The flow past a
$6:1$ prolate spheroid at a moderate pitch angle
$\alpha =10^\circ$ is investigated with a focus on the turbulent wake in a high-fidelity large eddy simulation (LES) study. Two length-based Reynolds numbers,
${\textit{Re}}_L=3\times 10^4$ and
$9\times 10^4$, and four Froude numbers,
${\textit{Fr}} = \infty \text{(unstratified)}, 6, 1.9 \text{ and }1$, are selected for the parametric study. Spectral proper orthogonal decomposition (SPOD) analysis of the flow reveals the leading coherent modes in the unsteady separated flow at the tail of the body. At the higher
${\textit{Re}}_L=9\times 10^4$, a high-frequency spanwise flapping of shear layers on either side of the body is observed in the separated boundary layer for all cases. The flapping does not perturb the lateral symmetry of the wake. At
${\textit{Fr}}=\infty$, a low-frequency oscillating laterally asymmetric mode, which is found in addition to the shear-layer mode, leads to a sidewise unsteady lateral load. All temporally averaged wakes at
${\textit{Re}}=9\times 10^4$ are found to be spanwise symmetric in the mean as opposed to the lower
${\textit{Re}}=3\times 10^4$, at which the
${\textit{Fr}}=\infty \text{ and }6$ wakes exhibit asymmetry. The turbulent kinetic energy (TKE) budget is compared among cases. Here,
${\textit{Fr}}=\infty$ exhibits higher production and dissipation compared with
${\textit{Fr}}=6 \text{ and }1.9$. The streamwise vortex pair in the wake induces a significant mean vertical velocity (
$U_z$). Therefore, in contrast to straight-on flow, the terms involving gradients of
$U_z$ matter to TKE production. Buoyancy reduces
$U_z$ and also the Reynolds shear stresses involving
$u^{\prime}_z$. Through this indirect mechanism, buoyancy exerts control on the wake TKE budget, albeit being small relative to production and dissipation. Buoyancy, through the baroclinic torque, is found to qualitatively affect the streamwise vorticity. In particular, the primary vortex pair is extinguished in the intermediate wake and two new vortex pairs form with opposite-sense circulation relative to the primary.