平流层臭氧损耗由于空气污染一向被认为是威胁人类健康以及地球的生态系统。
Stratospheric ozone depletion due to air pollution has long been recognized as a threat to human health as well as to the Earth's ecosystems.
因此,向平流层添加硫酸雾很可能会导致臭氧的损耗,从而使更多的紫外线穿过大气层。
It is therefore likely that the addition of sulphate to the stratosphere would result in a loss of ozone, and thus in more ultraviolet radiation getting through.
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.
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