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DOI10.5194/acp-20-9771-2020
Investigating stratospheric changes between 2009 and 2018 with halogenated trace gas data from aircraft, AirCores, and a global model focusing on CFC-11
Laube J.C.; Elvidge E.C.L.; Adcock K.E.; Baier B.; Brenninkmeijer C.A.M.; Chen H.; Droste E.S.; Grooß J.-U.; Heikkinen P.; Hind A.J.; Kivi R.; Lojko A.; Montzka S.A.; Oram D.E.; Randall S.; Röckmann T.; Sturges W.T.; Sweeney C.; Thomas M.; Tuffnell E.; Ploeger F.
发表日期2020
ISSN16807316
起始页码9771
结束页码9782
卷号20期号:16
英文摘要We present new observations of trace gases in the stratosphere based on a cost-effective sampling technique that can access much higher altitudes than aircraft. The further development of this method now provides detection of species with abundances in the parts per trillion (ppt) range and below. We obtain mixing ratios for six gases (CFC-11, CFC-12, HCFC-22, H-1211, H-1301, and SF6), all of which are important for understanding stratospheric ozone depletion and circulation. After demonstrating the quality of the data through comparisons with ground-based records and aircraft-based observations, we combine them with the latter to demonstrate its potential. We first compare the data with results from a global model driven by three widely used meteorological reanalyses. Secondly, we focus on CFC-11 as recent evidence has indicated renewed atmospheric emissions of that species relevant on a global scale. Because the stratosphere represents the main sink region for CFC-11, potential changes in stratospheric circulation and troposphere-stratosphere exchange fluxes have been identified as the largest source of uncertainty for the accurate quantification of such emissions. Our observations span over a decade (up until 2018) and therefore cover the period of the slowdown of CFC-11 global mixing ratio decreases measured at the Earth's surface. The spatial and temporal coverage of the observations is insufficient for a global quantitative analysis, but we do find some trends that are in contrast with expectations, indicating that the stratosphere may have contributed to the slower concentration decline in recent years. Further investigating the reanalysis-driven model data, we find that the dynamical changes in the stratosphere required to explain the apparent change in tropospheric CFC-11 emissions after 2013 are possible but with a very high uncertainty range. This is partly caused by the high variability of mass flux from the stratosphere to the troposphere, especially at timescales of a few years, and partly by large differences between runs driven by different reanalysis products, none of which agree with our observations well enough for such a quantitative analysis. © 2020 Author(s).
语种英语
scopus关键词airborne survey; altitude; atmospheric chemistry; atmospheric modeling; data processing; halogen; mixing ratio; sampling; stratosphere; trace gas
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/152866
作者单位Institute of Energy and Climate Research: Stratosphere, Jülich Research Centre, Jülich, 52428, Germany; School of Environmental Sciences, University of East Anglia, Norwich, NR4 7TJ, United Kingdom; Faculty of Science, University of East Anglia, Norwich Research Park, Norwich, NR4 7TJ, United Kingdom; Cooperative Institute for Research in Environmental Sciences, University of Colorado Boulder, Boulder, CO 80309, United States; Global Monitoring Division, National Oceanic and Atmospheric Administration, Boulder, CO 80305-3337, United States; Air Chemistry Division, Max Planck Institute for Chemistry, Mainz, 55128, Germany; Centre for Isotope Research, University of Groningen, Groningen, 9747 AG, Netherlands; Space and Earth Observation Centre, Finnish Meteorological Institute, Sodankylä, 99600, Finland; Department of Climate and Space Sciences and Engineering, University of Michigan, Ann Arbor, MI 48109-2143, United States; Random Engineering Ltd., Felixstowe, IP11 9SL, United Kingdom; Institute for Mar...
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Laube J.C.,Elvidge E.C.L.,Adcock K.E.,et al. Investigating stratospheric changes between 2009 and 2018 with halogenated trace gas data from aircraft, AirCores, and a global model focusing on CFC-11[J],2020,20(16).
APA Laube J.C..,Elvidge E.C.L..,Adcock K.E..,Baier B..,Brenninkmeijer C.A.M..,...&Ploeger F..(2020).Investigating stratospheric changes between 2009 and 2018 with halogenated trace gas data from aircraft, AirCores, and a global model focusing on CFC-11.Atmospheric Chemistry and Physics,20(16).
MLA Laube J.C.,et al."Investigating stratospheric changes between 2009 and 2018 with halogenated trace gas data from aircraft, AirCores, and a global model focusing on CFC-11".Atmospheric Chemistry and Physics 20.16(2020).
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