Résumé
The 0–300 m, 300–700 m, 700–2,000 m and below-2,000 m layers are responsible for 42%, 22%, 29% and 7% of total OHC accumulated since 1960, respectively. OHC increased relative to 2023, with contributions of 9.9, 8.4, 2.6, –4.8 and –0.7 ZJ from the upper 2,000 m Atlantic, Indian, Southern, Pacific, and abyssal oceans below 2,000 m, respectively. The most vigorous ocean warming from 2023 to 2024 occurred in the Northwest Pacific, Southwest and East Indian oceans, and the Pacific sector of the Southern Ocean.
| langue originale | Anglais |
|---|---|
| Numéro d'article | 22975 |
| Pages (de - à) | 249-251 |
| Nombre de pages | 3 |
| journal | Nature Reviews Earth and Environment |
| Volume | 6 |
| Numéro de publication | 4 |
| Les DOIs | |
| état | Publié - 1 avr. 2025 |
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