GS Paper 1 15 marks · 250w 14 min Medium
“Western disturbances are indispensable to North India’s water and food security, yet increasingly erratic under climate change.” Analyse.
Subtopic: Western disturbances and winter precipitation
How to structure your answer
Introduction → Why they are indispensable → Why they are increasingly erratic → Way forward → Conclusion
Written within the word limit
279 words · target 250 words · 14 min
Western disturbances are extra-tropical cyclonic systems that originate over the Mediterranean and Caspian region and travel eastwards on the subtropical westerly jet, reaching North India between December and March. They supply the winter rainfall that the summer monsoon cannot.
Why they are indispensable
- Rabi lifeline: Winter rain over Punjab, Haryana, western Uttar Pradesh and Rajasthan is critical for wheat, barley, mustard and gram, and reduces irrigation demand at a key growth stage.
- Snow accumulation: They build the Himalayan snowpack that feeds the Indus, Ganga and their tributaries through the lean season.
- Groundwater and reservoir recharge: Winter precipitation supports storage before the pre-monsoon dry spell.
- Air quality and temperature: Associated rain scavenges particulates over the Indo-Gangetic plain, and cold-wave and fog conditions follow their passage.
Why they are increasingly erratic
- Jet stream instability: Arctic amplification is weakening the thermal gradient and making the westerly jet more meandering, so tracks and timing shift.
- Fewer but more intense events: Rain arrives in concentrated bursts rather than gentle spells, causing hailstorms and lodging in standing crops.
- Out-of-season occurrence: Late-season disturbances in March and April damage the ripening rabi crop.
- Cloudbursts and landslides: Interaction with a warmer, moister atmosphere has produced destructive events in Uttarakhand and Himachal Pradesh.
- Snow-to-rain shift: Warmer temperatures mean precipitation falls as rain rather than snow, reducing the stored water that matters most.
Way forward
- Improved extended-range forecasting and district-level agro-advisories.
- Crop insurance and climate-resilient wheat varieties tolerant of terminal heat.
- Slope-stability regulation and early-warning systems in the western Himalaya.
The same system that secures the rabi harvest is now also a hazard. Managing that dual character, rather than treating winter rain as a dependable bonus, is the adaptation challenge.
What an examiner expects to see
- Rabi lifeline: Winter rain over Punjab, Haryana, western Uttar Pradesh and Rajasthan is critical for wheat, barley, mustard and gram, and reduces
- Snow accumulation: They build the Himalayan snowpack that feeds the Indus, Ganga and their tributaries through the lean season
- Groundwater and reservoir recharge: Winter precipitation supports storage before the pre-monsoon dry spell
- Air quality and temperature: Associated rain scavenges particulates over the Indo-Gangetic plain, and cold-wave and fog conditions follow their passage
- Jet stream instability: Arctic amplification is weakening the thermal gradient and making the westerly jet more meandering, so tracks and timing shift
- Fewer but more intense events: Rain arrives in concentrated bursts rather than gentle spells, causing hailstorms and lodging in standing crops
- Out-of-season occurrence: Late-season disturbances in March and April damage the ripening rabi crop
Terminology to weave into the answer
North IndiaUttar PradeshHimachal Pradesh