This PR just changes the thermocline in three_layer_constant_fluxes.jl to have a variable N²(z) structure parameterized by a fitted cubic function.
The idea is to enrich the training data as convection is no longer entraining into a fluid layer of constant stratification, although might need to play around with the model parameters to get a temperature profile where the N²(z) structure is significant (and it still finishes in a reasonable amount of time).
This PR just changes the thermocline in
three_layer_constant_fluxes.jl
to have a variable N²(z) structure parameterized by a fitted cubic function.The idea is to enrich the training data as convection is no longer entraining into a fluid layer of constant stratification, although might need to play around with the model parameters to get a temperature profile where the N²(z) structure is significant (and it still finishes in a reasonable amount of time).
To give some idea of what it looks like: