Rare Atmospheric Collision: Cyclone Arnab Meets Western Disturbance, Triggering Rain & Himalayan Snowfall!
A rare atmospheric interaction between Cyclone Arnab's tropical moisture and an active Western Disturbance brings widespread rain, hailstorms, and Himalayan snowfall. Read the full weather breakdown.
Rare Weather Phenomenon: How Cyclone Arnab's Collision with a Western Disturbance is Bringing Rain, Hailstorms, and Himalayan Snowfall
Weather & Environment Desk: In a rare meteorological phenomenon, tropical energy and mid-latitude westerlies have merged over the Indian subcontinent. The remnants of Cyclone Arnab—a severe cyclonic storm originating over the Bay of Bengal—are interacting with an incoming Western Disturbance.
This double-system weather event is causing an unusual clash of weather conditions: heavy downpours along the eastern coastal belts, unseasonal rain across central and northern plains, and fresh snowfall over the high-altitude Himalayan ranges.
1. The Mechanics: How Tropical Moisture Meets Cold Westerlies
Tropical cyclones typically weaken rapidly after making landfall as they lose their primary power source—warm ocean waters. However, Cyclone Arnab’s interaction with a Western Disturbance has altered this pattern:
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Moisture Inflow: As Cyclone Arnab pushed inland from the Bay of Bengal across Andhra Pradesh and Odisha, its outer bands dragged massive volumes of warm, moisture-laden air toward northern and central India.
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Western Disturbance System: Simultaneously, an active upper-air trough (Western Disturbance) carrying cold westerly winds swept across the western Himalayas.
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Atmospheric Instability: When warm tropical moisture collides with cold mid-latitude winds, it creates high atmospheric instability, triggering thunderstorm clusters, rapid cloud condensation, and localized hailstorms.
2. Regional Impact Matrix: Coastal Deluge to Mountain Snow
| Region / Zone | Weather Phenomenon | Key Affected Areas |
| Eastern Coast | Extremely Heavy Rain & Coastal Squalls | Coastal Andhra Pradesh, Odisha, West Bengal |
| Central & East India | Thunderstorms & Waterlogging | Chhattisgarh, Jharkhand, Bihar, Eastern UP |
| Northern Plains | Light-to-Moderate Rain & Hailstorms | Delhi-NCR, Haryana, Punjab, Western UP |
| Western Himalayas | Fresh Snowfall & Temperature Drop | High reaches of J&K, Himachal Pradesh, Uttarakhand, Sikkim |
3. Rain and Cold Snap in Delhi-NCR and Northern Plains
For the northern plains, including Delhi-NCR, Haryana, and Punjab, the influx of cyclone-fed moisture combined with westerly winds has brought unseasonal showers.
The India Meteorological Department (IMD) noted that while Delhi avoids the direct eye of the cyclonic storm, the interaction produces gusty winds, localized thunderstorms, and sharp nighttime drops in temperature, signaling an early winter transition.
4. Snowfall in the Himalayan Heights & Nepal
While plains experience rain and hailstorms, higher elevations are witnessing early snowfall. High-altitude zones in Kedarnath, Sikkim, Himachal Pradesh, and neighbor Nepal are reporting fresh snow accumulation.
Meteorologists warn that moisture interactions at altitudes above 3,500 meters rapidly freeze, turning heavy rainfall into dense snow layers, which could disrupt mountain passes and high-altitude highway traffic.
5. Advisory for Farmers and Coastal Communities
The dual weather system presents operational challenges for agriculture and logistics:
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Standing Crop Protection: Farmers in Haryana, Punjab, and Uttar Pradesh are advised to protect standing unharvested crops from potential lodging and hail damage.
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Coastal & Maritime Restrictions: Fishermen along the Andhra Pradesh, Odisha, and West Bengal coasts are strictly advised against venturing into deep seas due to squally winds.
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Mountain Travel: Travelers visiting high-altitude regions in Uttarakhand and Himachal Pradesh should check road clearance bulletins before embarking on mountain routes.
Conclusion
The collision between Cyclone Arnab’s remnants and the Western Disturbance demonstrates the complex dynamics of regional climate interactions. As the cyclone continues to weaken over land, its atmospheric footprint will persist for a few days, giving northern and eastern India an early winter preview.





