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Intercomparison of long-term ground-based measurements of tropospheric and stratospheric ozone at Lauder, New Zealand (45S)
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dc.contributor.authorBjörklund, Robines_ES
dc.contributor.authorVigouroux, Corinnees_ES
dc.contributor.authorEffertz, Peteres_ES
dc.contributor.authorGarcía Rodríguez, Omaira Elenaes_ES
dc.contributor.authorGeddes, Alexes_ES
dc.contributor.authorHannigan, James W.es_ES
dc.contributor.authorMiyagawa, Kojies_ES
dc.contributor.authorKotkamp, Michaeles_ES
dc.contributor.authorLangerock, Bavoes_ES
dc.contributor.authorNedoluha, Geraldes_ES
dc.contributor.authorOrtega, Ivanes_ES
dc.contributor.authorPetropavlovskikh, Irinaes_ES
dc.contributor.authorPoyraz, Denizes_ES
dc.contributor.authorQuerel, Richardes_ES
dc.contributor.authorRobinson, Johnes_ES
dc.contributor.authorShiona, Hisakoes_ES
dc.contributor.authorSmale, Danes_ES
dc.contributor.authorSmale, Pennyes_ES
dc.contributor.authorVan Malderen, Roelandes_ES
dc.contributor.authorDe Mazière, Martinees_ES
dc.date.accessioned2024-01-22T07:38:25Z-
dc.date.available2024-01-22T07:38:25Z-
dc.date.issued2023-
dc.identifier.citationEGUsphere. 2023, p. 1-38es_ES
dc.identifier.urihttp://hdl.handle.net/20.500.11765/15373-
dc.description.abstractLong-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.es_ES
dc.language.isoenges_ES
dc.publisherCopernicus Publicationses_ES
dc.rightsLicencia CC: Reconocimiento CC BYes_ES
dc.subjectOzone measurementses_ES
dc.subjectStratospheric ozonees_ES
dc.subjectTropospheric ozonees_ES
dc.subjectClimate changees_ES
dc.subjectGreenhouse gaseses_ES
dc.titleIntercomparison of long-term ground-based measurements of tropospheric and stratospheric ozone at Lauder, New Zealand (45S)es_ES
dc.typeinfo:eu-repo/semantics/preprintes_ES
dc.relation.publisherversionhttps://doi.org/10.5194/egusphere-2023-2668es_ES
dc.rights.accessRightsinfo:eu-repo/semantics/openAccesses_ES
Colecciones: Artículos científicos 2000-2004


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