| 1. | Evolution and structures of meiyu - front during the secondary meiyu - season in
1998年二度梅雨锋的演变及结构特征 |
| 2. | Simulation study of three - dimensional airflow structure of mesovortexes along meiyu front
梅雨锋低涡系统三维流场结构的分析 |
| 3. | The meso - scale systems are the direct influencial systems of the meiyu frontal rainstorm
中尺度系统是梅雨锋暴雨发生发展的直接影响系统。 |
| 4. | Meso - and - - scale structure of heavy rain on meiyu front detected by dual - doppler radar
梅雨锋暴雨中尺度对流系统结构模型的双多普勒雷达研究 |
| 5. | Numerical study on the genesis and development of the low vortex - rain gush system on a jianghuai meiyu front
江淮梅雨锋强暴雨低涡系统发生发展的数值研究 |
| 6. | The effect of model horizontal resolution on quantitative precipitation forecast for meiyu front torrential rainfall
模式水平分辨率对梅雨锋降水定量预报的影响 |
| 7. | Diagnostic analysis and numerical simulation of the meso - scale system during quot; 03 . 7 quot; meiyu frontal rainstorm event
江淮梅雨锋暴雨中尺度系统的数值模拟研究 |
| 8. | Only above soohpa , the mei - yu front is similar when we use the two ways to analysis
在500hpa以上，用假相当位温确定的梅雨锋区与用温度场确定的梅雨锋区才较为一致。 |
| 9. | Mei - yu front and low along yangtze river is an important and difficult event for meteorologists of china
长江流域的梅雨锋及梅雨锋中的低涡一直是我国气象工作者关心和研究的重点和难点。 |
| 10. | In fact , the subtropical high affects the position of the meiyu cloud system so that the region of heavy rainfall determined
副热带高压决定梅雨锋云系的位置，因此也决定了暴雨发生的区域。 |
