The complexity of anisotropic turbulent processes over a wide range of spatiotemporal scales in engineering turbulence and climate atmosphere ocean science requires novel computational strategies with the current and next generations of supercomputers. In these applications the smaller-scale fluctuations do not statistically equilibrate as assumed in traditional closure modeling and intermittently send significant energy to the large-scale fluctuations. Superparametrization is a novel class of seamless multi-scale algorithms that reduce computational labor by imposing an artificial scale gap between the energetic smaller-scale fluctuations and the large-scale fluctuations. The main result here is the systematic development of simple test models that are mathematically tractable yet capture key features of anisotropic turbulence in applications involving statistically intermittent fluctuations without local statistical equilibration, with moderate scale separation and significant impact on the large-scale dynamics. The properties of the simplest scalar test model are developed here and utilized to test the statistical performance of superparametrization algorithms with an imposed spectral gap in a system with an energetic -5/3 turbulent spectrum for the fluctuations.intermittency | moderate-scale separation | multiscale algorithms T he complexity of anisotropic turbulent processes over a wide range of spatiotemporal scales in engineering shear turbulence and combustion (1-3) as well as climate atmosphere ocean science requires novel computational strategies even with the current and next generations of supercomputers. This is especially important since energy often flows intermittently from the smaller unresolved or marginally resolved scales to affect the largest observed scales in such anisotropic turbulent flows. For example, atmospheric processes of weather and climate cover ≈10 decades of spatial scales, from a fraction of a millimeter to planetary scales. Regarding atmospheric fluid dynamics, one is primarily concerned with spatial scales larger than tens of meters because the smaller scales fall whithin the inertial range of atmospheric turbulence. Spatial scales between 100 m and 100 km, referred to as small through mesoscale, show an abundance of processes associated with dry and moist convection, clouds, waves, boundary layer, topographic, and frontal circulations. A major stumbling block in the accurate prediction of weather and short-term climate on the planetary and synoptic scales is the accurate parametrization of moist convection. These problems involve intermittency in space and time due to complex evolving, strongly chaotic, and quiescent regions without statistical equilibration and with only moderatescale separation so that traditional turbulence closure modeling fails (1-3). Cloud-system-resolving models realistically represent small-scale and mesoscale processes with fine computational grids. But because of the high computational cost, they cannot be applied to large ensemble size weather pr...