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In fact, the great adaptability of numerical models has led to incorporate preventive and corrective maintenance measures in the calculations.
The reliability of the numerical models has been demonstrated through good agreement between the calculated and measured efficiency of an H-Darrieus.
Hypothesis testing via numerical models has emerged as a powerful tool which permits the verification of theoretical frameworks against canonical experimental and clinical observations.
A wide range of numerical models has been employed for the study of this region and, hence, only phase-resolving approaches (i.e., depth-averaged and depth-resolving models) are analyzed.
Finally, altimetry, in synergy with other observations and high-resolution numerical models, has helped reveal the complexity of the sub-mesoscale features, associated with stirring and mixing around the mesoscale eddies, of great importance for the vertical exchange of oceanic tracers.
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For forty years, numerous thermo-hydraulic coupled numerical models have been developed.
The numerical models have advantage that they are based on the physics of the underlying process.
Essentially, two main distinct categories of numerical models have been developed for ICE studies.
Previously, two types of numerical models have been proposed to calculate the front condition.
Numerical models have been developed over recent decades to investigate the crack behavior in rock media.
Previously, two types of numerical models have been proposed to solve the front condition.
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