Abstract | The Maritime Continent, which lies over the tropical interface of the Indian and the Pacific Ocean, is home to intense Madden-Julian Oscillations during boreal winters. Here we show that the strong Madden-Julian Oscillation winds over this continent drives a barotropic dynamics that adjusts the Indo-Pacific basin in a few days, and induces a barotropic circulation about the Australian continent which reverses its direction every 30-80 days. This novel ocean dynamics generates a seesaw of oceanic mass in the Indo-Pacific basin. The large-scale ocean mass redistribution in the Indo-Pacific basin, accompanied by strong concurrent meridional transports in the Indian and Pacific basin, elicits a variability of 50 milliarcseconds in the polar motion of the Earth relative to its crust. |