Please use this identifier to cite or link to this item: https://oar.tib.eu/jspui/handle/123456789/5912
Files in This Item:
File SizeFormat 
Schaefer-Rolffs2015.pdf479,65 kBAdobe PDFView/Open
Title: A scale invariance criterion for les parametrizations
Authors: Schaefer-Rolffs, U.Knöpfel, R.Becker, E.
Publishers Version: https://doi.org/10.1127/metz/2014/0623
Issue Date: 2014
Published in: Meteorologische Zeitschrift Vol. 24 (2014), No. 1
Publisher: Stuttgart : Gebrüder Bornträger Verlagsbuchhandlung
Abstract: Turbulent kinetic energy cascades in fluid dynamical systems are usually characterized by scale invariance. However, representations of subgrid scales in large eddy simulations do not necessarily fulfill this constraint. So far, scale invariance has been considered in the context of isotropic, incompressible, and three-dimensional turbulence. In the present paper, the theory is extended to compressible flows that obey the hydrostatic approximation, as well as to corresponding subgrid-scale parametrizations. A criterion is presented to check if the symmetries of the governing equations are correctly translated into the equations used in numerical models. By applying scaling transformations to the model equations, relations between the scaling factors are obtained by demanding that the mathematical structure of the equations does not change. The criterion is validated by recovering the breakdown of scale invariance in the classical Smagorinsky model and confirming scale invariance for the Dynamic Smagorinsky Model. The criterion also shows that the compressible continuity equation is intrinsically scale-invariant. The criterion also proves that a scaleinvariant turbulent kinetic energy equation or a scale-invariant equation of motion for a passive tracer is obtained only with a dynamic mixing length. For large-scale atmospheric flows governed by the hydrostatic balance the energy cascade is due to horizontal advection and the vertical length scale exhibits a scaling behaviour that is different from that derived for horizontal length scales.
Keywords: Atmospheric physics; GCMs; General fluid dynamics; LES parametrizations; Scale invariance; compressible flow; fluid dynamics; general circulation model; hydrostatics; large eddy simulation; parameterization; turbulent flow
DDC: 530
License: CC BY-NC 3.0 Unported
Link to License: https://creativecommons.org/licenses/by-nc/3.0/
Appears in Collections:Physik



This item is licensed under a Creative Commons License Creative Commons