Problèmes de Pourcentage Mixtes avec des Montants de Nombres Décimaux et des Pourcentages Multiples de 5 (Sommes en Dollars) (A)

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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

(2002) and Desinov (2004) believe that the high water input to the glacier in combination with the overload of debris by continuous rock/ice fall in late summer 2002 was sufficient

8a where are re- ported the results of conventional direct shear tests on the marine Bisaccia clay shale, run, as usual, in a bath of distilled water, under a normal stress less