The use of QBO, ENSO, and NAO perturbations in the evaluation of GOME-2 MetOp A total ozone measurements

In this work we present evidence that quasi-cyclical perturbations in total ozone (quasi-biennial oscillation – QBO, El Niño–Southern Oscillation – ENSO, and North Atlantic Oscillation – NAO) can be used as independent proxies in evaluating Global Ozone Monitoring Experiment (GOME) 2 aboard MetOp A...

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Bibliographic Details
Published in:Atmospheric Measurement Techniques
Main Authors: K. Eleftheratos, C. S. Zerefos, D. S. Balis, M.-E. Koukouli, J. Kapsomenakis, D. G. Loyola, P. Valks, M. Coldewey-Egbers, C. Lerot, S. M. Frith, A. S. Haslerud, I. S. A. Isaksen, S. Hassinen
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2019
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Online Access:https://doi.org/10.5194/amt-12-987-2019
https://doaj.org/article/74f551669bc341259df1920038d17bf2
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Summary:In this work we present evidence that quasi-cyclical perturbations in total ozone (quasi-biennial oscillation – QBO, El Niño–Southern Oscillation – ENSO, and North Atlantic Oscillation – NAO) can be used as independent proxies in evaluating Global Ozone Monitoring Experiment (GOME) 2 aboard MetOp A (GOME-2A) satellite total ozone data, using ground-based (GB) measurements, other satellite data, and chemical transport model calculations. The analysis is performed in the frame of the validation strategy on longer time scales within the European Organisation for the Exploitation of Meteorological Satellites (EUMETSAT) Satellite Application Facility on Atmospheric Composition Monitoring (AC SAF) project, covering the period 2007–2016. Comparison of GOME-2A total ozone with ground observations shows mean differences of about <math xmlns="http://www.w3.org/1998/Math/MathML" id="M1" display="inline" overflow="scroll" dspmath="mathml"><mrow><mo>-</mo><mn mathvariant="normal">0.7</mn><mo>±</mo><mn mathvariant="normal">1.4</mn></mrow></math> <svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="52pt" height="10pt" class="svg-formula" dspmath="mathimg" md5hash="dba8c66e297c0601baccc6ab115a0086"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="amt-12-987-2019-ie00001.svg" width="52pt" height="10pt" src="amt-12-987-2019-ie00001.png"/></svg:svg> % in the tropics (0–30 ∘ ), about <math xmlns="http://www.w3.org/1998/Math/MathML" id="M3" display="inline" overflow="scroll" dspmath="mathml"><mrow><mo>+</mo><mn mathvariant="normal">0.1</mn><mo>±</mo><mn mathvariant="normal">2.1</mn></mrow></math> <svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="52pt" height="10pt" class="svg-formula" dspmath="mathimg" md5hash="63d75ddfa7d430e7ceb7a4033cb0075f"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="amt-12-987-2019-ie00002.svg" ...