期刊名称:Journal of Advances in Modeling Earth Systems
电子版ISSN:1942-2466
出版年度:2020
卷号:12
期号:12
页码:1-22
DOI:10.1029/2020MS002090
出版社:John Wiley & Sons, Ltd.
摘要:An important characteristic of geophysically turbulent flows is the transfer of energy
between scales. Balanced flows pass energy from smaller to larger scales as part of the well-known
upscale cascade, while submesoscale and smaller scale flows can transfer energy eventually to smaller,
dissipative scales. Much effort has been put into quantifying these transfers, but a complicating factor in
realistic settings is that the underlying flows are often strongly spatially heterogeneous and anisotropic.
Furthermore, the flows may be embedded in irregularly shaped domains that can be multiply connected.
As a result, straightforward approaches like computing Fourier spatial spectra of nonlinear terms suffer
from a number of conceptual issues. In this paper, we develop a method to compute cross-scale energy
transfers in general settings, allowing for arbitrary flow structure, anisotropy, and inhomogeneity. We
employ Green's function approach to the kinetic energy equation to relate kinetic energy at a point to its
Lagrangian history. A spatial filtering of the resulting equation naturally decomposes kinetic energy into
length-scale-dependent contributions and describes how the transfer of energy between those scales
takes place. The method is applied to a doubly periodic simulation of vortex merger, resulting in the
demonstration of the expected upscale energy cascade. Somewhat novel results are that the energy
transfers are dominated by pressure work, rather than kinetic energy exchange, and dissipation is
a noticeable influence on the larger scale energy budgets. We also describe, but do not employ here, a
technique for developing filters to use in complex domains.