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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

Monthly events and exam calendar context
Static GK and one-liner notes
Quiz and mock-test revision path

Key points

Exam-ready takeaways

North India experienced a warm and dry winter attributed to weak Western Disturbances (WDs).

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.

How to study

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Revise monthly events by exam family instead of reading random updates.

Pair one-liners with mock tests so mistakes become the next revision list.

Note which exams each story matters for, and revise it again in the week before that exam.