Tracking ocean heat uptake during the surface warming hiatus
Mechanisms for the warming hiatus are inferred by tracking regional ocean heat uptake in different regions. Here, the authors show that the Indo-Pacific heat redistribution holds the key while the abyssal heat uptake in the Atlantic and Southern Oceans primarily reflects the downward penetration of...
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| Auteurs principaux: | , , |
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| Format: | article |
| Langue: | EN |
| Publié: |
Nature Portfolio
2016
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| Accès en ligne: | https://doaj.org/article/e7f67660e5fa49fdbd1ce79a9d8911dd |
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| Résumé: | Mechanisms for the warming hiatus are inferred by tracking regional ocean heat uptake in different regions. Here, the authors show that the Indo-Pacific heat redistribution holds the key while the abyssal heat uptake in the Atlantic and Southern Oceans primarily reflects the downward penetration of anthropogenic heat. |
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