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...
Αποθηκεύτηκε σε:
| Κύριοι συγγραφείς: | , |
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| Μορφή: | Artigo |
| Γλώσσα: | Inglês |
| Έκδοση: |
Wiley
2024-02-01
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| Σειρά: | Geophysical Research Letters |
| Θέματα: | |
| Διαθέσιμο Online: | https://doi.org/10.1029/2023GL106499 |
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