Type of uncertainty Error propagation Box 1 Error propagation rules using standard deviation (σ ) Addition and Subtraction: z = x + y + .. or z = x - y - .. ..)()( 22 ++= yxz σσσ /media/loftslag/Refsgaard_2-uncertainty.pdf

• 47. aerodrome_summaries_20140603

  14 0 1 2 3 8 12 15 0 1 2 3 8 12 16 0 1 2 4 8 12 17 0 1 2 4 8 12 18 0 1 2 4 8 12 19 0 1 2 4 8 13 20 0 1 2 4 8 13 21 0 2 3 5 9 13 22 1 2 3 5 9 13 23 1 2 3 4 9 13 MEAN 1 2 2 4 8 13 10 AE R OD R OM E CLIM A T OLOGICA L SUMMA R Y - T ABL E D AE R OD R OME :BIK F - KEFL A VÍ K /K efl avi k PERIO D O F RECORD :2001–201 0 L A TITUDE :6 3 59’06" N LONGITUDE :2 2 36’20" W ELE V A TIO N AB O V E MSL :5 2 /media/vedur/aerodrome_summaries_20140603.pdf

• 48. VI_2014_006

  the com- plexity of the hydrological processes through modelling, but its application is usually limited to the short-range. Although the results demonstrated a great potential for this method, its success- ful application in real-time will strongly depend on the quality and availability of streamflow observations, which can be poor or simply missing during periods of variable durations, e.g /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_006.pdf

• 49. Mid-Latitudes-Agenda1_nov2013EH

  polarity reversal from winter to summer in 2010 and its relation to extreme hot summer associated with polar jet, summer AO and blocking - Y Tachibana Group Discussion 10:30 – 11:00 Coffee Break 11:00 – 12:00 11:00 – 11:20 11:20 – 11:40 11:40 – 12:00 12:00 – 12:30 Potential Arctic / Mid-Latitude Linkages – Large Scale (Chair: Jim Overland) Large scale linkages between fall /media/loftslag/Mid-Latitudes-Agenda1_nov2013EH.pdf

• 50. CES_D2.4_task2_CMIP3_winds

  % 6,0 % 8,0 % 10,0 % 1 3 5 7 9 11 13 15 17 19 21 23 25 27 29 31 33 35 Fr eq ue nc y (% ) Geostrophic wind (m/s) September-April 1971-2000 2046-2065 -0,5 % -0,4 % -0,3 % -0,2 % -0,1 % 0,0 % 0,1 % 0,2 % 0,3 % 0,4 % 0,5 % 0,6 % 1 3 5 7 9 11 13 15 17 19 21 23 25 27 29 31 33 35 C ha ng e in % Wind class in m/s September-April change 46-71 Fig. 6. Top: 10-GCM mean frequency distributions of daily /media/ces/CES_D2.4_task2_CMIP3_winds.pdf