LA NINA AND CLIMATE CHANGE

Last Updated on 13th March, 2025
9 minutes, 43 seconds

Description

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Context  

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.

Key Highlights

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.

El Nino vs La Nina

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. 
Colder, wetter winters in the southern U.S. and Peru. 
Increased risk of
 hurricanes in the Central/Eastern Pacific but fewer hurricanes in the Atlantic.

Cooler temperatures, heavy rainfall, and flooding in parts of Asia and Australia. 
Drier conditions in the southern U.S. and Peru. 
More hurricanes in the
 Atlantic, but fewer in the Central/Eastern Pacific.

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. 
2015-16 El Niño – Led to severe heatwaves in India and global coral bleaching. 
2023-24 El Niño – One of the strongest five on record, fueling extreme weather.

1988-89 La Niña – Led to stronger monsoons and heavy rainfall in India. 
2010-11 La Niña  Severe floods in Australia and Pakistan. 
2020-22 La Niña  Triple-dip event, lasted three consecutive years, causing record cold winters in some regions.

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:

ET

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.

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