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Causal analysis of inner and outer motions in near-wall turbulence

Published online by Cambridge University Press:  14 September 2026

Jingxuan Zhang
Affiliation:
Center for Particle-Laden Turbulence, Key Laboratory of Mechanics on Disaster and Environment in Western China, The Ministry of Education, School of Civil Engineering and Mechanics, Lanzhou University, Lanzhou 730000, PR China
Zhengping Zhu
Affiliation:
Zhejiang Laboratory, Hangzhou 310000, PR China
Limin Wang
Affiliation:
Zhejiang Laboratory, Hangzhou 310000, PR China
Wei Gao
Affiliation:
State Key Laboratory of Water Resources Engineering and Management, Wuhan University, Wuhan, Hubei 430072, PR China Mechanical Engineering, Physical Science and Engineering Division, King Abdullah University of Science and Technology, Thuwal 23955-6900, Saudi Arabia
Ruifeng Hu*
Affiliation:
Center for Particle-Laden Turbulence, Key Laboratory of Mechanics on Disaster and Environment in Western China, The Ministry of Education, School of Civil Engineering and Mechanics, Lanzhou University, Lanzhou 730000, PR China
*
Corresponding author: Ruifeng Hu, hurf@lzu.edu.cn

Abstract

Content of image described in text.

In this work we study the causality of near-wall inner and outer turbulent motions. The inner motions are defined as the self-sustained near-wall cycle and the outer motions as those living in the logarithmic layer exhibiting footprints on the near-wall region. Causal inference with three typical methods is performed, i.e. transfer entropy, information flow and the synergistic–unique–redundant decomposition of causality. The causal inference methods are first applied to several canonical problems to illustrate their abilities, including a linear problem, a nonlinear problem and a low-dimensional model of near-wall turbulence. It is demonstrated that all three methods can produce consistent causal findings. Furthermore, we study the causalities between the inner and outer turbulent motions in a channel flow using the three methods with an improved inner–outer decomposition method. It is revealed that both the inner and outer motions are causally self-sustained, supporting the self-sustaining mechanism of turbulent motions at all scales. We also find that there are top-down and bottom-up causalities between the outer motions and their near-wall footprints owing to the dynamical coherence of inclined large-scale turbulent motions. More interestingly, pressure is identified to play an active role in the inner–outer causalities and may act as a bridge in linking the inner and outer turbulent motions.

Information

Type
JFM Papers
Copyright
© The Author(s), 2026. Published by Cambridge University Press
Figure 0

Figure 1. Figure 1 long description.Causal maps of the linear problem: (a) TE, (b) IF, (c) SURD. Red boxes: the ground-truth causal links in the system.

Figure 1

Figure 2. Causal maps of the nonlinear problem: (a) TE, (b) IF, (c) SURD. Red boxes: the causal links in the system.

Figure 2

Figure 3. Figure 3 long description.Causal maps of the low-dimensional model of near-wall turbulence: (a) TE, (b) IF, (c) SURD. Red boxes: the causal links associated with the self-sustaining cycle of streaks and vortex.

Figure 3

Table 1. Summary of the DNS datasets. The computational domain sizes in the streamwise and spanwise directions are denoted by Lx$L_x$ and Lz$L_z$, respectively, scaled by the outer length scale δ$\delta$. The viscous-scaled grid resolutions are represented by Δx+$\Delta x^+$ and Δz+$\Delta z^+$ for the streamwise and spanwise directions, with Δyw+$\Delta y^+_w$ and Δyc+$\Delta y^+_c$ indicating the wall-normal grid spacings at the wall and channel centre, respectively. The time span of the data is normalised as Tuτ/δ$\textit{Tu}_{\tau }/\delta$.Table 1 long description.

Figure 4

Figure 4. Wall-normal profiles of the RSS and its decomposed components at Reτ=1000,2000$Re_\tau =1000,2000$ and 5200$5200$. The line colours correspond to the cases listed in table 1.

Figure 5

Figure 5. Velocity fluctuation intensities of the demodulated inner motions at friction Reynolds numbers Reτ=1000,2000$Re_\tau =1000,2000$ and 5200$5200$. (a) Streamwise velocity fluctuations, (b) wall-normal velocity fluctuations, (c) spanwise velocity fluctuations, (d) cross components of the decomposed RSS. The line colours correspond to the cases listed in table 1.

Figure 6

Figure 6. Figure 6 long description.Causal maps for the demodulated inner and outer motions at y+=15$y^+=15$: (a) TE, (b) IF, and (c) SURD. Yellow boxes: inter-scale causalities. Cyan boxes: intra-scale causalities. Red boxes: causalities identified by both TE and IF.

Figure 7

Figure 7. Causal maps for the demodulated inner and outer motions at y+=70$y^+=70$: (a) TE, (b) IF, and (c) SURD. Yellow boxes: inter-scale causalities. Cyan boxes: intra-scale causalities. Red boxes: causalities identified by both TE and IF.

Figure 8

Figure 8. Figure 8 long description.Two-point causal maps for the inner and outer motions at y+=15$y^+=15$ and y+=200$y^+=200$: (a) TE, (b) IF, and (c) SURD. Yellow boxes: causalities between the two heights. Green boxes: causalities at the same height.

Figure 9

Figure 9. Two-point causal maps for the inner and outer motions at y+=70$y^+=70$ and y+=200$y^+=200$: (a) TE, (b) IF, and (c) SURD. Yellow boxes: causalities between the two heights. Green boxes: causalities at the same height.

Figure 10

Figure 10. Figure 10 long description.Schematic diagram of the causal links between inner and outer motions. Black arrows: the streak-vortex self-sustaining cycle of outer motions; blue arrows: the streak-vortex self-sustaining cycle of outer footprints; red arrows: the streak-vortex self-sustaining cycle of inner motions; green arrows: the bidirectional causalities of the outer motions and their near-wall footprints; brown arrows: the inner-pressure-related causal links; magenta arrows: the outer-pressure-related causal links; cyan arrow: the causal links between the inner and outer pressure.

Figure 11

Figure 11. Comparison of turbulence statistics of the present DNS with Lee & Moser (2015). (a) Mean streamwise flow velocity, (b) Reynolds normal and shear stresses.

Figure 12

Table 2. The mean absolute errors of the three methods with half of the dataset in temporal length.Table 2 long description.

Figure 13

Figure 12. Causal maps computed using (a,c)$(a,c)$ the complete dataset, and (b,d)$(b,d)$ half of the dataset in temporal length.

Figure 14

Figure 13. Figure 13 long description.Synergistic, unique and redundant decomposition computed using (a)$(a)$ the complete dataset, and (b)$(b)$ half of the dataset in temporal length.

Figure 15

Figure 14. Causal maps for the inner and outer motions at y+=15$y^+=15$: (a) TE, (b) IF, and (c) SURD. Yellow boxes: inter-scale causalities. Green boxes: intra-scale causalities. Red boxes: causalities identified by both TE and IF.

Figure 16

Figure 15. Figure 15 long description.Causal maps for the inner and outer motions at y+=70$y^+=70$: (a) TE, (b) IF, and (c) SURD. Yellow boxes: inter-scale causalities. Green boxes: intra-scale causalities. Red boxes: causalities identified by both TE and IF.

Figure 17

Figure 16. Causal maps for the square of the modulated inner motions and the outer motions at y+=15$y^+=15$: (a) TE, (b) IF, and (c) SURD. Yellow boxes: inter-scale causalities. Cyan boxes: intra-scale causalities. Red boxes: causalities identified by both TE and IF.

Figure 18

Figure 17. Causal maps for the square of the demodulated inner motions and the outer motions at y+=15$y^+=15$: (a) TE, (b) IF, and (c) SURD. Yellow boxes: inter-scale causalities. Cyan boxes: intra-scale causalities. Red boxes: causalities identified by both TE and IF.

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