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The Double Dip: How Tropospheric Expansion Counteracts Increases in Extratropical Stratospheric Ozone Under Global Warming

Abstract In response to rising CO2, chemistry‐climate models (CCMs) project that extratropical stratospheric ozone will increase, except around 10 and 17 km. We call the muted increases or reductions at these altitudes the “double dip.” The double dip results from surface warming (not stratospheric...

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Principais autores: Aaron Match, Edwin P. Gerber
Format: Artigo
Sprog:Inglês
Udgivet: Wiley 2025-05-01
Serier:Geophysical Research Letters
Fag:
ozone layer
global warming
tropospheric expansion
brewer‐dobson circulation
chemistry‐climate models
idealized modeling
Online adgang:https://doi.org/10.1029/2024GL112409
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