气候变化领域集成服务门户(CCPortal): Local and remote response of ozone to Arctic stratospheric circulation extremes

CCPortal

DOI	10.5194/acp-21-1159-2021
	Local and remote response of ozone to Arctic stratospheric circulation extremes
	Hong H.-J.; Reichler T.
发表日期	2021
ISSN	1680-7316
起始页码	1159
结束页码	1171
卷号	21 期号:2
英文摘要	Intense natural circulation variability associated with stratospheric sudden warmings, vortex intensifications, and final warmings is a typical feature of the winter Arctic stratosphere. The attendant changes in transport, mixing, and temperature create pronounced perturbations in stratospheric ozone. Understanding these perturbations is important because of their potential feedbacks with the circulation and because ozone is a key trace gas of the stratosphere. Here, we use Modern-Era Retrospective analysis for Research and Applications, version 2 (MERRA-2), reanalysis to contrast the typical spatiotemporal structure of ozone during sudden warming and vortex intensification events. We examine the changes of ozone in both the Arctic and the tropics, document the underlying dynamical mechanisms for the observed changes, and analyze the entire life cycle of the stratospheric events - from the event onset in midwinter to the final warming in early spring. Over the Arctic and during sudden warmings, ozone undergoes a rapid and long-lasting increase of up to 1/4 50 DU, which only gradually decays to climatology before the final warming. In contrast, vortex intensifications are passive events, associated with gradual decreases in Arctic ozone that reach g1/4 40 DU during late winter and decay thereafter. The persistent loss in Arctic ozone during vortex intensifications is dramatically compensated by sudden warming-like increases after the final warming. In the tropics, the changes in ozone from Arctic circulation events are obscured by the influences from the quasi-biennial oscillation. After controlling for this effect, small but coherent reductions in tropical ozone can be seen during the onset of sudden warmings (1/4 2.5 DU) and also during the final warmings that follow vortex intensifications (1/4 2 DU). Our results demonstrate that Arctic circulation extremes have significant local and remote influences on the distribution of stratospheric ozone. © 2021 Georg Thieme Verlag. All rights reserved.
语种	英语
来源期刊	Atmospheric Chemistry and Physics
文献类型	期刊论文
条目标识符	http://gcip.llas.ac.cn/handle/2XKMVOVA/168803
作者单位	Department of Atmospheric Sciences, University of Utah, Salt Lake City, UT 84112, United States; Research Center for Environmental Changes, Academia Sinica, Taipei City, 11529, Taiwan
推荐引用方式 GB/T 7714	Hong H.-J.,Reichler T.. Local and remote response of ozone to Arctic stratospheric circulation extremes[J],2021,21(2).
APA	Hong H.-J.,&Reichler T..(2021).Local and remote response of ozone to Arctic stratospheric circulation extremes.Atmospheric Chemistry and Physics,21(2).
MLA	Hong H.-J.,et al."Local and remote response of ozone to Arctic stratospheric circulation extremes".Atmospheric Chemistry and Physics 21.2(2021).