The Lagrangian-averaged Navier–Stokes-
alpha
α
$\alpha$
(LANS-
alpha
α
$\alpha$
) model, a turbulence closure scheme based on energy-conserving modifications to nonlinear advection, can produce more energetic simulations than standard models, leading to improved fidelity (e.g. in ocean models). However, comprehensive understanding of the mechanism driving this energetic enhancement has proven elusive. To address this, we derive the fast quasi-geostrophic limit of the three-dimensional, stably stratified LANS-
alpha
α
$\alpha$
equations. This provides both the slow, balanced flow and the leading-order fast wave dynamics. Analysis of these wave dynamics suggests that an explanation for the energetic enhancement lies in the dual role of the smoothing parameter itself: increasing
alpha
α
$\alpha$
regularises the dynamics and simultaneously generates a robust landscape of wave–wave resonant interactions. Direct numerical simulations show that
alpha
α
$\alpha$
plays an analogous role to the Burger number (
italic Bu
Bu
${\textit{Bu}}$
) in governing the partition of energy between slow and fast modes – and, consequently, the time scale of geostrophic adjustment – but with key differences. Increasing
alpha
α
$\alpha$
, regardless of the relative strengths of rotation and stratification, extends the persistence of wave energy by delaying the dominance of the slow modes. We find that the creation of an energy pathway involving only fast waves is a universal outcome of the regularisation across all values of
italic Bu
Bu
${\textit{Bu}}$
, accompanied by a restructuring of slow–fast–fast interactions. These insights unify the LANS-
alpha
α
$\alpha$
model’s characteristic energetic enhancement with, in some cases, its known numerical stiffness, identifying potential pathways to mitigate stability issues hindering the broader application of LANS-
alpha
α
$\alpha$
-type models.