Quantification of ocean heat uptake from changes in atmospheric O(2) and CO(2) composition

The ocean is the main source of thermal inertia in the climate system. Ocean heat uptake during recent decades has been quantified using ocean temperature measurements. However, these estimates all use the same imperfect ocean dataset and share additional uncertainty due to sparse coverage, especial...

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Detalles Bibliográficos
Autores principales: Resplandy, L., Keeling, R. F., Eddebbar, Y., Brooks, M., Wang, R., Bopp, L., Long, M. C., Dunne, J. P., Koeve, W., Oschlies, A.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2019
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6934503/
https://www.ncbi.nlm.nih.gov/pubmed/31882758
http://dx.doi.org/10.1038/s41598-019-56490-z

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6934503/
https://www.ncbi.nlm.nih.gov/pubmed/31882758
http://dx.doi.org/10.1038/s41598-019-56490-z

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