<p>Future changes in rainfall over India are critically important, given their impact on millions of people and the country’s agriculture. However, most studies focus only on changes up to the year 2100, leaving long-term projections largely unexplored. In this study, we leverage a 10-member ensemble with an Earth system model under relatively strong emissions to examine rainfall changes over India to 2500. Our results show a pronounced weakening of large-scale monsoon circulation after 2100, mainly due to increased atmospheric stability caused by rapid warming in the upper troposphere over land. At the same time, the Indian monsoon system expands significantly to the north and west. The northward expansion is driven by accelerated warming over the Tibetan Plateau, which pushes the low-level monsoonal winds and pressure systems further north. This, along with the development of a strong anomalous anticyclonic circulation over the Bay of Bengal, leads to more consistent upward motion over northern India and a northward expansion of the monsoon. Meanwhile, the westward expansion is linked to uneven warming in the Indian Ocean as the warm pool shifts westwards. These circulation changes, combined with the asymmetric warming pattern, enhance northward moisture transport and contribute to the intensification of rainfall across northwestern and northern India post-2100. These local expressions of large-scale perturbations provide a mechanistic framework for informing long-term mitigation and adaptation efforts for India.</p>