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- W4386997965 abstract "<strong class=journal-contentHeaderColor>Abstract.</strong> The assumption of nighttime ozone chemical equilibrium (NOCE) is widely used for retrieval of the Ðx-ÐOx components in the mesopause from rocket and satellite measurements. In this work, recently developed analytical criterion of determining the NOCE boundary is applied (1) to study of connection of this boundary with O and H spatiotemporal variability basing on the 3D chemical transport modeling, and (2) to retrieve and analyze the spatiotemporal evolution of the NOCE boundary in 2002–2021 from SABER/TIMED data set. It was revealed, first, that the NOCE boundary well reproduces the transition zone dividing deep and weak diurnal oscillations of O and H at the low and middle latitudes. Second, the NOCE boundary is sensitive to sporadic abrupt changes in the middle atmosphere dynamics, in particular, due to powerful sudden stratospheric warmings leading to events of elevated (up to ~80 km) stratopause, which took place in January–February 2004, 2006, 2009, 2010, 2012, 2013, 2018 and 2019. Third, the space-time evolution of this characteristics expressed via pressure-height contains a clear signal of 11-year solar cycle in the range of 55º S–55º N. In particular, average annual the NOCE boundary averaged in this range of latitudes anticorrelates well with F<sub>10.7</sub> index with the coefficient of -0.96. Moreover, it shows a weak linear trend of 49.2±36.2 m/decade." @default.
- W4386997965 created "2023-09-25" @default.
- W4386997965 creator A5075717758 @default.
- W4386997965 date "2023-09-24" @default.
- W4386997965 modified "2023-09-30" @default.
- W4386997965 title "Reply on RC2" @default.
- W4386997965 doi "https://doi.org/10.5194/egusphere-2023-1046-ac2" @default.
- W4386997965 hasPublicationYear "2023" @default.
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