Connection between encounter volume and diffusivity in geophysical flows

Trajectory encounter volume – the volume of fluid that passes close to a reference fluid parcel over some time interval – has been recently introduced as a measure of mixing potential of a flow. Diffusivity is the most commonly used characteristic of turbulent diffusion. We derive the analytical rel...

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Bibliographic Details
Published in:Nonlinear Processes in Geophysics
Main Authors: Rypina, Irina I., Llewellyn Smith, Stefan G., Pratt, Larry J.
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2018
Subjects:
Online Access:https://doi.org/10.5194/npg-25-267-2018
https://noa.gwlb.de/receive/cop_mods_00006870
https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00006827/npg-25-267-2018.pdf
https://npg.copernicus.org/articles/25/267/2018/npg-25-267-2018.pdf
Description
Summary:Trajectory encounter volume – the volume of fluid that passes close to a reference fluid parcel over some time interval – has been recently introduced as a measure of mixing potential of a flow. Diffusivity is the most commonly used characteristic of turbulent diffusion. We derive the analytical relationship between the encounter volume and diffusivity under the assumption of an isotropic random walk, i.e., diffusive motion, in one and two dimensions. We apply the derived formulas to produce maps of encounter volume and the corresponding diffusivity in the Gulf Stream region of the North Atlantic based on satellite altimetry, and discuss the mixing properties of Gulf Stream rings. Advantages offered by the derived formula for estimating diffusivity from oceanographic data are discussed, as well as applications to other disciplines.