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Tropospheric ozone precursors: global and regional distributions, trends, and variability

<p>Tropospheric ozone results from in situ chemical formation and stratosphere–troposphere exchange (STE), with the latter being more important in the middle and upper troposphere than in the lower troposphere. Ozone photochemical formation is nonlinear and results from the oxidation of methane and...

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Bibliografiske detaljer
Principais autores: Y. Elshorbany, J. R. Ziemke, S. Strode, H. Petetin, K. Miyazaki, I. De Smedt, K. Pickering, R. J. Seguel, H. Worden, T. Emmerichs, D. Taraborrelli, M. Cazorla, S. Fadnavis, R. R. Buchholz, B. Gaubert, N. Y. Rojas, T. Nogueira, T. Salameh, M. Huang
Format: Artigo
Sprog:Inglês
Udgivet: Copernicus Publications 2024-11-01
Serier:Atmospheric Chemistry and Physics
Online adgang:https://acp.copernicus.org/articles/24/12225/2024/acp-24-12225-2024.pdf
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