Tectonic and climatic drivers of Asian monsoon evolution

Asian Monsoon rainfall supports the livelihood of billions of people, yet the relative importance of different drivers remains an issue of great debate. Here, we present 30 million-year model-based reconstructions of Indian summer monsoon and South East Asian monsoon rainfall at millennial resolution. We show that precession is the dominant direct driver of orbital variability, although variability on obliquity timescales is driven through the ice sheets. Orographic development dominated the evolution of the South East Asian monsoon, but Indian summer monsoon evolution involved a complex mix of contributions from orography (39%), precession (25%), atmospheric CO2 (21%), ice-sheet state (5%) and ocean gateways (5%). Prior to 15Ma, the Indian summer monsoon was broadly stable, albeit with substantial orbital variability. From 15Ma to 5Ma, strengthening was driven by a combination of orography and glaciation, while closure of the Panama gateway provided the prerequisite for the modern Indian summer monsoon state through a strengthened Atlantic meridional overturning circulation. The drivers of monsoon systems in the past are not well known. Here, the authors present a model-based reconstruction of the last 30 million years and show that the south east Asian monsoon evolution is dominated by orographic development while the strength of the Indian Summer monsoon is controlled by a combination of factors.

Automated summary

The study reconstructed the evolution of monsoon systems in the past 30 million years using models, revealing the different drivers influencing the Asian monsoon and South East Asian monsoon. It shows that the Indian summer monsoon evolution is more complex compared to the South East Asian monsoon, with a combination of factors controlling its strength.