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20(th) century cooling of the deep ocean contributed to delayed acceleration of Earth’s energy imbalance
The historical evolution of Earth’s energy imbalance can be quantified by changes in the global ocean heat content. However, historical reconstructions of ocean heat content often neglect a large volume of the deep ocean, due to sparse observations of ocean temperatures below 2000 m. Here, we provid...
| Autores principales: | , |
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
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Nature Publishing Group UK
2021
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| Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8322321/ https://www.ncbi.nlm.nih.gov/pubmed/34326319 http://dx.doi.org/10.1038/s41467-021-24472-3 |