蒋国荣. 1996. 热带大气的CISK-Rossby波和30-50天振荡[J]. 气象学报, 54(6):745-752, doi:10.11676/qxxb1996.077 |
热带大气的CISK-Rossby波和30-50天振荡 |
CISK-ROSSBY WAVES IN THE TROPICAL ATMOSPHERE AND 30-50 DAY OSCILLATION |
投稿时间:1995-04-13 修订日期:1995-09-18 |
DOI:10.11676/qxxb1996.077 |
中文关键词: 30-50d振荡 积云对流反馈 CISK-Rossby波 |
英文关键词:30-50 day oscillation Convection feedback CISK-Rossby wave |
基金项目:空司气象局资助 |
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中文摘要: |
利用斜压准地转滤波方法,通过引入一个反映CISK机制的无量纲凝结潜热参数η(Z),建立了描述热带大气的CISK-Rossby波模式,并求得了该模式的解析解。理论研究表明,考虑CISK机制的CISK-Rossby波与经典的Rossby波有明显差别,它可较好地解释热带大气30-50d振荡现象。 |
英文摘要: |
In terms of a baroclinic quasi-geostrophic wave-filtering technique and through introducing a dimensionless parameter.η(Z),of condensation-released heat that indicates the CISK mechanism.a model is established for describing tropical atmosphere CISK-Rossby waves.At the same time.the model's analytical solution has also been obtained.Theoretical study shows that there is pronounced difference between CISK-involving Rossby waves and classic Rossby waves.and CISK-Rossby waves can better interpret some aspects of 30-50 day oscillation in the tropical atmosphere. |
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