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Enhanced hydrological cycle increases ocean heat uptake and moderates transient climate change
The large-scale moistening of the atmosphere in response to increasing greenhouse gases amplifies the existing patterns of precipitation minus evaporation (P-E) which, in turn, amplifies the spatial contrast in sea surface salinity (SSS). Through a series of transient CO(2) doubling experiments, we...
| Autores principales: | , , , , |
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
| Publicado: |
2021
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| Materias: | |
| Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8587804/ https://www.ncbi.nlm.nih.gov/pubmed/34777581 http://dx.doi.org/10.1038/s41558-021-01152-0 |