The problem is the context was
eddy diffusion which is not diffusive mixing.
Not exact matches
They then estimated the heat flux into the thermocline using a standard (accepted) model, with a thermocline
eddy diffusion coefficient of 1.2E - 5 m ^ 2 / s from Ledwell: We estimate s by using this slope along with k = 1.2x10 - 5 m2 / s (the
eddy diffusion coefficient in the thermocline [Ledwell et al., 1998]-RRB- So if they are wrong, either their basic model is wrong (
which seems unlikely - it is just a simple energy balance model after all), or their choice of
eddy diffusion coefficient is wrong.
Ledwell's 1998 SF6 tracer experiments established an
eddy diffusion coefficient of around 10 - 5,
which is what Douglass uses.
When a gyre region is added to the channel, vertical
diffusion in the gyre exerts some control on the channel stratification even at higher winds, forcing the mass balance into a mixed regime in
which both
eddy and diffusive effects are important.