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Global warming is weakening the traditional circulation of the Indian monsoon. Rising sea surface temperatures in the Indian Ocean change air pressure patterns, disrupting rainfall distribution. This results in weaker overall monsoons and more frequent extreme weather events.
Rainfall has decreased in central and northern India—key agricultural regions—while increasing in western areas such as Gujarat and parts of Rajasthan. These shifts threaten food security as fertile regions receive less rainfall.
Extreme rainfall events are becoming more frequent and intense in regions like Himachal Pradesh, Uttarakhand, and the northwestern Himalayas. Meanwhile, some central and southern areas are experiencing fewer such events.
Breaks in monsoon rains are now followed by hotter, more humid conditions, increasing heat stress. The imbalance between wet and dry spells amplifies health risks and discomfort.
El Niño, caused by warming in the central and eastern Pacific, typically reduces rainfall in India. Climate change is making these weakening effects stronger and more frequent, complicating seasonal forecasts.
The monsoon provides water for over half of India’s farmland. Reduced rainfall in fertile states like Madhya Pradesh, Chhattisgarh, and Uttar Pradesh threatens crop yields, while erratic heavy rains increase flood damage to standing crops.
Monitoring and forecasting extreme rainfall is difficult due to limited radar coverage, particularly in remote mountainous areas. Rapid-onset flash floods often catch communities unprepared.
With 47% of the population dependent on agriculture and 40% of food production tied to the monsoon, shifts in rainfall pose significant risks to food security, rural livelihoods, urban planning, and disaster management.
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