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DOI10.5194/acp-22-11657-2022
Updated trends of the stratospheric ozone vertical distribution in the 60 degrees S-60 degrees N latitude range based on the LOTUS regression model
Godin-Beekmann, Sophie; Azouz, Niramson; Sofieva, Viktoria F.; Hubert, Daan; Petropavlovskikh, Irina; Effertz, Peter; Ancellet, Gerard; Degenstein, Doug A.; Zawada, Daniel; Froidevaux, Lucien; Frith, Stacey; Wild, Jeannette; Davis, Sean; Steinbrecht, Wolfgang; Leblanc, Thierry; Querel, Richard; Tourpali, Kleareti; Damadeo, Robert; Barras, Eliane Maillard; Stuebi, Rene; Vigouroux, Corinne; Arosio, Carlo; Nedoluha, Gerald; Boyd, Ian; Van Malderen, Roeland; Mahieu, Emmanuel; Smale, Dan; Sussmann, Ralf
发表日期2022
ISSN1680-7316
EISSN1680-7324
起始页码11657
结束页码11673
卷号22期号:17页码:17
英文摘要This study presents an updated evaluation of stratospheric ozone profile trends in the 60 degrees S-60 degrees N latitude range over the 2000-2020 period using an updated version of the Long-term Ozone Trends and Uncertainties in the Stratosphere (LOTUS) regression model that was used to evaluate such trends up to 2016 for the last WMO Ozone Assessment (2018). In addition to the derivation of detailed trends as a function of latitude and vertical coordinates, the regressions are performed with the datasets averaged over broad latitude bands, i.e. 60-35 degrees S, 20 degrees S-20 degrees N and 35-60 degrees N. The same methodology as in the last assessment is applied to combine trends in these broad latitude bands in order to compare the results with the previous studies. Longitudinally resolved merged satellite records are also considered in order to provide a better comparison with trends retrieved from ground-based records, e.g. lidar, ozonesondes, Umkehr, microwave and Fourier transform infrared (FTIR) spectrometers at selected stations where long-term time series are available. The study includes a comparison with trends derived from the REF-C2 simulations of the Chemistry Climate Model Initiative (CCMI-1). This work confirms past results showing an ozone increase in the upper stratosphere, which is now significant in the three broad latitude bands. The increase is largest in the Northern and Southern Hemisphere midlatitudes, with similar to 2.2 +/- 0.7 % per decade at similar to 2.1 hPa and similar to 2.1 +/- 0.6 % per decade at similar to 3.2 hPa respectively compared to similar to 1.6 +/- 0.6 % per decade at similar to 2.6 hPa in the tropics. New trend signals have emerged from the records, such as a significant decrease in ozone in the tropics around 35 hPa and a non-significant increase in ozone in the southern midlatitudes at about 20 hPa. Non-significant negative ozone trends are derived in the lowermost stratosphere, with the most pronounced trends in the tropics. While a very good agreement is obtained between trends from merged satellite records and the CCMI-1 REF-C2 simulation in the upper stratosphere, observed negative trends in the lower stratosphere are not reproduced by models at southern and, in particular, at northern midlatitudes, where models report an ozone increase. However, the lower-stratospheric trend uncertainties are quite large, for both measured and modelled trends. Finally, 2000-2020 stratospheric ozone trends derived from the ground-based and longitudinally resolved satellite records are in reasonable agreement over the European Alpine and tropical regions, while at the Lauder station in the Southern Hemisphere midlatitudes they show some differences.
学科领域Environmental Sciences; Meteorology & Atmospheric Sciences
语种英语
WOS研究方向Environmental Sciences & Ecology ; Meteorology & Atmospheric Sciences
WOS记录号WOS:000851384500001
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/273636
作者单位Centre National de la Recherche Scientifique (CNRS); UDICE-French Research Universities; Sorbonne Universite; Universite Paris Saclay; Finnish Meteorological Institute; University of Colorado System; University of Colorado Boulder; University of Saskatchewan; California Institute of Technology; National Aeronautics & Space Administration (NASA); NASA Jet Propulsion Laboratory (JPL); National Aeronautics & Space Administration (NASA); NASA Goddard Space Flight Center; National Oceanic Atmospheric Admin (NOAA) - USA; National Oceanic Atmospheric Admin (NOAA) - USA; California Institute of Technology; National Aeronautics & Space Administration (NASA); NASA Jet Propulsion Laboratory (JPL); National Institute of Water & Atmospheric Research (NIWA) - New Zealand; Aristotle University of Thessaloniki; National Aeronautics & Space Administration (NASA); NASA Langley Research Center; Federal Office of Meteorology & Climatology (MeteoSwiss); University of Bremen; United States Department of Defense; United States ...
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Godin-Beekmann, Sophie,Azouz, Niramson,Sofieva, Viktoria F.,et al. Updated trends of the stratospheric ozone vertical distribution in the 60 degrees S-60 degrees N latitude range based on the LOTUS regression model[J],2022,22(17):17.
APA Godin-Beekmann, Sophie.,Azouz, Niramson.,Sofieva, Viktoria F..,Hubert, Daan.,Petropavlovskikh, Irina.,...&Sussmann, Ralf.(2022).Updated trends of the stratospheric ozone vertical distribution in the 60 degrees S-60 degrees N latitude range based on the LOTUS regression model.ATMOSPHERIC CHEMISTRY AND PHYSICS,22(17),17.
MLA Godin-Beekmann, Sophie,et al."Updated trends of the stratospheric ozone vertical distribution in the 60 degrees S-60 degrees N latitude range based on the LOTUS regression model".ATMOSPHERIC CHEMISTRY AND PHYSICS 22.17(2022):17.
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