The Northwest Indian Dust Storms

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A massive dust storm swept across Churu and several other districts of Rajasthan on May 30, 2026.
This event highlights the structural degradation of the Aravalli range.

A dust storm, known locally as Andhi, is a natural weather event common in dry and semi-dry regions.
Strong winds pick up large amounts of loose sand and dust from dry soils and create a thick wall of dust.
This phenomenon heavily reduces visibility and ruins air quality.

The main affected area is Northwest India, covering Rajasthan districts like Churu, Hanumangarh, Bikaner, and Jodhpur.
It also affects Delhi-NCR, Haryana, Punjab, and western Uttar Pradesh.
The protective Aravalli barrier is breaking down, allowing the dust to travel much deeper into the crowded Indo-Gangetic plains.

Pre-monsoon dust storms form due to a specific mix of heat and weather conditions.
Intense sunshine heats up the Thar Desert between April to June, creating pockets of extreme heat and unstable air.
This heavy heating creates a strong low-pressure zone near the ground.
Strong south-westerly and westerly winds rush in from the Middle East and the Thar to fill this empty space, carrying heavy dust.
Wind speeds crossing 35-40 kmph over dry soil lift dust particles into the air.
Without the tree cover and height of the Aravallis to stop them, these winds carry dust thousands of kilometers to the east.

These storms happen only before the monsoon, reaching their peak strength in May and June.
In the past, the western slopes of the Aravalli range acted as a natural wall against these winds.
Winds hitting the slopes drop their dust, forming special obstacle sand dunes held down by desert plants.
Data from the IMD shows that Delhi faces an average of 2.5 dust-storm days in June alone, the highest in the country.
A study by the Wildlife Institute of India (WII) confirmed 12 widening operational gaps in the Aravallis because 31 entire hillocks vanished due to illegal mining.