256 research outputs found

    Les espaces de l'halieutique

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    On the decrease of intermittency in decaying rotating turbulence

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    The scaling of the longitudinal velocity structure functions, Sq(r)=<∣Ύu(r)∣q>∌rζqS_q(r) = < | \delta u (r) |^q > \sim r^{\zeta_q}, is analyzed up to order q=8q=8 in a decaying rotating turbulence experiment from a large Particle Image Velocimetry (PIV) dataset. The exponent of the second-order structure function, ζ2\zeta_2, increases throughout the self-similar decay regime, up to the Ekman time scale. The normalized higher-order exponents, ζq/ζ2\zeta_q / \zeta_2, are close to those of the intermittent non-rotating case at small times, but show a marked departure at larger times, on a time scale Ω−1\Omega^{-1} (Ω\Omega is the rotation rate), although a strictly non-intermittent linear law ζq/ζ2=q/2\zeta_q / \zeta_2 = q/2 is not reached.Comment: 5 pages, 5 figures. In revision for Phys. Fluids Letter

    Experimental and numerical study of mean zonal flows generated by librations of a rotating spherical cavity

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    International audienceWe study both experimentally and numerically the steady zonal flow generated by longitudinal librations of a spherical rotating container. This study follows the recent weakly nonlinear analysis of Busse (2010), developed in the limit of small libration frequency - rotation rate ratio, and large libration frequency - spin-up time product. Using PIV measurements as well as results from axisymmetric numerical simulations, we confirm quantitatively the main features of Busse's analytical solution: the zonal flow takes the form of a retrograde solid body rotation in the fluid interior, which does not depend on the libration frequency nor on the Ekman number, and which varies as the square of the amplitude of excitation. We also report the presence of an unpredicted prograde flow at the equator near the outer wall

    Campagne CORAIL 1 de chalutage exploratoire aux ßles Chesterfield et à Lansdowne ("N.O. ALIS" - 15 août au 4 septembre 1988)

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    Au cours de la campagne de chalutage exploratoire CORAIL 1 le N.O. ALIS a rĂ©alisĂ© 55 traits de chalut aux Ăźles Chesterfield, Bellona et sur le banc de Lansdowne. La proportion de fonds chalutables n'excĂšde pas 30 % des fonds de plus de 50 m et est nulle entre 0 et 50 m. Au total 123 espĂšces ont Ă©tĂ© collectĂ©es dont trois pourraient ĂȘtre nouvelles. Les affinitĂ©s des peuplements ichthyologiques rencontrĂ©s sont plus importantes avec la Nouvelle-CalĂ©donie qu'avec l'Australie. Les densitĂ©s (8 Ă  35 poissons/ha) et les biomasses (0.4 Ă  2.6 kg/ha) estimĂ©es sont trĂšs faibles, de 8 Ă  60 fois moindres que ce qui a Ă©tĂ© observĂ© en Nouvelle CalĂ©donie. Les frĂ©quences de longueur des principales espĂšces sont du mĂȘme ordre que celles observĂ©es en Nouvelle-CalĂ©donie Ă  des Ă©poques similaires. La taille maximale des espĂšces commerciales est supĂ©rieure Ă  celles notĂ©es en Nouvelle-CalĂ©donie. (RĂ©sumĂ© d'auteur

    From granular collapses to shallow water waves: A predictive model for tsunami generation

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    In this article, we present a predictive model for the amplitude of impulse waves generated by the collapse of a granular column into a water layer. The model, which combines the spreading dynamics of the grains and the wave hydrodynamics in shallow water, is successfully compared to a large dataset of laboratory experiments, and captures the influence of the initial parameters while giving an accurate prediction. Furthermore, the role played on the wave generation by two key dimensionless numbers, i.e., the global Froude number and the relative volume of the immersed deposit, is rationalized. These results provide a simplified, yet comprehensive, physical description of the generation of tsunami waves engendered by large-scale subaerial landslides, rockfalls, or cliff collapses in a shallow water
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