The cross-stream diffusivity in the Southern Ocean (75S to 30S) for the period 2005 to 2015. The diffusion coefficients are calculated using the theory of Ferrari and Nikurashin (2010). The dataset includes the suppressed and unsupressed diffusivities, as well as the supression factor (the ratio of the unsuppressed and suppressed diffusivity
The transport induced by ocean mesoscale eddies remains unresolved in most state-of-the-art climate ...
Lagrangian isopycnal diffusivities quantify the along-isopycnal mixing of any tracer with mean gradi...
The article of record as published may be found at http://dx.doi.org/10.1155/2015/751404Sequential, ...
In this paper, the diffusion cloud method by dyes and the velocity correlation method are used to ca...
A statistical analysis of surface drifter observations is used to compute eddy length and time scale...
Diffusion coefficients are derived from trajectory analyses. Derived horizontal diffusivity in the l...
Surface cross-stream eddy diffusion in the Southern Ocean is estimated by monitoring dispersion of p...
Lagrangian isopycnal diffusivities quantify the along-isopycnal mixing of any tracer with mean gradi...
Finescale estimates of diapycnal diffusivity κ are computed from CTD and expendable CTD (XCTD) data ...
The apparent diapycnal diffusivity below the wind-driven surface mixed layer of the ocean was determ...
We describe a process called “squeeze dispersion” in which the squeezing of oceanic tracer gradients...
There are two distinct mechanisms by which eddies provide systematic transport of tracer on isopycna...
Copyright © 2015 Xuefeng Zhang et al.This is an open access article distributed under the Creative C...
An integral balance is developed for steady fluid flows relating dissipation in volumes bounded by i...
The horizontal dispersion of tracers in the presence of a random field of ocean surface waves is exa...
The transport induced by ocean mesoscale eddies remains unresolved in most state-of-the-art climate ...
Lagrangian isopycnal diffusivities quantify the along-isopycnal mixing of any tracer with mean gradi...
The article of record as published may be found at http://dx.doi.org/10.1155/2015/751404Sequential, ...
In this paper, the diffusion cloud method by dyes and the velocity correlation method are used to ca...
A statistical analysis of surface drifter observations is used to compute eddy length and time scale...
Diffusion coefficients are derived from trajectory analyses. Derived horizontal diffusivity in the l...
Surface cross-stream eddy diffusion in the Southern Ocean is estimated by monitoring dispersion of p...
Lagrangian isopycnal diffusivities quantify the along-isopycnal mixing of any tracer with mean gradi...
Finescale estimates of diapycnal diffusivity κ are computed from CTD and expendable CTD (XCTD) data ...
The apparent diapycnal diffusivity below the wind-driven surface mixed layer of the ocean was determ...
We describe a process called “squeeze dispersion” in which the squeezing of oceanic tracer gradients...
There are two distinct mechanisms by which eddies provide systematic transport of tracer on isopycna...
Copyright © 2015 Xuefeng Zhang et al.This is an open access article distributed under the Creative C...
An integral balance is developed for steady fluid flows relating dissipation in volumes bounded by i...
The horizontal dispersion of tracers in the presence of a random field of ocean surface waves is exa...
The transport induced by ocean mesoscale eddies remains unresolved in most state-of-the-art climate ...
Lagrangian isopycnal diffusivities quantify the along-isopycnal mixing of any tracer with mean gradi...
The article of record as published may be found at http://dx.doi.org/10.1155/2015/751404Sequential, ...
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