The role of the SST-thermocline relationship in Indian Ocean Dipole skewness and its response to global warming

A positive Indian Ocean Dipole (IOD) tends to have stronger cold sea surface temperature anomalies (SSTAs) over the eastern Indian Ocean with greater impacts than warm SSTAs that occur during its negative phase. Two feedbacks have been suggested as the cause of positive IOD skewness, a positive Bjer...

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Detalles Bibliográficos
Autores principales: Ng, Benjamin, Cai, Wenju, Walsh, Kevin
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group 2014
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4129411/
https://www.ncbi.nlm.nih.gov/pubmed/25112717
http://dx.doi.org/10.1038/srep06034

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4129411/
https://www.ncbi.nlm.nih.gov/pubmed/25112717
http://dx.doi.org/10.1038/srep06034

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