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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Egile Nagusiak:	Aaron Match, Edwin P. Gerber
Formatua:	Artigo
Hizkuntza:	Inglês
Argitaratua:	Wiley 2025-05-01
Saila:	Geophysical Research Letters
Gaiak:	ozone layer global warming tropospheric expansion brewer‐dobson circulation chemistry‐climate models idealized modeling
Sarrera elektronikoa:	https://doi.org/10.1029/2024GL112409
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