Figure 2. Antarctic
Total Ozone of 2016 (left) and 2017 (right) (Source: NASA).
NASA announced that the reason for the smaller ozone hole this year was resulted from the warmer vortex over the Antarctic. The Antarctic vortex is a low-lying, low-pressure region rotating clockwise over the Antarctic. However, since the depletion of ozone occurs in cold environment (for a reference to previous blogs), the ozone hole reaches its annual maximum in September or October at the end of the southern hemisphere winter. This year, however, the system is warmer and more unstable than usual and contributes to reducing clouds in the lower stratosphere which is formed during the Antarctic winter. When the temperature drops below -78 degrees, nitric acid or sulfuric acid particles adsorb water droplets to form larger particles, resulting in large-scale polar stratospheric clouds. These clouds store ozone-depleting substances such as chlorine and bromine (Rowland, 1996). When Antarctic spring comes, the ozone depletion in these clouds will consume a large amount of ozone under UV catalysis. Thus, the warmer stratosphere this year weakened the formation of stratospheric clouds and, as a result, reduced ozone depletion.
Scientists expect that around 2070, the Antarctic ozone hole may recover to 1980
levels .
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