The 3-D primitive equations and incompressible Navier-Stokes equations with full hyperviscosity and only horizontal hyper-viscosity are considered on the torus, i.e., the diffusion term −∆ isHyper-viscosity is applied in many numerical schemes, and in particular horizontal hyper-viscosity appears in meteorological models. A classical result by Lions states that for the Navier-Stokes equations uniqueness of global weak solutions for initial data in L 2 holds if −∆ is replaced by (−∆) 5/4 . Here, for the primitive equations the corresponding result is proven for (−∆) 8/5 . For the case of horizontal hyperviscosity l = 2 is sufficient in both cases. Strong convergence for ε → 0 of hyper-viscous solutions to a weak solution of the Navier-Stokes and primitive equations, respectively, is proven as well. The approach presented here is based on the construction of strong solutions via an evolution equation approach for initial data in L 2 and weak-strong uniqueness.2010 Mathematics Subject Classification. Primary: 35Q35; Secondary: 35K25, 35K30, 35Q30, 76D03, 86A05.