North India experienced a warm and dry winter attributed to weak Western Disturbances (WDs).
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Weak western disturbances and shifting jet stream drive warm, dry winter in North India
North India experienced an unusually warm and dry winter primarily due to weak Western Disturbances and a shifting jet stream. This climatic anomaly, driven by altered upper-level winds, has significantly suppressed crucial rain and snowfall over the Himalayas. The resulting dry conditions are also contributing to worsening air quality across the north-west, making understanding these meteorological phenomena vital for competitive exams focusing on Indian geography and environment.
Source: Down To Earth. This summary and analysis are AI-written from that report and are not individually fact-checked — confirm names, dates and figures with the source before you rely on them.
Revision structure
Key points
Exam-ready takeaways
A shifting upper-level jet stream is identified as a primary meteorological factor contributing to the altered winter patterns.
The lack of adequate Western Disturbances has led to suppressed rain and snow over the Himalayan region.
The dry winter conditions and atmospheric changes are exacerbating air quality issues across North-West India.
Western Disturbances are extratropical storms originating in the Mediterranean region, bringing winter precipitation to North India.
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