Disclaimer: Copyright infringement not intended.
IMD has predicted an early summer with extreme heatwaves in India as climate change accelerates altering impacts of El Nino & La Nina on global weather patterns.
Rising Temperatures & Early Summer:
IMD predicts an early summer in 2025 with above normal temperatures & prolonged heatwaves.
February 2025 was India warmest since 1901 with low rainfall affecting cooling mechanisms.
Climate Change & Heatwave Intensification:
Human caused climate change is making winters warmer & springs shorter in India.
2024 saw 536 heatwave days highest in 14 years with northwest region recording its hottest June since 1901.
Role of Jet Streams in Weather Patterns:
Jet streams which influence weather by shifting north-south are linked to heatwave duration & intensity.
A northward shift in pre-monsoon worsens extreme heat conditions.
El Nino & La Nina Impact on India Weather:
El Nino (warming phase) is associated with hotter summers & drier conditions.
La Nina (cooling phase) traditionally brings cooler temperatures but may lose its cooling effect in a warming world.
2023-24 El Nino was one of the strongest on record contributing to extreme weather events globally.
Weak La Nina in 2025 & ENSO Predictions:
WMO noted that La Nina emerging in Dec 2024 is weak & likely short-lived.
Predictions suggest a 60% chance of ENSO-neutral conditions in March-May 2025.
Scientists warn that even in ENSO-neutral years climate change alone can drive severe heatwaves.
Future Projections & Risks:
Studies predict stronger & more frequent El Nino events in a warmer future.
Scientists caution that La Nina may not provide relief from heat extremes as global temperatures continue to rise.
The record-breaking warming trend of 2023 is still continuing into 2025.
Feature |
El Niño(Warm Phase) |
La Niña (Cool Phase) |
Definition |
A climate phenomenon characterized by the warming of sea surface temperatures (SSTs) in the central and eastern Pacific Ocean. |
A climate phenomenon characterized by the cooling of sea surface temperatures (SSTs) in the central and eastern Pacific Ocean. |
Cause |
Weakening or reversal of trade winds over the Pacific, causing warm water to move eastward. |
Strengthening of trade winds, pushing warm water westward, leading to an upwelling of cold water from deep ocean layers. |
Temperature Impact |
Leads to higher global temperatures and extreme heat events. |
Generally associated with cooler global temperatures but may not offset global warming trends. |
Effect on Indian Monsoon |
Weakens monsoon → Causes droughts and reduced rainfall in India. |
Strengthens monsoon → Leads to above-normal rainfall and potential floods in India. |
Effect on Global Weather |
Warmer temperatures, extreme heat, and drier conditions in Asia, Australia, and Africa. |
Cooler temperatures, heavy rainfall, and flooding in parts of Asia and Australia. |
Impact on Indian Agriculture |
Lower rainfall → Crop failures, drought stress, and food price inflation. |
Higher rainfall → Good harvests but potential crop damage due to excessive rainfall and floods. |
Impact on Fisheries |
Warm waters disrupt marine ecosystems, reducing fish populations off the coast of Peru, Ecuador, and Southeast Asia. |
Cold waters boost nutrient-rich upwelling, leading to better fish populations and higher fish catch. |
Extreme Events |
1997-98 El Niño – One of the strongest recorded, causing global droughts and floods. |
1988-89 La Niña – Led to stronger monsoons and heavy rainfall in India. |
Frequency |
Occurs every 2-7 years (lasts 9-12 months). |
Occurs every 3-5 years (lasts 9-12 months). |
Climate Change Impact |
El Niño events are becoming stronger and more frequent due to global warming, intensifying heatwaves and extreme weather. |
La Niña’s cooling effect may weaken in a warmer world, reducing its ability to counteract heat extremes. |
ENSO (El Nino-Southern Oscillation) is climate phenomenon in Pacific Ocean that affects global weather patterns. It consists of three phases: El Niño, La Niña, Neutral. The process is driven by changes in sea surface temperatures (SSTs), trade winds, atmospheric pressure over equatorial Pacific Ocean.
Feature |
El Niño (Warm Phase) |
La Niña (Cool Phase) |
Neutral (Normal Conditions) |
Trade Winds |
Weak or reverse (eastward) |
Stronger than normal (westward) |
Normal (east to west) |
Sea Surface Temperature (SST) |
Warmer than normal in the central & eastern Pacific |
Cooler than normal in the central & eastern Pacific |
Normal SST in the Pacific |
Upwelling (Cold Water Rising) |
Decreases, leading to fewer nutrients for marine life |
Increases, supporting marine ecosystems |
Normal upwelling near South America |
Rainfall in South America (Peru, Ecuador, Chile) |
Higher (Floods & landslides) |
Lower (Drought) |
Normal rainfall |
Rainfall in Australia & Indonesia |
Lower (Droughts & wildfires) |
Higher (Floods & heavy storms) |
Normal monsoons |
Indian Monsoon Impact |
Weaker monsoon → Droughts & heatwaves |
Stronger monsoon → Heavy rains & floods |
Normal monsoon season |
Effect on Hurricanes |
More hurricanes in Central & Eastern Pacific but fewer in the Atlantic |
More hurricanes in the Atlantic but fewer in the Pacific |
Normal hurricane activity |
Effect on Global Temperatures |
Warmer than average (Extreme heatwaves) |
Slightly cooler than average |
Normal global temperatures |
Effect on Agriculture |
Crop failures due to droughts (India, Australia) |
Excess rainfall, flood damage to crops |
Normal agricultural productivity |
Effect on Fisheries |
Decline in fish population near South America due to lack of nutrients |
Increase in fish population due to cold nutrient-rich water |
Normal fishing conditions |
Occurrence Frequency |
Every 2-7 years, lasts 9-12 months |
Every 2-7 years, lasts 9-12 months |
Occurs between El Niño & La Niña phases |
Strongest Recent Event |
2015-16 El Niño (India drought, coral bleaching, heatwaves) |
2020-22 La Niña (Pakistan floods, strong Indian monsoon) |
ENSO neutral phase in 2019 |
Sources:
PRACTICE QUESTION Q. Discuss significance of El Niño-Southern Oscillation (ENSO) phenomenon in influencing global climate patterns. Analyze its impact on the Indian monsoon & potential socio-economic implications for agriculture in India. |
© 2025 iasgyan. All right reserved