Nonlinear processes reinforce extreme Indian Ocean Dipole events

Under global warming, climate models show an almost three-fold increase in extreme positive Indian Ocean Dipole (pIOD) events by 2100. These extreme pIODs are characterised by a westward extension of cold sea surface temperature anomalies (SSTAs) which push the downstream atmospheric convergence fur...

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Detalles Bibliográficos
Autores principales: Ng, Benjamin, Cai, Wenju, Walsh, Kevin, Santoso, Agus
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group 2015
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4481856/
https://www.ncbi.nlm.nih.gov/pubmed/26114441
http://dx.doi.org/10.1038/srep11697

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4481856/
https://www.ncbi.nlm.nih.gov/pubmed/26114441
http://dx.doi.org/10.1038/srep11697

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