Since this effect would not depend on slow rates of thermal
diffusion though frozen sediments, but instead
by a
simple loss of ice, which could occur more quickly, such hydrates might be more vulnerable to destabilization than hydrates buried under permafrost.
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.