The relation between natural variations in ocean heat uptake and global mean surface temperature anomalies in CMIP5

It is still unclear whether a hiatus period arises due to a vertical redistribution of ocean heat content (OHC) without changing ocean heat uptake (OHU), or whether the increasing radiative forcing is associated with an increase in OHU when global mean surface temperature (GMST) rise stalls. By isol...

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Detalles Bibliográficos
Autor principal: Drijfhout, Sybren
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2018
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5943251/
https://www.ncbi.nlm.nih.gov/pubmed/29743486
http://dx.doi.org/10.1038/s41598-018-25342-7

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5943251/
https://www.ncbi.nlm.nih.gov/pubmed/29743486
http://dx.doi.org/10.1038/s41598-018-25342-7

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