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Titlebook: IUTAM Symposium on Developments in Geophysical Turbulence; Robert M. Kerr,Yoshifumi Kimura Book 2000 Springer Science+Business Media Dordr

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Boundary Sources of Potential Vorticity in Geophysical Circulations,lation is determined by mass, heat and momentum exchange with the atmosphere and the solid Earth. The primary conservible tracers, potential vorticity (PV) and potential density, are also forced at these boundaries, and yet it is difficult to assess the rate of PV influx from the other, more ‘natura
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Three-Dimensional Initiation of Thermohaline Fingering,ses which demonstrate how the salt finger flow field development is dependent upon the density ratio..In both density ratio cases, the initial stages of the flow field are wave dominated. In the lower density ratio case...1.2, interfaces with jumps in salinity and temperature develop within the firs
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Evolution of a Tracer Gradient in an Incompressible, Two-Dimensional Flow,gradients grow exponentially. They argue that their criteria provides more predictive power than the known Obuko-Weiss criterion. The present paper makes two points: first, the problem posed by these authors can be solved exactly for a two-dimensional, incompressible flow. Second, for many flows no
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Analytical Models for Vertical Collapse and Instability in Stably Stratified Flows, here through exact laminar solutions of the equations describing low Froude number limiting dynamics. It is found that fairly weak rotation with moderately large Rossby numbers.1, 5, can prevent the vertical collapse process in these exact solutions; the collapse process is also suppressed for suff
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Direct Laboratory Simulations of 3D Vortex Structures in Stably Stratified Rotating Fluids,aboratory Simulation (DLS) relies on getting the Reynolds number from the length scale while keeping the velocity small, hence providing a characteristic time scale that is sufficiently large to permit full 3D scanning through the measurement volume in a relatively short time. 3D measurements of the
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