On the modelled thermal response of the Antarctic stratosphere to a depletion of ozone
On the modelled thermal response of the Antarctic stratosphere to a depletion of ozone
复制标题
南极平流层对臭氧消耗的模拟热响应
DOI：
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发表时间：
1986
期刊：
影响因子：
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通讯作者：
K. Shine
中科院分区：
文献类型：
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作者：
K. Shine
简单的模型被用来调查春季南极臭氧消耗对平流层温度的影响。结果表明，冷却超过5 K是可能的，在较低的平流层。没有证据表明发生了这种变化。抵消这种冷却的一个可能机制是，由于极地平流层云层的干燥过程，平流层下部的水蒸气流失。
Simple models are used to investigate the effect of a spring-time depletion of ozone in the Antarctic on stratospheric temperatures. It is shown that coolings in excess of 5 K are possible in the lower stratosphere. No evidence for such changes exist. One possible mechanism that could offset this cooling involves the loss of water vapour from the lower stratosphere due to desiccation processes associated with polar stratospheric clouds.