Problèmes de Pourcentage Mixtes avec des Montants de Nombres Décimaux et des Pourcentages Multiples de 25 (Sommes en Dollars) (A)

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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

The resulting spatial and temporal pat- terns of land surface fluxes and surface resistance are used to more fully understand the hydro-ecological trends observed across a

(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

Wavelet maxima curves of surface latent heat flux anomalies associated with Indian

The calanoid copepod Acartia tonsa, observed in the Gironde estuary for the first time in 1983, have since colonized most part of the estuary, reaching a level of abundance