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Book ChapterDOI

The Turbulent Ocean: Structure and résumé

S. A. Thorpe
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The article was published on 2005-01-01. It has received 1 citations till now.

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Vortex pairing in an unstable anticyclonic shear flow: discrete subharmonics of one pendulum day

TL;DR: In this article, the authors observed the downstream evolution of an oceanic zonal horizontal shear flow at a Reynolds number of about 1011, formed as the westward North Equatorial Current passes the island of Hawai'i, revealing finite-amplitude anticyclonic vortices resulting from instability of the shear.
References
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Journal ArticleDOI

Dispersion of soluble matter in solvent flowing slowly through a tube

TL;DR: In this paper, it was shown analytically that the distribution of concentration produced in this way is centred on a point which moves with the mean speed of flow and is symmetrical about it in spite of the asymmetry of the flow.
Journal ArticleDOI

On density effects and large structure in turbulent mixing layers

TL;DR: In this article, Spark shadow pictures and measurements of density fluctuations suggest that turbulent mixing and entrainment is a process of entanglement on the scale of the large structures; some statistical properties of the latter are used to obtain an estimate of entrainedment rates, and large changes of the density ratio across the mixing layer were found to have a relatively small effect on the spreading angle.
MonographDOI

Turbulent Transport of Momentum and Heat

TL;DR: In this article, the authors discuss the Reynolds equations and estimate of the Reynolds stress in the kinetic theory of gases, and describe the effects of shear flow near a rigid wall.
MonographDOI

The Statistical Description of Turbulence

TL;DR: In this article, the probability density, Fourier transforms and characteristic functions, joint statistics and statistical independence, Correlation functions and spectra, the central limit theorem, and the relation functions are discussed.
Journal ArticleDOI

The Instability of Liquid Surfaces when Accelerated in a Direction Perpendicular to their Planes. I

TL;DR: In this article, it was shown that when two superposed fluids of different densities are accelerated in a direction perpendicular to their interface, this surface is stable or unstable according to whether the acceleration is directed from the heavier to the lighter fluid or vice versa.