Roles of Indian and Pacific Ocean air–sea coupling in tropical atmospheric variability

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Regimes of seasonal air–sea interaction and implications for performance of forced simulations (2007, methodology): “ Wu and Kirtman (2005) showed that in regions where the atmosphere has a strong negative feedback on SST (e.g., tropical western North Pacific in boreal summer and tropical southwestern Indian Ocean in austral summer), the negative rainfall–SST tendency correlation is larger than the rainfall–SST c”
How are seasonal prediction skills related to models’ performance on mean state and annual cycle? (2010, background): “Treating atmosphere as a slave may limit the level of skill for Atmospheric Model Intercomparison Project (AMIP) type monsoon simulation (Kitoh and Arakawa 1999; Wang et al. 2004; Wu and Kirtman 2005) and two-tier summer”
An Assessment of the CFS Real-Time Seasonal Forecasts (2010, result): “the tropical Indian Ocean are consistent with previous studies that have shown that the atmospheric variability in the Indian Ocean is related to the atmosphere–ocean coupled response to remote forcings from the Pacific through the atmospheric bridge (Wang et al. 2005; Wu and Kirtman 2005; Krishna K”