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I asked a researcher about this and the answer is basically no, more or less. While the kind of stratification shown in the diagram in the main post is highly simplified, it can still be broken up into three main layers in terms of temperature and density. The coldest water at the bottom, the warmest at the top, and a slowly mixing layer between them.
The image below is a cross section of lake Ontario in late summer, the hypolimnion in blue, the metalimnion/thermocline is somewhere in the bottom of the green section, and the epilimnion is the red and most of the green.
The other image below is a graph showing temperature at depth over time, the parts in May and October where it is all one color represent mixing events when the temperature difference between the layers is not enough to enforce stratification.
I see. Thanks for the response!
That lake thermal structure is quite interesting.
So as the temperature/wind speed is raised, the epilimnion just becomes bigger until everything is just one layer.
Or is it more a function of time? It takes months for the hypolimnion to mix and heat?