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• W2176670690 abstract "Abstract Vertical chemical transport occurs when the density fluctuations of a species, caused by perturbations of its chemistry, are strongly correlated with the vertical wind fluctuations. Chemical transport can exceed dynamical and eddy transport of chemically active species. Theoretical expressions are derived for the chemical fluxes and transport velocities and used to characterize the vertical transport of mesospheric O 3 and meteoric Na and Fe between 85 and 100 km. Chemical transport is dependent on the intrinsic frequency spectrum of the temperature fluctuations and on the chemical cutoff periods of the species. For O 3 only high‐frequency fluctuations contribute to chemical transport because slower, larger‐amplitude density perturbations are damped by chemistry. The cutoff periods for O 3 range from ~15 min during the day when photolysis is important to ~200 min at night. The chemical transport velocities of Na and Fe are proportional to the O 3 , O 2 + , and NO + densities above 85 km. For O 3 , Na, and Fe the magnitudes of the vertical transport velocity can be as large as 10 cm/s, and they exhibit strong diurnal variations. O 3 chemical transport is downward at night and upward during the day. Na and Fe chemical transport are largely upward with the strongest upward velocities at night near 85 and 100 km." @default.
• W2176670690 created "2016-06-24" @default.
• W2176670690 creator A5004669093 @default.
• W2176670690 creator A5048007083 @default.
• W2176670690 date "2016-01-07" @default.
• W2176670690 modified "2023-10-17" @default.
• W2176670690 title "Chemical transport of neutral atmospheric constituents by waves and turbulence: Theory and observations" @default.
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• W2176670690 doi "https://doi.org/10.1002/2015jd023145" @default.
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