The tropopause inversion layer in models and analyses
模式和分析对流层顶逆温层
Effects of cirrus near the tropopause on anvil cirrus dynamics
对流层顶附近卷云对砧状卷云动力学的影响
Radiation balance of the tropical tropopause layer
热带对流层顶层的辐射平衡
Next comes the tropopause, which is the upper boundary of the troposphere.
其上是对流层顶，它是对流层的上部边界。
Convective generation of cirrus near the tropopause.
对流层顶附近的对流产生的云。
Longitudinal variability of water vapor and cirrus in the tropical tropopause layer
热带对流层顶水汽和卷云的纬经向变化
Fluctuations of Cloud, Humidity, and Thermal Structure near the Tropical Tropopause.
热带对流层顶云、湿度和热结构的变化。
Distribution and influence of convection in the tropical tropopause region
热带对流层顶的对流分布和影响
Convective impact on temperatures observed near the tropical tropopause.
对流对热带对流层顶附近观测到的温度的作用。
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。
tropopause inversion.
对流层顶逆温
The whole tropical tropopause has been warmed up from cold period to warm period.
从偏冷期到偏暖期，整个热带对流层顶显著变暖。
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