La Niña is the cool phase of the El Niño Southern Oscillation (ENSO), quite the opposite of the warm El Niño event. It cools central and eastern Pacific waters and causes strong trade winds that influence the rainfall patterns globally. Today’s blog explains the La Niña effect, its impact on the climate and agriculture and policy measures.
La Niña is also known as ‘Little Girl’ in Spanish. It is a global climatic phenomenon recognized as the cool phase of the El Niño Southern Oscillation (ENSO). Due to this climate pattern, sea surface temperatures in the central and eastern tropical Pacific Ocean experience periodic cooling. It involves the movement of strong trade winds, which intensifies the upwelling of cold water in the eastern Pacific. It has a significant impact during the winter and monsoon seasons in India.
Generally, these climatic episodes occur every 2-7 years but are not regular events. The Down to Earth report says that the January 2025 was recorded as the warmest month with a 1.75°C anomaly despite La Niña.
According to the World Meteorological Organization's forecast, 55% of sea surface temperatures in the equatorial Pacific were expected to cool to La Niña levels, and 45% to remain at ENSO-neutral levels during the September–November 2025 period. For October–December 2025, the La Niña establishment slightly increased to about 60%, while the ENSO-neutral conditions decreased to around 40%.
The Pacific Ocean temperatures change due to La Niña which impacts tropical rainfall patterns from Indonesia to South America (west coast). La Niña effects include changes in global weather patterns. In North America, northern regions experience colder winters, while southern regions experience warmer, drier conditions. In South America, Brazil experiences increased rainfall, while Ecuador and Peru experience drought. Central America can face crop loss due to floods.
In Asia, intense monsoons occur in India and South Asia. There is increased precipitation and a higher risk of flooding in Southeast Asia and Australia. In Africa, enhanced rainfall may be observed in Southern Africa. Also, there is a risk of droughts that can endanger crops and livestock.
The major effects of La Nina are on the climate and agriculture. Let’s discuss both:
El Niño-Southern Oscillation (ENSO) has a big impact on the Indian climate, along with the monsoon and agriculture. More intense monsoons are observed due to La Niña, resulting in above-average rainfall in most parts of the country. Cooler temperatures can be observed post-monsoon and during winter months. Coastal regions are at risk due to increased cyclone activity in the Indian Ocean. La Niña leads to colder winters in northern India, with states like Himachal Pradesh, Haryana, and Punjab experiencing cold waves and frost.
The agricultural sector of India is impacted by weather patterns induced by La Niña. It is usually beneficial for monsoon-dependent crops like paddy, sugarcane, and pulses because of increased rainfall. More rainfall boosts the growth and development of several Kharif crops. In addition, it can help in recharging groundwater levels. The rainfall intensity and timing can also influence variations in crop yields.
However, there are high chances of crop damage in regions that receive flooding or excessive precipitation. Low-lying areas can get flooded, which damages standing crops, which also delays their harvesting. Waterlogging can cause pest and disease infestations to hamper yields. Due to changes in the onset and intensity of rainfall, planting schedules and variety selection need to be adjusted accordingly.
La Niña can easily impact water management, agriculture, health, energy, and infrastructure in India. There is a need for mitigating risks related to increased cyclone activity, extreme winters, and intense monsoon seasons.
La Niña effects are complex and vary across regions. In India, La Niña can cause a cooler winter in North India, increased cyclone activity in the Indian Ocean, and an intense southwest monsoon. La Niña has both pros and cons for the Indian climate and agriculture. Thus, there is a need for strategic preparedness to handle damage to crops and infrastructure.
The main La Niña effect in India is more-than-normal rainfall during the Southwest monsoon and Northeast monsoon and colder winters in North India.
El Niño and La Niña are two opposing components of the El Niño Southern Oscillation, where El Niño signifies the warm phase while La Niña is the cool phase.
The last La Niña event occurred from 2020 to early 2023 in India. A short-lived La Niña also occurred in September 2025.
Yes, La Niña causes more rainfall in Southeast Asia. Also, more rain is expected with the Indian monsoon.