Oman coral δ(18)O seawater record suggests that Western Indian Ocean upwelling uncouples from the Indian Ocean Dipole during the global-warming hiatus

The Indian Ocean Dipole (IOD) is an interannual mode of climate variability in the Indian Ocean that has intensified with 20(th) century global-warming. However, instrumental data shows a global-warming hiatus between the late-1990s and 2015. It is presently not clear how the global-warming hiatus a...

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Detalles Bibliográficos
Autores principales: Watanabe, Takaaki K., Watanabe, Tsuyoshi, Yamazaki, Atsuko, Pfeiffer, Miriam, Claereboudt, Michel R.
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/PMC6374511/
https://www.ncbi.nlm.nih.gov/pubmed/30760830
http://dx.doi.org/10.1038/s41598-018-38429-y

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6374511/
https://www.ncbi.nlm.nih.gov/pubmed/30760830
http://dx.doi.org/10.1038/s41598-018-38429-y

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