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...

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Detalles Bibliográficos
Autores principales: Liu, Maofeng, Vecchi, Gabriel, Soden, Brian, Yang, Wenchang, Zhang, Bosong
Formato: Online Artículo Texto
Lenguaje:English
Publicado: 2021
Materias:
Article
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

Internet

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

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