Problèmes de Pourcentage Mixtes avec des Montants de Nombres Entiers et des Pourcentages Variant de 1 à 99 (A)

In this paper, we derive the statistical distribution in the far field zone from the first-order small perturbation method in the particular case of perfectly conducting 1D random

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One approach is based on a Helmert or similarity coordinate transforma- tion where the displacements and the respective covariance matrix are transformed into a unique

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Since the particle and flow characteristics are close to those corresponding to the copepod framework: the value of β is close to 1, and the Stokes number is close to the range (0.4,

Cell can also be explained by the change in the barotropic velocity field, an increase in the zonal wind stress producing an increased northward flow in shallow regions and

By adapting and then solving the associated cubic nonlinear Schr¨odinger equation, we have shown that the EMIC waves are mod- ulationally stable against quasi-stationary

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