Or it may be, as others have suggested in the past, that the long-term trend, as the troposphere warms up, will be to a wetter, more warming lower stratosphere, too.
也可能像前人建议的，当对流层温度升高，长期起来会形成一个湿度更大、温度更高、高度更低的平流层。
These mechanisms can largely explain occurring of abnormal circulation in the stratosphere and troposphere during stratospheric sudden warming and returning then to normal regime.
这些机制可以大致说明一些爆发性增温期间平流层和对流层大气环流出现异常以及随后又恢复到正常冬季环流的过程。
The zonal wind anomalies associated IOD are found to weaken, likely due to increased static stability of the troposphere from global warming.
这是由于全球变暖中对流层静力稳定度的增强，与IOD模态相关的纬向风异常减弱。
The warming is not due to direct radiative effect of ozone depletion, instead, it is throughout dynamic processes, such as wave-mean flow and stratosphere-troposphere interactions.
当然，这些增温并非是由臭氧损耗的辐射效应直接造成的，而是通过波-流相互作用以及平流层-对流层相互作用等动力学过程实现的。
The warming is not due to direct radiative effect of ozone depletion, instead, it is throughout dynamic processes, such as wave-mean flow and stratosphere-troposphere interactions.
当然，这些增温并非是由臭氧损耗的辐射效应直接造成的，而是通过波-流相互作用以及平流层-对流层相互作用等动力学过程实现的。
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