“…Algebraic models for the variance [8,9,10,11,12] and the dissipation rate [8,13,14] directly describe the modeled parameter using information about the local scalar field and filter width, and have the advantage of being conceptually simple and computationally inexpensive. Transport equation models for the variance [12,15,16] and for the dissipation rate [17,18,19] offer different advantages: they do not forcibly assume that production and dissipation processes are in equilibrium, they produce fields that are less noisy than algebraic models, and they incorporate a wider range of physics. Nonetheless, transport equation approaches are sensitive to the descriptions used to model unclosed subfilter terms, and the performance of these equations is not always superior to the performance of algebraic models [12].…”