- The study shows that monsoon rainfall over India was higher during the mid-Pliocene period (around three million years ago), and a similar increase is expected in the future due to a warmer climate.
- These findings are important for climate preparedness, agriculture, and water management in India and nearby regions.
ROURKELA, 17th March 2026: Research led by researchers from National Institute of Technology Rourkela (NIT Rourkela) has studied how the Indian Summer Monsoon may change under future global warming. The findings of this study have been published in the prestigious International Journal of Climatology.
The Indian Summer Monsoon brings about 80 percent of India’s yearly rainfall and supports the livelihoods of hundreds of millions of people, especially those who depend on agriculture. Consistent monsoon rainfall is important for food production, water resources, and economic stability, not only in India but across South Asia.
As global temperatures increase because of climate change, there is a contradiction in the results of various studies conducted globally. While some studies suggest that rising temperatures may reduce rainfall, other studies have concluded that monsoon rainfall could become stronger. Given the monsoon’s strong impact on human livelihoods, it is important to understand how the Indian monsoon might respond.
To bridge this gap, Prof. Nagaraju Chilukoti, Assistant Professor, and Dr. Karishma Dahiya, Research Graduate, Department of Earth and Atmospheric Sciences, NIT Rourkela, in collaboration with Prof. Raju Attada, Department of Earth and Environmental Sciences, IISER Mohali, analysed how the monsoon behaved during warmer periods in Earth’s past to understand how it might behave in the future.
For this, the research team used climate models to compare two warm periods:
- the mid-Pliocene period
- the projected future climate of the late 21st century (2071–2100) under a high-emissions scenario
The Mid-Pliocene period is a subdivision of the geologic time scale that spans approximately 3.3 to 3.0 million years ago. This period is frequently studied by scientists to better understand potential future climate change, as many aspects of Earth’s climate system during the Mid-Pliocene resemble conditions projected under ongoing global warming. Consequently, it serves as an important analog for assessing future climate responses, including temperature, sea level, and atmospheric circulation changes.
During the mid-Pliocene, global temperatures were about four degrees higher than pre-industrial levels. Climate projections today indicate that similar levels of warming could occur by the end of this century. Based on this, the researchers studied how the Indian Summer Monsoon responds when the planet becomes warmer.
The study shows that monsoon rainfall over India was higher during the mid-Pliocene, and a similar increase is expected in a warmer future climate.
However, the reasons behind the increase in rainfall are different in the two cases. In the mid-Pliocene, stronger winds and more active atmospheric circulation led to stronger monsoon rainfall. In the future scenario, the increase in rainfall is expected to happen because a warmer atmosphere can hold more moisture.
Explaining the findings of this study, Prof. Nagaraju Chilukoti, Assistant Professor, Department of Earth and Atmospheric Sciences, NIT Rourkela, said, “The past is the key to the future and thus by examining the Mid-Pliocene warm climate, we gain crucial insights into how the Indian Summer Monsoon may respond to ongoing global warming. Our team observed that a warmer climate will likely increase the moisture in the atmosphere over the Indian Ocean and the Indian landmass, which could strengthen the movement of moisture toward India. The team also noted that the peak monsoon rainfall month may shift from July to August. These findings are important for climate preparedness, agriculture, and water management in India and nearby regions.”
As the next step, the research team aims to study the influence of large weather systems that form far north of India on rainfall patterns in the region.
A better understanding of rainfall patterns can help government officials and forecasting agencies improve early warning systems for floods and droughts. This can also help farmers in planning crop cycles and irrigation effectively if the timing and intensity of rainfall change.
Additionally, the study may also help policymakers manage water resources in major river systems like the Ganges and Brahmaputra and improve disaster preparedness and urban planning in flood-prone areas.
The research supports informed decision-making in various sectors and highlights the need for continued scientific investigation into regional climate systems to better anticipate future changes and their potential impacts on society.
