Reversal of the warm Arctic–cold Eurasia intraseasonal coupling by CO2 removal

Midlatitude winter climate variability arises partly from its interactions with Arctic climate variability. A prominent example is the intraseasonal coupling between warm temperature anomalies over the Barents–Kara Seas and cold anomalies over central Eurasia, commonly referred to as the warm Arctic...

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Autori principali:	M Inês Cajada, Seok-Woo Son, Ye-Jun Jun, S-Y Simon Wang, Jin-Ho Yoon, Seung-Ki Min
Natura:	Artigo
Lingua:	Inglês
Pubblicazione:	IOP Publishing 2026-01-01
Serie:	Environmental Research Letters
Soggetti:	warm Arctic–cold Eurasia relationship carbon dioxide removal experiment baroclinicity meridional temperature gradient
Accesso online:	https://doi.org/10.1088/1748-9326/ae6dd7
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