The asymmetric influence of the positive and negative IOD events on China's rainfall

Rainfall anomalies over southern China are found to be asymmetricly influenced by the Indian Ocean Dipole (IOD), with a far stronger influence from positive IOD (pIOD) events. A greater convection anomaly and an equivalent-barotropic Rossby wave train response occurs during pIOD events than during n...

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Detalles Bibliográficos
Autores principales: Qiu, Yun, Cai, Wenju, Guo, Xiaogang, Ng, Benjamin
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group 2014
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4021319/
https://www.ncbi.nlm.nih.gov/pubmed/24828947
http://dx.doi.org/10.1038/srep04943

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4021319/
https://www.ncbi.nlm.nih.gov/pubmed/24828947
http://dx.doi.org/10.1038/srep04943

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