DELHI HEATWAVE

Last Updated on 30th April, 2025
12 minutes, 40 seconds

Description

Source: TIMES OF INDIA

Disclaimer: Copyright infringement not intended.

Context

India Meteorological Department (IMD) has issued a yellow alert for a heatwave in Delhi on April 25–26 forecasting maximum temperatures between 40–42°C with clear skies, dry westerly winds & sustained poor air quality despite slight improvements across Delhi-NCR.

IMD Heatwave Classification (Plains Region including Delhi)

Criteria

Threshold Value

Remarks

Maximum Temperature ≥ 40°C

With departure of ≥ 4.5°C to 6.4°C

Heatwave

Maximum Temperature ≥ 40°C

With departure of > 6.4°C

Severe Heatwave

Absolute Maximum Temperature ≥ 45°C

Irrespective of normal

Heatwave

Absolute Maximum Temperature ≥ 47°C

Irrespective of normal

Severe Heatwave

Minimum Temperature Influence

Not considered directly

But contributes to thermal stress during heatwave spells

Duration

Usually 2 or more consecutive days

But warning may be issued even for 1 day in exceptional cases

Air Quality Index (AQI) Color Categories – CPCB India

AQI Range

Color Code

Category

Associated Health Impacts

0 – 50

Green

Good

Minimal or no health risk. Air quality is considered satisfactory.

51 – 100

Light Green

Satisfactory

Acceptable; may cause minor breathing discomfort to sensitive individuals.

101 – 200

Yellow

Moderate

Breathing discomfort to people with asthma, heart disease, elderly & children.

201 – 300

Orange

Poor

Increased likelihood of respiratory symptoms among sensitive groups.

301 – 400

Red-Purple

Very Poor

Respiratory illness on prolonged exposure; affects general public health.

401 – 500

Maroon

Severe

Serious health effects even on healthy people; emergency conditions for sensitive groups.

 Air Quality Alerts Based on AQI Levels

Alert Type

AQI Range

Description

Health Advisory

No Alert

0 – 50

Air quality is considered satisfactory with little or no risk to general population.

No action required.

Moderate

51 – 100

Air quality is acceptable; however there may be some health effects for sensitive individuals (e.g. asthma or breathing issues).

People with respiratory conditions should limit prolonged exertion outdoors.

Unhealthy for Sensitive Groups

101 – 200

Health effects may be felt by sensitive individuals such as children, elderly people & those with respiratory or heart conditions.

Sensitive individuals should avoid prolonged outdoor activities.

Unhealthy

201 – 300

Health effects are likely to occur for general population not just sensitive groups. Outdoor activities should be limited.

Everyone may begin to experience health effects; sensitive individuals should avoid outdoor exertion.

Very Unhealthy

301 – 400

Health alert. Everyone may experience more serious health effects.

Everyone should avoid outdoor activities; stay indoors with air conditioning.

Hazardous

401 – 500

Emergency conditions. Serious health effects for entire population.

All individuals should remain indoors & avoid physical activities.

Western Disturbance (WD)

A Western Disturbance (WD) refers to an extratropical storm that originates in Mediterranean region or North Africa & moves eastward across Middle East & northern Indian subcontinent primarily affecting India, Pakistan & Nepal.

Aspect

Description

Origin

Mediterranean & North African regions where warm & moist air meets cold air from polar regions.

Nature

These disturbances are low-pressure systems & are responsible for bringing rainfall & colder conditions.

Movement

They generally travel eastward from Mediterranean crossing Iran, Afghanistan & Pakistan into northern India.

Impact on Weather

WD brings rain to northwestern & northern India (Punjab, Haryana, Delhi, Himachal Pradesh, Jammu & Kashmir) & can cause fluctuations in winter temperatures.

Duration

Typically these disturbances last 3-5 days & affect western Himalayan region with varying intensities.

Precipitation Type

The precipitation associated with Western Disturbances is mostly light to moderate rainfall or snowfall in hilly areas although heavy rainfall may occur in some cases.

Seasonality

Predominantly observed during winter season (from October to March) with some weakening or absence during summer monsoon months.

Influence on Indian Climate

WDs are crucial for winter precipitation in northwestern & northern India & play a significant role in maintaining agricultural productivity of these regions.

Thunderstorms

WDs also bring thunderstorms particularly in plains of northern India often associated with sudden temperature drops & shifting wind patterns.

Impact of Western Disturbance (WD) on India

Snowfall in Himalayas WDs cause snowfall in higher altitudes of western Himalayas, which affects water resources in region.

Rainfall in Plains Regions like Delhi, Punjab, Haryana & Uttar Pradesh receive rainfall often leading to a sudden drop in temperatures.

Temperature Variations WDs can cause sharp fluctuations in temperatures with warm spells followed by cold spells. They can also lead to fog & low visibility during winter months.

Cyclonic Storms: In certain instances if disturbance intensifies it can lead to cyclonic storms though this is rarer.

East India Thunderstorms

Thunderstorms in East India including states like Odisha, West Bengal, Bihar, Jharkhand & parts of Uttar Pradesh are typically linked to warm, moist air & significant atmospheric instability. These storms are particularly active during pre-monsoon & monsoon months.

Key Characteristics of Thunderstorms in East India

Aspect

Description

Formation

Thunderstorms in East India generally form due to convergence of moist air from Bay of Bengal & hot, dry air from north. The region experiences frequent occurrences of low-pressure areas.

Seasons

Thunderstorms are most common during pre-monsoon season (March to June) & monsoon season (June to September). However they can occur in post-monsoon period as well.

Conditions Favoring Formation

High surface temperatures, moisture availability from Bay of Bengal & atmospheric instability are key ingredients for thunderstorm development.

Wind Patterns

Strong easterly winds coupled with influx of moisture from Bay of Bengal help in creating conditions for thunderstorms.

Intensity

These thunderstorms can be severe often producing heavy rainfall, strong winds (30-60 km/h), lightning & occasionally hail.

Tornadoes

Tornadoes are rare but can occur especially with intense thunderstorms in this region.

Duration & Frequency

Thunderstorms typically last for 1-2 hours but can be frequent in summer months especially in region’s hilly terrain & coastal areas.

Impact on Weather

The thunderstorms bring much-needed rain to agricultural regions of East India but can also result in localized flooding, property damage & loss of life.

Rainfall

Thunderstorms often lead to heavy & localized rainfall which can cause flash floods particularly in hilly areas.

Lightning

Lightning strikes are frequent & can cause fires, power outages & injuries especially in rural & agricultural areas.

Thunderstorm Dynamics in East India

Development of Low-Pressure Areas Low-pressure areas or cyclonic circulations over Bay of Bengal can significantly enhance thunderstorm activity by strengthening convergence of air masses.

Influence of Sea Breeze The sea breeze from Bay of Bengal plays a critical role in triggering convection particularly in coastal regions like Odisha & West Bengal where afternoon thunderstorms are common.

Convection & Instability High temperature gradients between land & sea cause vertical convection resulting in upward movement of warm, moist air. As air rises, it cools, condenses & forms clouds leading to thunderstorm activity.

Thunderstorms & Crop Damage These storms often lead to damage of standing crops due to strong winds, hail & flooding. The region heavy reliance on agriculture makes these storms both a boon (for rainfall) & a bane (for crop destruction).

Key Meteorological Factors Affecting East India Thunderstorms

Sea Surface Temperatures (SSTs) Warm SSTs in Bay of Bengal increase moisture content in air enhancing thunderstorm development.

Atmospheric Instability A sharp contrast between warm surface air & cooler air aloft fosters conditions for deep convection & thunderstorm formation.

Low-Level Jet Streams The presence of low-level jet streams which transport moisture into region is crucial for intensity of these thunderstorms.

Impact of Western Disturbance on Delhi Weather

Aspect

Impact on Delhi Weather

Details

Temperature Variations

Sudden Drop in Temperature

WDs cause cold northerly winds leading to a sharp decrease in temperature particularly during winter months.

Precipitation

Light to Moderate Rain

Light rainfall often intermittent caused by WDs passing over Delhi. Rainfall can last over a few days increasing humidity levels.

Fog Formation

Dense Fog

WDs lead to foggy conditions especially in mornings due to drop in temperature & high humidity.

Hailstorms

Occasional Hailstorms

WDs may occasionally cause hailstorms in Delhi especially during winter though this is rare.

Wind Patterns

Cold Westerlies, Gusty Winds

Strong westerly winds reduce temperatures & may bring brief gusts of rain followed by clear skies.

Visibility

Reduced Visibility (Fog)

The fog reduces visibility especially in early mornings which can affect air & road transport.

Impact of East India Thunderstorms on Delhi Weather

Aspect

Impact on Delhi Weather

Details

Temperature Variations

Hot & Humid Conditions

Thunderstorms from East India bring warm, moist air to Delhi raising temperatures & increasing humidity particularly before or during thunderstorms.

Precipitation

Unpredictable Rainfall

Brief, sudden rainfall occurs in Delhi especially in pre-monsoon months but is usually lighter compared to eastern states.

Humidity

Increased Humidity

The moist air from East India thunderstorms causes a rise in humidity levels leading to uncomfortable conditions especially during pre-monsoon months.

Air Quality

Deterioration in Air Quality

Humidity & rising temperatures can exacerbate pollution levels, causing smog & haze & occasionally dust storms.

Heat Index

Higher Apparent Temperature

Due to increase in humidity, heat index (feels-like temperature) is higher than actual temperatures making it feel hotter.

Dust Storms

Higher Dust Concentration

Strong winds from thunderstorms may carry dust & particulate matter into Delhi worsening air quality.

 For more such articles, please refer to IAS GYAN

Sources:

BUSINESS STANDARD

PRACTICE QUESTION

Q. Discuss how Western Disturbances & East India-origin thunderstorms differently impact weather patterns of Delhi particularly in terms of temperature, precipitation & air quality.

 

Free access to e-paper and WhatsApp updates

Let's Get In Touch!