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66 results were found for 【77AGG.COM】citratoto slot banjir69 slot box 138 slot login sarangsbobet slot zpk.


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  • 51. Refsgaard_etal-2007-Uncertainty-EMS

    equations are valid only if the following conditions are met: (1) the uncertainties have Gaussian (normal) distribu- tions; (2) the uncertainties for non-linear models are relatively small: the standard deviation divided by the mean value is less than 0.3; and (3) the uncertainties have no significant covariance. The error propagation equations for the most common oper- ators can be seen in Box 1 /media/loftslag/Refsgaard_etal-2007-Uncertainty-EMS.pdf
  • 52. VI_2015_009

    )=(θ0) + (θ1)(AP) Rel. RMSE= 1 NS= 0.89 MAE= 71 l l l l l l l ll ll 0 500 1500 2500 0 50 0 150 0 250 0 Pred. (m³/s) R ef . (m ³/s ) µ(D)=(θ0) + (θ1)(AP Z) Rel. RMSE= 1.2 NS= −0.095 MAE= 161 l l l l l l l ll l ll 0 400 800 1200 0 50 0 100 0 150 0 Pred. (m³/s) R ef . (m ³/s ) µ(D)=(θ0) + (θ1)(AP L) Rel. RMSE= 0.95 NS= 0.71 MAE= 138 l l l l l l l ll l ll 0 400 800 1200 0 50 0 100 0 150 0 Pred. (m³/s /media/vedurstofan/utgafa/skyrslur/2015/VI_2015_009.pdf
  • 53. VI_2021_008

    a coherent, emergent signal in RSAM data (see Figure 2), raising the question: Can RSAM data be empirically used to detect volcanic tremor events preceding eruptions? 6 Figure 1. Photo of the monitoring setup in the IMO’s natural hazards monitoring room. The right screen shows real-time earthquake and tremor data. Tremv output is displayed in red box with the last 24 hrs of all frequency /media/vedurstofan-utgafa-2021/VI_2021_008.pdf
  • 54. VI_2014_005

    ), and the National Energy Authority (Orkustofnun). 3 Model terrain and surface type The HARMONIE model dominant surface type and terrain elevation are shown in Figures 1 and 2, respectively. Surface type is specified in SURFEX by the global land surface database ECOCLIMAP-I (Champeaux et al., 2005). Within each grid box, ground coverage is represented by fractions of one for each category of surface type /media/vedurstofan/utgafa/skyrslur/2014/VI_2014_005.pdf
  • 55. Henriksen_Barlebo-2008-AWM_BBN-Journ_Env_Management

    should be incorporated into decision support systems and tools to capture the and the complexity of water management as it is seen from different mental frames and interest group positions should be used in adaptive water management. The broad range of tools available for integrated water resource management (IWRM) includes e.g. GWP Tool- box, HarmoniCA/Catchmod tools, decision support sys- tems /media/loftslag/Henriksen_Barlebo-2008-AWM_BBN-Journ_Env_Management.pdf
  • 56. 2010_005_

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

    the location of the mass balance stakes at Breiðamerkurjökull (Bre). The red box indicates the posi- tion of the frame to the right. (C) Hoffellsjökull surface topography in 2001. The ice divide and the model domain are indicated with the red curve enclosing a glaciated area of ∼212 km2 in 2001. Black triangles show the locations of automatic weather stations on the glacier. N is the location /media/ces/Adalgeirsdottir-etal-tc-5-961-2011.pdf
  • 58. CES_D2.4_task1

    1 Probability distributions of monthly-to-annual mean temperature and precipitation in a changing climate (CES Climate Modelling and Scenarios Deliverable D2.4, task I) Jouni Räisänen Department of Physics, P.O. Box 48, FI-00014 University of Helsinki, Finland Email: jouni.raisanen@helsinki.fi 17 November 2009 AVAILABLE FROM: http://www.atm.helsinki.fi/~jaraisan/CES_D2.4 /media/ces/CES_D2.4_task1.pdf
  • 59. Kok_et_al._TFSC_published_2011

    development: Experiences from the SCENES project Kasper Kok a,, Mathijs van Vliet a, Ilona Bärlund c, Anna Dubel b, Jan Sendzimir b a Wageningen University, P.O. Box 47, 6700 AA Wageningen, Netherlands b International Institute for Applied Systems Analysis, Schlossplaz 1, A-2361 Laxenburg, Austria c Helmholtz Centre for Environmental Research (UFZ), Brückstrasse 3a, 39114 Magdeburg, Germany a r t i c /media/loftslag/Kok_et_al._TFSC_published_2011.pdf
  • 60. Reykholt-abstracts

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