86 results were found for 다우나스닥(WWW͵88M͵KR)WWW͵88M͵KR 독일닥스매매 코스닥실시간◥r 대여계좌㋮d 해외선물 ぜ乜 causeway.

Results:

• 71. Refsgaard_2-uncertainty

  Delta Change Method (correction of observed precipitation) Transformation of precipitation cont fut obsfut M M PP = Observeret n dbør 0 5 10 15 20 25 30 1-12-99 11-12-99 21-12-99 31-12-99 Dato N ed bø r (m m /d ag ) Observeret Skal ring af e 5 10 15 20 25 30 35 4 - - - - t N ed bø r (m m /d ag ) Observeret D lta Change Critical assumption: Future dynamics = present dynamics No change in number /media/loftslag/Refsgaard_2-uncertainty.pdf

• 72. Lorenzoni_Pidgeon_2006

  /media/loftslag/Lorenzoni_Pidgeon_2006.pdf

• 73. Eriksson_Garvill_Nordlund_2006

  ) measures. The main purpose ARTICLE IN PRESS of this study is to test a model of the relations between factors expected to influence the acceptability of TDM measures. In addition, comparisons between car users’ 0272-4944/$ - see front matter r 2006 Elsevier Ltd. All rights reserved. doi:10.1016/j.jenvp.2006.05.003
  Corresponding author. Department of Psychology, Umea˚ University, Sweden. Tel.: +46 90 /media/loftslag/Eriksson_Garvill_Nordlund_2006.pdf

• 74. Journal_of_Hydrology_Veijalainen_etal

  in Finland Noora Veijalainen a,*, Eliisa Lotsari b, Petteri Alho b, Bertel Vehviläinen a, Jukka Käyhkö b a Freshwater Centre, Finnish Environment Institute, Mechelininkatu 34a, P.O. Box 140, FI-00251, Helsinki, Finland b Department of Geography, FI-20014 University of Turku, Turku, Finland a r t i c l e i n f o Article history: Received 7 January 2010 Received in revised form 13 June 2010 Accepted /media/ces/Journal_of_Hydrology_Veijalainen_etal.pdf

• 75. Daniell_etal-2010

  /media/loftslag/Daniell_etal-2010.pdf

• 76. PhD_course-Programme_26Aug2011-final

  Hare MP, Barreteau O, Beck MB, Letcher RA, Mostert E, Tabara JD, Ridder D, Cogan V, Pahl-Wostl C (2006) Methods for stakeholder participation in water management. Chapter 8 in Giupponi, C. Jakeman, A.J., Karssenberg, D. & Hare, M. (Eds) Sustainable management of water resources: an integrated approach. Edward Elgar: Chichester. Hare MP (2011) Forms of participatory modelling and its potential /media/vedurstofan/PhD_course-Programme_26Aug2011-final.pdf

• 77. VI_2020_004

  -CALPUFF model is not using plume height estimates as an input parameter. The model itself solves the equations describing the rising of the mixture in the atmosphere and calculates the top-plume height by using some physical parameters as the vertical mixture velocity (V) and the radius of the vent (R). Based on these two parameters, V and R, we get an estimate of the mass flow rate and we /media/vedurstofan-utgafa-2020/VI_2020_004.pdf

• 78. VI_2013_006

  Estimation of eruption site location using volcanic lightning Þórður Arason Guðrún Nína Petersen Halldór Björnsson VÍ 2013-006 Report   Estimation of eruption site location using volcanic lightning V Í 201 3 - 006 ISS N 167 0 - 8 261 Report? +354 522 60 00 ved u r@ ve d u r. is Veð u rst of a Ísla n d s Búst a ð a ve gur 7–9 150 Reykja vík Þórður Arason, Icelandic Met /media/vedurstofan/utgafa/skyrslur/2013/VI_2013_006.pdf

• 79. 2010_017

  ) storage coefficient of interflow ki; (3) drainage density d; (4) the fraction of surface runoff from snowmelt; and (5) the recession constant krec for the decreasing saturated hydraulic conductivity with increasing depth. For the groundwater flow, adjusted parameters (6–7) are the hydraulic conductivity in the X and Y direction. The hydraulic conductivity is adjusted in distributed grids unlike /media/ces/2010_017.pdf

• 80. VI_2017_009

  and glaciers. The former trend is mainly visible in the Westfjords, an area in northwest Iceland, in the winter (see Figure 8a and 8b) and in northeast Iceland in the summer, especially east of Akureyri in the RCP8.5 scenario (see Figures 8c and d). The latter trend is most clearly seen during summer and in cases with the RCM RCA4 with RCP8.5. Extreme temperature trends In a previous section we /media/vedurstofan-utgafa-2017/VI_2017_009.pdf