Next comes the tropopause, which is the upper boundary of the troposphere.
其上是對流層頂, 它是對流層的上部邊界.
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As soon as the tropopause is reached, temperature stops decreasing with height.
一達到對流層, 溫度就停止隨高度上升.
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Convective generation of cirrus near the tropopause.
對流層頂附近的對流產生的云.
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