On the Rotation‐Induced Pressure‐Strain Correlation in Rotating Boundary Layer Flows

Abstract Rotation is a fundamental feature of many weather systems. The pressure‐strain correlation plays an important role in the Reynolds stress budget. However, the behavior of the pressure‐strain correlation under rotation remains insufficiently explored. This study develops a closure model for the rotation‐induced pressure‐strain correlation. In rotating boundary layers, quasi two‐dimensional turbulent eddies are identified as key contributors to modulating the magnitude of the pressure‐strain correlation. By involving the anisotropic characteristics of these eddies, the proposed model represents the rotation‐induced pressure‐strain correlation as a function of the turbulence Rossby number and the Reynolds stresses. Direct numerical simulations are performed to evaluate the performance of the closure model. The results show that our closure model is in good agreement with direct numerical simulations. These findings provide valuable insights for improving the representation of rotating boundary layers in weather and climate models.

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Publication Details

Journal
Geophysical Research Letters
Published
2026-01-22
DOI
https://doi.org/10.1029/2025gl118391
Primary Topic
Meteorological Phenomena and Simulations
Type
article
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article

On the Rotation‐Induced Pressure‐Strain Correlation in Rotating Boundary Layer Flows

Xin Shao, N. Zhang
Geophysical Research Letters
Meteorological Phenomena and Simulations
article

On the Rotation‐Induced Pressure‐Strain Correlation in Rotating Boundary Layer Flows

Xin Shao, N. Zhang
article en

Abstract

Abstract Rotation is a fundamental feature of many weather systems. The pressure‐strain correlation plays an important role in the Reynolds stress budget. However, the behavior of the pressure‐strain correlation under rotation remains insufficiently explored. This study develops a closure model for the rotation‐induced pressure‐strain correlation. In rotating boundary layers, quasi two‐dimensional turbulent eddies are identified as key contributors to modulating the magnitude of the pressure‐strain correlation. By involving the anisotropic characteristics of these eddies, the proposed model represents the rotation‐induced pressure‐strain correlation as a function of the turbulence Rossby number and the Reynolds stresses. Direct numerical simulations are performed to evaluate the performance of the closure model. The results show that our closure model is in good agreement with direct numerical simulations. These findings provide valuable insights for improving the representation of rotating boundary layers in weather and climate models.

Geophysical Research LettersVol. 53(2)
China Meteorological Administration (CN), Nanjing University of Information Science and Technology (CN)
Climate action
Openalex Percentile: Top 86%
Meteorological Phenomena and Simulations
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