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Navier-Stokes equation , and numerical extrapolation of observed data . He shunned calculations of any length and numerical constants were often considered irrelevant . Observations and numerical model results reinforce the importance of using the locations of clouds , stationary boundaries , and horizontal rolls as potential indicators of deep moisture and potential locations of thunderstorm initiation . Calculations using recent rock characterization methods and numerical techniques will be made of the stability of the rock structure , and recent physico / chemical clay and concrete models will be used for calculating the isolating capacity of suitably backfilled reference repositories in terms of the concentration of hazardous ion species appearing in the farfield environment . In particular , the heavy emphasis placed on data as well as on graphical and numerical analysis reflects these discussions .