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.
全球气候变迁的驱动力主要来自于温室气体的增温效应，以及大气中气溶胶的降温效应。
The force of global climate variance mainly comes from greenhouse gases and aerosols in the atmosphere.
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