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Original Paper

Conservative Transport Using a Compact Third-Order Scheme on the Yin–Yang Grid

College of Aviation Meteorology, Civil Aviation Flight University of China, Guanghan 618307
CMA Earth System Modeling and Prediction Centre (CEMC), China Meteorological Administration (CMA), Beijing 100081
State Key Laboratory of Severe Weather Meteorological Science and Technology (LaSW), Chinese Academy of Meteorological Sciences, China Meteorological Administration, Beijing 100081
Zhejiang Key Laboratory of Environment and Health of New Pollutants, School of Environment, Hangzhou Institute for Advanced Study, University of Chinese Academy of Sciences, Hangzhou 310024
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Abstract

The Yin–Yang grid, while offering advantages such as quasi-uniformity and pole-singularity avoidance, inherently lacks global conservation owing to interpolation at grid boundaries. To address this problem, we proposed a compact flux correcting method to ensure conservation based on a third-order multimoment constrained finite volume scheme. Using the nine point values within each computational cell, a bivariate quadratic polynomial was constructed for high-fidelity boundary interpolation and flux reconstruction. Identical flux across the boundary of overlapped grids was enforced in the Yin and Yang components with the help of the polynomial. A third-order conservative advection scheme was therefore achieved on the Yin–Yang grid, effectively balancing numerical accuracy and computational efficiency. Several standard numerical tests were conducted to confirm the performance of the interpolation algorithm and the conservation calculation scheme. Results revealed that the high accuracy and the stability of the strict conservation scheme are helpful in passive transport situations on Yin–Yang grids.

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Journal of Meteorological Research
Pages 589-604

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Cite this article:
GU J, QIU Y, PENG X, et al. Conservative Transport Using a Compact Third-Order Scheme on the Yin–Yang Grid. Journal of Meteorological Research, 2026, 40(2): 589-604. https://doi.org/10.1007/s13351-026-5123-8

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Received: 16 May 2025
Revised: 30 October 2025
Accepted: 01 December 2025
Published: 18 April 2026
© The Chinese Meteorological Society 2026