Evolution of observed ozone, trace gases, and meteorological variables over Arrival Heights, Antarctica (77.8°S, 166.7°E) during the 2019 Antarctic stratospheric sudden warming

D. Smale, S. Strahan, R. Querel, U. Friess, G. Nedoluha, S. Nichol, John Robinson, I. Boyd, M. Kotkamp, R. Gomez, M. Murphy, Hue Tran, Jamie McGaw
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引用次数: 4

Abstract

Abstract We use ground-based spectroscopic remote sensing measurements of the stratospheric trace gases O3, HCl, ClO, BrO, HNO3, NO2, OClO, ClONO2, N2O and HF, along with radiosonde profiles of temperature to track the springtime development of the 2019 ozone hole over Arrival Heights (77.8°S, 166.7°E, AHTS), Antarctica, during, and after, the 2019 stratospheric sudden warming (SSW) event. Both measurements and model simulations show that the 2019 SSW caused an extraordinarily warm stratosphere within the polar vortex, resulting in record low ozone depletion over AHTS. We also contrast the evolution of the 2019 ozone hole to that in 2002, which also had a major springtime SSW event. The SSW event started around 28th August. By ∼17th September, stratospheric temperatures inside the polar vortex over AHTS were ∼45 K higher than the climatological average. The SSW did not cause an en masse displacement of mid-latitude air over AHTS as in the 2002 SSW event. However, the increased temperatures did cause an unusually early reduction in polar stratospheric clouds, halting the denitrification early and leading to increased gas-phase HNO3 and record high levels of NO2 (‘renoxification’). This caused the earliest observed deactivation of chlorine, returning all active chlorine into the chlorine reservoir species, HCl and ClONO2. The deactivation rate into HCl remained relatively unaffected by the SSW, whilst there was a dramatic increase in ClONO2 formation. This chlorine deactivation pathway via ClONO2 is typical of the Arctic and atypical for the Antarctic. At AHTS, record high levels of springtime ozone were observed. The measured ozone total column did not drop below 220 DU. Record high stratospheric temperatures persisted until 7th October over AHTS. By 22nd October, AHTS was not beneath the polar vortex. The polar vortex break-up date on 9th November was one of the earliest observed.
2019年南极平流层突然变暖期间南极到达高地(77.8°S, 166.7°E)观测到的臭氧、微量气体和气象变量的演变
摘要利用地面光谱遥感测量平流层微量气体O3、HCl、ClO、BrO、HNO3、NO2、OClO、ClONO2、N2O和HF,并结合探空温度剖面图,追踪2019年平流层突然变暖(SSW)事件期间和之后到达高地(77.8°S, 166.7°E, AHTS)上空臭氧空洞的春季发展。测量和模型模拟都表明,2019年的SSW在极地涡旋内造成了异常温暖的平流层,导致AHTS上空的臭氧消耗创历史新低。我们还将2019年臭氧空洞的演变与2002年进行了对比,2002年也发生了一次重大的春季SSW事件。SSW活动于8月28日左右开始。到9月17日,AHTS上空极地涡旋内的平流层温度比气候平均温度高~ 45k。南南风并没有像2002年的南南风那样造成中纬度空气的大规模位移。然而,升高的温度确实导致极地平流层云层异常早地减少,提前停止了反硝化作用,导致气相HNO3增加和创纪录的高水平NO2(“再氧化”)。这引起了最早观察到的氯的失活,将所有活性氯返回到氯库物质HCl和ClONO2中。进入HCl的失活速率相对不受SSW的影响,而ClONO2的形成则急剧增加。这种通过ClONO2的氯失活途径在北极是典型的,在南极则是非典型的。在AHTS,观测到春季臭氧水平创历史新高。实测臭氧总柱未低于220 DU。创纪录的平流层高温一直持续到10月7日。到10月22日,AHTS已经不在极地涡旋之下。11月9日的极地涡旋破裂日期是最早观测到的日期之一。
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