No Emergence of Deep Convection in the Arctic Ocean Across CMIP6 Models

Abstract As sea ice disappears, the emergence of open ocean deep convection in the Arctic, which would enhance ice loss, has been suggested. Here, using 36 state‐of‐the‐art climate models and up to 50 ensemble members per model, we show that Arctic deep convection is rare under the strongest warming...

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Hlavní autoři:	Céline Heuzé, Hailong Liu
Médium:	Artigo
Jazyk:	Inglês
Vydáno:	Wiley 2024-02-01
Edice:	Geophysical Research Letters
Témata:	Arctic Ocean climate models mixing stratification climate change
On-line přístup:	https://doi.org/10.1029/2023GL106499
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