Strong oceanic-atmospheric coupling exists between the Indian Ocean and Pacific Ocean basins
Multiple recent studies confirm that strong oceanic-atmospheric teleconnections and basin interactions link the Indian and Pacific Oceans, significantly modulating regional climate anomalies and ENSO predictability.
The retrieved papers provide robust, multi-faceted evidence supporting the claim of strong oceanic-atmospheric coupling between the Indian Ocean and Pacific Ocean basins (e.g., papers 1, 3, and 6). These studies demonstrate how climate modes and anomalies in one basin (like the IOBM in the Indian Ocean) interact with and modulate phenomena in the other basin (like ENSO in the Pacific), through atmospheric circulations, subsurface heat transport, and wave trains. No papers refute the claim.
Wenju Cai, Peter van Rensch. Austral Summer Teleconnections of Indo-Pacific Variability: Their Nonlinearity and Impacts on Australian Climate. 2013. https://doi.org/10.1175/jcli-d-12-00458.1
Demonstrates that Indian Ocean variability (IOBM) extends ENSO-induced climate and convection anomalies from the Pacific into the Australian region.
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Xue J, Zhang W, Zhang Y, Luo JJ, Zhu H, Sun C, Yamagata T. Interdecadal modulation of Ningaloo Niño/Niña strength in the Southeast Indian Ocean by the Atlantic Multidecadal Oscillation.. 2025. https://doi.org/10.1038/s41467-025-57160-7
Shows that Indian Ocean-atmosphere coupling and Indo-Pacific teleconnections modulate extreme regional events like Ningaloo Niño/Niña.
Zhou L, Zhang RH. Tropical basin interactions reduce spring predictability barrier of ENSO in a deep learning model.. 2026. https://doi.org/10.1126/sciadv.aeb0901
Highlights that tropical basin interactions between the Indian, Atlantic, and Pacific Oceans are critical for global ocean-atmosphere prediction and ENSO dynamics.
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