Zheng Xingyu, Zeng Qingcun, Huang Ronghui. 1992: The Propagation of Inertia-Gravity Waves and Their Influence on Zonal Mean Flow Part Two: Wave Breaking and Critical Levels. Adv. Atmos. Sci, 9(1): 29-36., https://doi.org/10.1007/BF02656927
Citation:
Zheng Xingyu, Zeng Qingcun, Huang Ronghui. 1992: The Propagation of Inertia-Gravity Waves and Their Influence on Zonal Mean Flow Part Two: Wave Breaking and Critical Levels. Adv. Atmos. Sci, 9(1): 29-36., https://doi.org/10.1007/BF02656927
Zheng Xingyu, Zeng Qingcun, Huang Ronghui. 1992: The Propagation of Inertia-Gravity Waves and Their Influence on Zonal Mean Flow Part Two: Wave Breaking and Critical Levels. Adv. Atmos. Sci, 9(1): 29-36., https://doi.org/10.1007/BF02656927
Citation:
Zheng Xingyu, Zeng Qingcun, Huang Ronghui. 1992: The Propagation of Inertia-Gravity Waves and Their Influence on Zonal Mean Flow Part Two: Wave Breaking and Critical Levels. Adv. Atmos. Sci, 9(1): 29-36., https://doi.org/10.1007/BF02656927
The Propagation of Inertia-Gravity Waves and Their Influence on Zonal Mean Flow Part Two: Wave Breaking and Critical Levels
The gravity wave breaking is crucial to the large-scale circulation of middle atmosphere. In this paper, we follow Lindzen (1981) to draw out the parameterization of two-dimensional gravity wave breaking including inertial effect. Also we present some properties of critical levels and inertial critical levels.