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+*Revise non-Boussinesq offline tracer diffusivity
Rescale the units diapycnal diffusivity used in the offline tracer mode to work in [H Z T-1 ~> m2 s-1 or kg m-1 s-1], making it consistent with what has already been done for other diapycnal diffusivities. This change involves changes to the units of arguments to update_offline_from_files and ALE_offline_inputs and to two elements of offline_transport_CS. It also includes a new thermo_vary_type argument to offline_diabatic_ale, as well as a call to thickness_to_dz in that same routine to set the values of the newly added 3-d array of the vertical distances across layers and a change in name and units of the inverse thickness variable used to find the fluxes. All answers are bitwise identical in Boussinesq mode, but in offline tracer calculations in non-Boussinesq mode they will change to become independent of the Boussinesq reference density.
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