Behind an early summer is a lack of winter rains

Why in the News?

An unusual surge in temperatures across north and north-western India during February-March has raised concerns about shifting seasonal patterns. Several regions recorded temperatures 8-13°C above normal, bringing heat-wave-like conditions weeks before the usual onset of summer. The phenomenon has been linked to deficient winter rainfall and weak Western Disturbances, which are critical for regulating winter climate in north India. 

Why is India witnessing unusually high temperatures early this year?

1. Temperature Anomaly: Several regions recorded temperatures 8-13°C above normal, reaching heat-wave-like conditions in February-March.
2. Early Heat Conditions: Warm weather replaced cool winter days earlier than usual in northern and western India.
3. Rare Occurrence: A similar situation occurred three years ago, but such an early onset of summer remains relatively uncommon.
4. Regional Evidence:
   1. Shimla: 25.3°C (March 2026, highest recorded till March 8).
   2. Pahalgam: 22.7°C.
   3. Gulmarg: 17.2°C.
   4. Srinagar: 24.7°C.

Climatological Significance: Heat waves are generally uncommon in high-altitude regions such as Shimla in March.

How did weak Western Disturbances influence the winter climate?

1. Western Disturbances: East-moving rain-bearing weather systems originating beyond Iran and drawing moisture from the Mediterranean Sea and other water bodies.
2. Seasonal Importance: These systems normally bring winter rainfall and snowfall across northern India.
3. Deficiency Since November 2025: Reduced frequency and intensity of Western Disturbances led to lower winter precipitation.
4. IMD Observation: Meteorologists noted lack of wind convergence between westerly and easterly winds, reducing moisture transport into north and central India.
5. Temperature Regulation: Winter precipitation normally moderates temperatures by maintaining soil moisture and atmospheric cooling.

Why was the winter of 2026 considered unusually dry?

1. Rainfall Deficit: All-India rainfall during January-February was only 16 mm, which is 60% below normal.
2. Historical Context: February 2026 became the third driest February since 1901.
3. Snowfall Decline: Both snowfall and rainfall remained subdued across Himalayan regions.
4. Meteorological Cause: Persistent lack of favourable weather systems during winter months.

How does a dry winter accelerate the onset of summer?

1. Soil Moisture Deficit: Reduced rainfall leaves soil dry and unable to moderate temperature increases.
2. Evaporation Mechanism: Moist soils normally evaporate moisture before heating up, delaying temperature rise.
3. Rapid Surface Heating: Dry soils heat faster, increasing land surface temperature and accelerating summer conditions.
4. Climate Feedback: Dry land conditions amplify regional warming and heat stress.

What are the implications for agriculture and water resources?

1. Impact on Rabi Crops: Sudden temperature spikes affect mustard, wheat, gram, groundnut, sesame, sorghum, and sunflower.
2. Horticulture Stress: Crops such as potatoes and apples may suffer due to heat stress.
3. Irrigation Demand: Farmers have been advised to increase irrigation frequency to maintain soil moisture.
4. Water Resource Pressure: Increased irrigation demand may strain local groundwater and water reserves.

What do temperature records indicate about changing climatic patterns?

1. Temperature Extremes: High temperatures in Himalayan regions during early March indicate increasing climate variability.
2. Comparison with Past Years:
   1. 2026: Shimla 25.3°C, Pahalgam 22.7°C, Gulmarg 17.2°C, Srinagar 24.7°C.
   2. 2025: Shimla 24.4°C, Pahalgam 20.4°C.
   3. 2024: Shimla 24.8°C.
3. Climate Signal: Frequent anomalies suggest greater unpredictability in seasonal transitions.

Conclusion

The early onset of summer in India highlights the critical role of winter rainfall and Western Disturbances in maintaining seasonal balance. Reduced precipitation has accelerated land heating and increased agricultural vulnerability. Strengthening climate monitoring, improving irrigation management, and integrating seasonal forecasting into agricultural planning are essential to mitigate the impacts of such climatic anomalies.

PYQ Relevance

[UPSC 2017] Climate Change’ is a global problem. How will India be affected by climate change? How will Himalayan and coastal states of India be affected?

Linkage: The early onset of summer due to weak winter rains and Western Disturbances reflects climate variability affecting Himalayan regions, highlighting changing temperature and precipitation patterns.