82 results were found for l 파생상품거래〔WWW-BYB-PW〕 파생상품매매 파생상품투자파생상품리딩㏯액토즈소프트 iRm.

Results:

• 61. Moellenkampetal_etal-2010

  supported by the majority of responses to one of the quantitative questions (to which 13 out of 20 participants responded on a five-point Likert scale—strongly agree, agree, neither agree or disagree, disagree, strongly disagree), where 11 respondents “agreed” that the activities in the workshop helped them to share their views and opinions with others, and the other two “neither agreed nor disagreed /media/loftslag/Moellenkampetal_etal-2010.pdf

• 62. vanRoosmalen_etal-2009-WRR_2007WR006760

  and Relative Changes When Comparing the A2 and B2 Scenarios to the Current Climatea Scenario Net Recharge Horizontal Boundary Outflow Drain Flow Base Flow Water Supply Irrigation Simulations Not Including Abstractions and Irrigation Current climate 550 23 279 252 A2 scenario + 67 (12%) + 1 (4%) + 56 (20%) + 13 (5%) B2 scenario + 113 (21%) + 1 (4%) + 92 (33%) + 22 (9%) Simulations Including Abstractions /media/loftslag/vanRoosmalen_etal-2009-WRR_2007WR006760.pdf

• 63. Hydropower, Hydrology

  S., Roald, L.A., Engen-Skaugen, T. Projected effects of climate change on the hydrology of Norway. Conference on Future Climate and Renewable Energy: Impacts, Risks and Adaptation, Oslo, 31 May - 2 June 2010, 80-81. Bergström, S. HUVA training course for the hydropower industry. Lecture on climate change and hydropower. Stockholm, December 2, 2010. Bergström, S. Lecture on climate /ces/publications/nr/1938

• 64. Kjellstrom_Erik_CES_2010

  ANN−10 −5 0 5 10 15 20 delta w (% ) 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17C h a n g e i n g e o s t r o p h i c w i n d s p e e d ( % ) Change in wind over the Baltic Sea in 70 years time at the time of CO2-doubling Chen and Aschberger, 2006 17 CM IP G CM s A need for regional ensemble simulations head2right Changes are uncertain head2right Size and sometimes even sign /media/ces/Kjellstrom_Erik_CES_2010.pdf

• 65. Linnet_Ulfar_CES_2010

  2015, 2025, 2035 and 2050 North (Blanda) East (Karahnjukar) South (Thorisvatn) Change in average inflow to the main storage reservoirs Watershed A v e r a g e i n f l o w [ m 3 / s ] 0 2 0 4 0 6 0 8 0 1 0 0 1 2 0 Last 50 years Last 20 years Last 15 years Last 10 years Last 5 years Temperature corrected Transformation of climate measurements •Change in temperature • 0.75 °C/100y 1950-1975 • 1.55 /media/ces/Linnet_Ulfar_CES_2010.pdf

• 66. RaisanenJouni_CES_2010

  not representative of present or future climate conditions? Winter mean T in Helsinki (1961-2008) 1961- 20081961- 1990 Temperature (°C) P r o b a b i l i t y d e n s i t y -12 4 Simplest case: change in mean climate, with no change in the magnitude of variability If variability changes as well, the two tails of the distribution (e.g., warm and cold) will be affected differently. IPCC (2001 /media/ces/RaisanenJouni_CES_2010.pdf

• 67. Case_B___Road_transport_operation_and_infrastructure_planning

  ) Annual Winter Summer • Accounts for natural variability and differences between climate models Width of the distribution primarily determined by natural temperature variability: larger in winter than in summer. Winter Summer Annual Best estimate (ºC) 1.3 0.7 1.0 5-95% uncertainty range (ºC) -0.5…+3.1 -0.2…+1.6 0.0…+1.8 Probability of warming (%) 90% 90% 96% Ref: Räisänen and Ruokolainen (2007 /media/loftslag/Case_B___Road_transport_operation_and_infrastructure_planning.pdf

• 68. Group3-The-future-of-the-Finnish-national-road-network

  The future of the Finnish national road network under changing climate Erik Schou Gudina L. Feyisa Karoliina Pilli-Sihvola NONAM summer school 26.8.2011 Copenhagen Fuzzy cognitive map -1 -0,5 0 0,5 1 1,5 1 3 5 7 9 11 13 15 17 19 21 Traffic Costs Policy CC Policy Traffic Research Tech Strat Nat.feat Costs 1 2 3 4 5 6 7 8 CC 1 0 0,2 0 0 0 0 0 0,7 Policy 2 0 0 -0,6 0,8 0 0 0 0 /media/loftslag/Group3-The-future-of-the-Finnish-national-road-network.pdf

• 69. CES_D2.4_VMGO

  deviation across the ensemble) and sign agreement (a percentage of models in the ensemble that project the same sign of changes as the entire ensemble does). Analysis In Fig.1a shown are simulated changes in the annual extreme temperature range calculated as difference between 20 yr mean absolute annual maxima and minima temperatures in baseline and future scenario periods. The range /media/ces/CES_D2.4_VMGO.pdf

• 70. PhD_course-Programme_26Aug2011-final

  presentations of own poster (2 minutes per student) + poster session + refreshments + formation of groups Students Tuesday, August 23 9:00 - 9:45 Introduction to Horsens case study on water HJH Horsens case + TOR 9:45 - 10:30 Introduction to Finnish case study on roads AP Coffee 11:00 - 12:45 Exersize works Students Lunch 13:45 - 15:30 Uncertainty concepts and tools JCR Refsgaard et al. (2007) van der /media/vedurstofan/PhD_course-Programme_26Aug2011-final.pdf