Ocean-atmosphere interactions are key processes that drive seasonal climate variability. In the global sense, the atmosphere drives the upper ocean via heat flux, fresh water flux and wind stress (Anderson 2008). But in the tropics where the ocean surface
Eun-Pa Lim,Harry H. Hendon,Sally Langford,et al. Improvements in POAMA2 for the prediction of major climate drivers and south eastern Australian rainfall. 2012-01-01.