气候变化领域集成服务门户(CCPortal): Stratospheric Ozone Changes From Explosive Tropical Volcanoes: Modeling and Ice Core Constraints

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DOI	10.1029/2019JD032290
	Stratospheric Ozone Changes From Explosive Tropical Volcanoes: Modeling and Ice Core Constraints
	Ming A.; Winton V.H.L.; Keeble J.; Abraham N.L.; Dalvi M.C.; Griffiths P.; Caillon N.; Jones A.E.; Mulvaney R.; Savarino J.; Frey M.M.; Yang X.
发表日期	2020
ISSN	2169897X
卷号	125 期号:11
英文摘要	Major tropical volcanic eruptions have emitted large quantities of stratospheric sulfate and are potential sources of stratospheric chlorine although this is less well constrained by observations. This study combines model and ice core analysis to investigate past changes in total column ozone. Historic eruptions are good analogs for future eruptions as stratospheric chlorine levels have been decreasing since the year 2000. We perturb the preindustrial atmosphere of a chemistry-climate model with high and low emissions of sulfate and chlorine. The sign of the resulting Antarctic ozone change is highly sensitive to the background stratospheric chlorine loading. In the first year, the response is dynamical, with ozone increases over Antarctica. In the high HCl (2 Tg emission) experiment, the injected chlorine is slowly transported to the polar regions with subsequent chemical ozone depletion. These model results are then compared to measurements of the stable nitrogen isotopic ratio, (Formula presented.), from a low snow accumulation Antarctic ice core from Dronning Maud Land (recovered in 2016–2017). We expect ozone depletion to lead to increased surface ultraviolet (UV) radiation, enhanced air-snow nitrate photochemistry and enrichment in (Formula presented.) in the ice core. We focus on the possible ozone depletion event that followed the largest volcanic eruption in the past 1,000 years, Samalas in 1257. The characteristic sulfate signal from this volcano is present in the ice core but the variability in (Formula presented.) dominates any signal arising from changes in ultraviolet from ozone depletion. Prolonged complete ozone removal following this eruption is unlikely to have occurred over Antarctica. ©2020. American Geophysical Union. All Rights Reserved.
英文关键词	Antarctica; chemistry-climate modeling; isotopes in ice cores; ozone; Samalas; volcanic eruption
语种	英语
来源期刊	Journal of Geophysical Research: Atmospheres
文献类型	期刊论文
条目标识符	http://gcip.llas.ac.cn/handle/2XKMVOVA/185987
作者单位	British Antarctic Survey, Cambridge, United Kingdom; Department of Chemistry, University of Cambridge, Cambridge, United Kingdom; National Centre for Atmospheric Science (NCAS), University of Cambridge, Cambridge, United Kingdom; Met Office Hadley Centre, Exeter, United Kingdom; Université Grenoble Alpes, CNRS, IRD, Grenoble INP, IGE, Grenoble, France
推荐引用方式 GB/T 7714	Ming A.,Winton V.H.L.,Keeble J.,et al. Stratospheric Ozone Changes From Explosive Tropical Volcanoes: Modeling and Ice Core Constraints[J],2020,125(11).
APA	Ming A..,Winton V.H.L..,Keeble J..,Abraham N.L..,Dalvi M.C..,...&Yang X..(2020).Stratospheric Ozone Changes From Explosive Tropical Volcanoes: Modeling and Ice Core Constraints.Journal of Geophysical Research: Atmospheres,125(11).
MLA	Ming A.,et al."Stratospheric Ozone Changes From Explosive Tropical Volcanoes: Modeling and Ice Core Constraints".Journal of Geophysical Research: Atmospheres 125.11(2020).