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• W2769912530 endingPage "6885" @default.
• W2769912530 startingPage "6867" @default.
• W2769912530 abstract "Abstract. In this study, we describe the recent changes in the tropospheric ozone (O3) columns measured by the Infrared Atmospheric Sounding Interferometer (IASI), onboard the Metop satellite, during the first 9 years of operation (January 2008 to May 2017). Using appropriate multivariate regression methods, we differentiate significant linear trends from other sources of O3 variations captured by IASI. The geographical patterns of the adjusted O3 trends are provided and discussed on the global scale. Given the large contribution of the natural variability in comparison with that of the trend (25–85 % vs. 15–50 %, respectively) to the total O3 variations, we estimate that additional years of IASI measurements are generally required to detect the estimated O3 trends with high precision. Globally, additional 6 months to 6 years of measurements, depending on the regions and the seasons, are needed to detect a trend of |5| DU decade−1. An exception is interestingly found during summer at mid- and high latitudes of the Northern Hemisphere (NH; ∼ 40 to ∼ 75∘ N), where the large absolute fitted trend values (∼ |0.5| DU yr−1 on average) combined with the small model residuals (∼ 10 %) allow for detection of a band-like pattern of significant negative trends. Despite no consensus in terms of tropospheric O3 trends having been reached from the available independent datasets (UV or IR satellites, O3 sondes, aircrafts, ground-based measurements, etc.) for the reasons that are discussed in the text, this finding is consistent with the reported decrease in O3 precursor emissions in recent years, especially in Europe and USA. The influence of continental pollution on that latitudinal band is further investigated and supported by the analysis of the O3–CO relationship (in terms of correlation coefficient, regression slope and covariance) that we found to be the strongest at northern midlatitudes in summer." @default.
• W2769912530 created "2017-12-04" @default.
• W2769912530 creator A5051970828 @default.
• W2769912530 creator A5052607964 @default.
• W2769912530 creator A5063875021 @default.
• W2769912530 creator A5072898737 @default.
• W2769912530 creator A5084185905 @default.
• W2769912530 date "2018-05-16" @default.
• W2769912530 modified "2023-10-01" @default.
• W2769912530 title "Decrease in tropospheric O&lt;sub&gt;3&lt;/sub&gt; levels in the Northern Hemisphere observed by IASI" @default.
• W2769912530 cites W1486615783 @default.
• W2769912530 cites W1833367443 @default.
• W2769912530 cites W1893343990 @default.
• W2769912530 cites W1903012642 @default.
• W2769912530 cites W1904230536 @default.
• W2769912530 cites W1969834329 @default.
• W2769912530 cites W1974427727 @default.
• W2769912530 cites W1974531400 @default.
• W2769912530 cites W1977531954 @default.
• W2769912530 cites W1979559580 @default.
• W2769912530 cites W1980223945 @default.
• W2769912530 cites W1982462510 @default.
• W2769912530 cites W1985794946 @default.
• W2769912530 cites W1989518161 @default.
• W2769912530 cites W1992450374 @default.
• W2769912530 cites W1992739954 @default.
• W2769912530 cites W1995801694 @default.
• W2769912530 cites W1998504943 @default.
• W2769912530 cites W2003403930 @default.
• W2769912530 cites W2004012328 @default.
• W2769912530 cites W2004136630 @default.
• W2769912530 cites W2004545547 @default.
• W2769912530 cites W2010654938 @default.
• W2769912530 cites W2011560911 @default.
• W2769912530 cites W2013167968 @default.
• W2769912530 cites W2013214260 @default.
• W2769912530 cites W2020100832 @default.
• W2769912530 cites W2026653324 @default.
• W2769912530 cites W2029211844 @default.
• W2769912530 cites W2032394154 @default.
• W2769912530 cites W2039665048 @default.
• W2769912530 cites W2041040655 @default.
• W2769912530 cites W2042187188 @default.
• W2769912530 cites W2046456896 @default.
• W2769912530 cites W2051992917 @default.
• W2769912530 cites W2055956082 @default.
• W2769912530 cites W2059006576 @default.
• W2769912530 cites W2059613035 @default.
• W2769912530 cites W2066431185 @default.
• W2769912530 cites W2066801828 @default.
• W2769912530 cites W2068774847 @default.
• W2769912530 cites W2073858030 @default.
• W2769912530 cites W2077314447 @default.
• W2769912530 cites W2083426098 @default.
• W2769912530 cites W2086099556 @default.
• W2769912530 cites W2087564723 @default.
• W2769912530 cites W2087789121 @default.
• W2769912530 cites W2094753333 @default.
• W2769912530 cites W2095431680 @default.
• W2769912530 cites W2103798415 @default.
• W2769912530 cites W2104758502 @default.
• W2769912530 cites W2105641924 @default.
• W2769912530 cites W2106820951 @default.
• W2769912530 cites W2118418063 @default.
• W2769912530 cites W2119735267 @default.
• W2769912530 cites W2128346119 @default.
• W2769912530 cites W2131240411 @default.
• W2769912530 cites W2133258543 @default.
• W2769912530 cites W2147522776 @default.
• W2769912530 cites W2148402338 @default.
• W2769912530 cites W2150287339 @default.
• W2769912530 cites W2154154220 @default.
• W2769912530 cites W2158466662 @default.
• W2769912530 cites W2160797250 @default.
• W2769912530 cites W2163894499 @default.
• W2769912530 cites W2164367741 @default.
• W2769912530 cites W2172097513 @default.
• W2769912530 cites W2202013945 @default.
• W2769912530 cites W2258429575 @default.
• W2769912530 cites W2283763499 @default.
• W2769912530 cites W2288934437 @default.
• W2769912530 cites W2302543561 @default.
• W2769912530 cites W2319404411 @default.
• W2769912530 cites W2409430606 @default.
• W2769912530 cites W2412212965 @default.
• W2769912530 cites W2471279947 @default.
• W2769912530 cites W2546518786 @default.
• W2769912530 cites W2585089065 @default.
• W2769912530 cites W2593839703 @default.
• W2769912530 cites W2610784301 @default.
• W2769912530 cites W2754107707 @default.
• W2769912530 cites W2761324230 @default.
• W2769912530 cites W2803010032 @default.
• W2769912530 cites W4232816666 @default.
• W2769912530 cites W4233644157 @default.
• W2769912530 cites W4240733927 @default.
• W2769912530 cites W4249135785 @default.
• W2769912530 doi "https://doi.org/10.5194/acp-18-6867-2018" @default.

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