| 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. | Statistical features of tropopause over qinghai province
青海省对流层顶若干统计特征 |
| 3. | 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 |
| 4. | 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 |
| 5. | As soon as the tropopause is reached , temperature stops decreasing with height
一达到对流层，温度就停止随高度上升。 |
| 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. | Wet and dry numerical simulation tests for explosive cyclone over western pacific were performed . by contrast the results show that : tropopause and constant temperature surface were raised by latent heat release in upper level and disturbance trough was produced because air flow ascended and became cold . owing to this process adaption , inertial instability emergenced
对气旋强烈爆发的过程进行干湿对比数值模拟试验，得出：潜热释放使对流层项和等温面抬高，气流在高层的上升冷却形成扰动槽，其适应过程使高层出现惯性不稳定。 |
| 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。 |
