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.
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.
应用推荐