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Intercomparison of long-term ground-based measurements of tropospheric and stratospheric ozone at Lauder, New Zealand (45S)
Título : Intercomparison of long-term ground-based measurements of tropospheric and stratospheric ozone at Lauder, New Zealand (45S)
Autor : Björklund, RobinVigouroux, CorinneEffertz, PeterGarcía Rodríguez, Omaira Elena ORCID RESEARCHERID Autor AEMETGeddes, AlexHannigan, James W.Miyagawa, KojiKotkamp, MichaelLangerock, BavoNedoluha, GeraldOrtega, IvanPetropavlovskikh, IrinaPoyraz, DenizQuerel, RichardRobinson, JohnShiona, HisakoSmale, DanSmale, PennyVan Malderen, RoelandDe Mazière, Martine
Palabras clave : Ozone measurements; Stratospheric ozone; Tropospheric ozone; Climate change; Greenhouse gases
Fecha de publicación : 2023
Editor: Copernicus Publications
Citación : EGUsphere. 2023, p. 1-38
Versión del editor: https://doi.org/10.5194/egusphere-2023-2668
Resumen : Long-term ground-based ozone measurements are crucial to study the recovery of stratospheric ozone as well as the trends of tropospheric ozone. This study is performed in the context of the LOTUS (Long-term Ozone Trends and Uncertainties in the Stratosphere) and TOAR-II (Tropospheric Ozone Assessment Report, phase II) initiatives. We perform an intercomparison study of total column ozone and multiple partial ozone columns between the ground-based measurements available at the Lauder station from 2000 to 2022, which are the Fourier transform infrared (FTIR) spectrometer, Dobson Umkehr, ozonesonde, lidar, and the microwave radiometer. We compare partial columns, defined to provide independent information: one tropospheric and three stratospheric columns. The intercomparison is analyzed using the median of relative differences (the bias) of FTIR with each of the other measurements, the scaled Median Absolute deviation (MADs), and a trend of these differences (measurement drift). The total column shows a bias and strong scatter well within the combined systematic and random uncertainties respectively. There is however a drift of 0.6±0.5 %/decade if we consider the full time series. In the troposphere we find a low bias of -1.9 % with the ozonesondes. No drift is found between the three instruments in the troposphere, which is good for trend studies within TOAR-II. In both the lower and upper stratosphere, we get a negative bias for all instruments with respect to FTIR (between -1.2 % and -6.8 %), but all are within the range of the systematic uncertainties.
URI : http://hdl.handle.net/20.500.11765/15373
Colecciones: Artículos científicos 2000-2004


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