What is it about?
Deficit and excessive rainfalls both harm monsoon-season rice yields. The response of crop yield to rainfall is nonlinear, but the optimal rainfall threshold across different regions and times is not well understood. Using historical rice production and climate data from 1990 to 2017, we identified the optimal rainfall point for peak Kharif rice yield in this study. The optimal rainfall threshold for monsoon rice yield in India is 1,621mm. Beyond this threshold, rice yield declines significantly. The threshold varies across 14 states, reflecting diverse climatic conditions and agricultural practices. Excessive rainfall could reduce rice yield by as much as 33.7%, while deficit rainfall 19%. For every 100 mm increase in rainfall beyond the optimal threshold, yield declines by 6.4 kg per hectare. Extreme climate events, like those associated with ENSO, cause substantial fluctuations in rice production. ENSO events have led to notable yield losses during extreme weather years.
Featured Image
Photo by R.S SAGAR on Unsplash
Why is it important?
India, along with many other countries in South Asia, experiences significant climatic variations, especially during the monsoon seasons influenced by the Indian Ocean. The summer monsoon, from June to September, provides 70-90% of the annual rainfall, crucial for agriculture. The El Niño-Southern Oscillation (ENSO) significantly affects monsoon precipitation and temperature, leading to variable rainfall patterns and impacting crop yields. India's agriculture sector heavily relies on these monsoons. Kharif rice, planted during the monsoon season, accounts for 85% of the country's total rice production, making it vital for food security and the economy. India contributes nearly 20% of the world's total rice production annually.
Perspectives
Read the Original
This page is a summary of: Optimal rainfall threshold for monsoon rice production in India varies across space and time, Communications Earth & Environment, June 2024, Springer Science + Business Media,
DOI: 10.1038/s43247-024-01414-7.
You can read the full text:
Contributors
The following have contributed to this page