How can Brewer–Dobson circulation trends be estimated from changes in stratospheric water vapour and methane?

How can Brewer–Dobson circulation trends be estimated from changes in stratospheric water vapour and methane?

<p>The stratospheric meridional overturning circulation, also referred to as the Brewer–Dobson circulation (BDC), controls the composition of the stratosphere, which, in turn, affects radiation and climate. As the BDC cannot be directly measured, one has to infer its strength and trends indire...

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Bibliographic Details
Main Authors: L. Poshyvailo-Strube, R. Müller, S. Fueglistaler, M. I. Hegglin, J. C. Laube, C. M. Volk, F. Ploeger
Format: Article
Language:English
Published: Copernicus Publications 2022-08-01
Series:Atmospheric Chemistry and Physics
Online Access:https://acp.copernicus.org/articles/22/9895/2022/acp-22-9895-2022.pdf

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