对流层顶

The temperature at the tropopause generally decreases with altitude.
对流层顶的温度通常随海拔高度而降低。
The tropopause is the boundary between the troposphere and stratosphere.
对流层顶是平流层和对流层的分界线。
鸟类常常在靠近暖性气团的高处，接近 tropopause飞行。
Birds often fly near the warm air masses close to the tropopause.
The ozone layer is located in the lower part of the stratosphere, just above the tropopause.
臭氧层位于平流层的下部，就在对流层顶之上。
At mid-latitudes, the tropopause can be as high as 17 kilometers (10.5 miles).
在中纬度地区，对流层顶可以高达17公里（10.5英里）。
Slight changes in the tropopause height can have significant impacts on climate.
对流层顶高度的微小变化可能对气候产生重大影响。
Planes flying at cruising altitude usually stay below the tropopause for fuel efficiency.
为了燃油效率，巡航中的飞机通常保持在对流层顶以下飞行。
The tropopause can be disturbed by weather systems such as jet streams or intense storms.
对流层顶可能会受到高速气流或强烈风暴等天气系统的干扰。
Satellites orbiting Earth often pass through the region near the tropopause.
环绕地球运行的卫星经常穿过对流层顶附近的区域。
Climatologists study variations in the tropopause to better understand global warming trends.
气候学家研究对流层顶的变化，以便更好地理解全球变暖趋势。