| 1. | The balance must be made up by heat transport through the tropopause .
必须通过对流层顶的热输送来建立平衡。 |
| 2. | The balance must be made up by heat transported through the troposphere .
必须通过对流层顶的热输送来建立平衡。 |
| 3. | Statistical features of tropopause over qinghai province
青海省对流层顶若干统计特征 |
| 4. | Statistics of the global tropopause temperature change
全球对流层顶温度场演变的气候学特征分析 |
| 5. | The variation of spatial - temporal distribution of the global tropopause ozone
大气对流层顶的臭氧时空分布变化 |
| 6. | 3 . synoptic meteorology : the general circulation ; air masses ; fronts ; tropopause ; jet stream ; fog ; local winds ; severe local storms
3 .天气学：大气环流气团锋对流层顶急流雾地方性风强烈地方性风暴。 |
| 7. | Radiative forcing is defined as a change in average net radiation at the top of the troposphere tropopause due to a change in either solar or infrared radiation
辐射力的定义是由于太阳或红外线辐射份量的转变而引致对流层顶部的平均辐射改变。 |
| 8. | Radiative forcing is defined as a change in average net radiation at the top of the troposphere ( tropopause ) due to a change in either solar or infrared radiation
辐射力的定义是由于太阳或红外线辐射份量的转变而引致对流层顶部的平均辐射改变。 |
| 9. | The analysis of dry pv shows that the high pv dominate the area of typhoon , the higher is the center value of pv , the stronger is the typhoon . lt is also shown that the most important reason resulting in rainstorm is the cold air ( high pv ) which spreads to south from the upper troposphere or lower stratosphere and transports into the warm air . the joining situation of upper and lower pv area make vortex develop . pv transpotation reduces static stability , which increases the releasing of instability energy and makes rainstorm amplify
对干位涡的分析表明：台风或台风环流区为高值位涡区，台风越强，位涡中心值越大；对流层上部或平流层下部冷空气(高位涡)的扩散南下与暖湿气流的交汇是造成特大暴雨的重要原因，因为上游斜压性的发展使对流层顶发生折叠，平流层与对流层相互作用增强，上下位涡区相接的形势使低层涡旋发展，上升运动加强，位涡的下传有效地降低了静力稳定度，有利于位势不稳定能量的释放，使得暴雨增幅。 |
| 10. | 3 in the years of cold spring , the inner mongolia high and the aliushen low are strengthened with the low index of the east asia trough and the negative anomaly center of temperature over northeast china from surface to tropopause while the contrary conditions occur in the years of warm spring
3 、东北地区出现春季低温的主要环流特征是：内蒙古高压，阿留申低压的强度加强；阿流申低压指数以及东亚大槽强度指数减弱，东北地区从地面到对流层顶处在温度负距平中心内，东北地区春季高温时则出现与上面相反的变化形式。 |
