WATER VAPOUR HEATS ATMOSPHERE MORE THAN AEROSOLS
Why in News?
- A new scientific study has found that water vapour contributes much more to atmospheric heating than aerosols.
- The study highlights that both aerosols and water vapour must be considered together for accurate climate projections, especially for the Indian Summer Monsoon and regional climate over the Indo-Gangetic Plain (IGP).
BACKGROUND: WHY THIS STUDY MATTERS?
- The Earth’s climate is controlled by its radiation balance.
- Aerosols and water vapour affect this balance by:
- Scattering and absorbing incoming solar radiation
- Absorbing outgoing heat from the Earth
- Understanding their combined radiative effects is critical for:
- Climate modelling
- Weather prediction
- Monsoon behaviour
- Long-term climate stability
INDO GANGETIC PLAIN: A CLIMATIC HOTSPOT
- The Indo-Gangetic Plain (IGP) is one of the most polluted regions in the world.
- It shows:
- Very high aerosol concentration
- Large seasonal and spatial variation in water vapour
- This makes climate prediction over the region complex and uncertain, especially for monsoon rainfall
INSTITUTIONS & RESEARCHERS INVOLVED
- The study was conducted by:
- Aryabhatta Research Institute of Observational Sciences (ARIES), Nainital
- Indian Institute of Astrophysics (IIA), Bengaluru
- International collaborators included:
- University of Western Macedonia
- Soka University
DATA & METHODOLOGY USED
- Data collected from 6 AERONET sites across the IGP.
- AERONET (Aerosol Robotic Network) is a global ground-based system that measures aerosol properties.
- Climate simulations were done using the SBDART (Santa Barbara DISORT Atmospheric Radiative Transfer) model.
- The study analysed Water Vapour Radiative Effects (WVRE) under both:
- Aerosol-free conditions
- Aerosol-loaded conditions
KEY FINDINGS OF THE STUDY
1. Water Vapour Heats the Atmosphere More Than Aerosols
- Water vapour has a stronger atmospheric heating effect than aerosols.
- This makes water vapour a dominant driver of regional climate warming, especially over the IGP.
2. Aerosols Modify Water Vapour’s Impact
- Water vapour radiative effects are:
- Stronger in clean (low-aerosol) atmospheres
- Weakened when aerosol concentration is high
- Aerosols alter how water vapour interacts with solar and terrestrial radiation.
VERTICAL DISTRIBUTION OF HEATING CHANGES
- In aerosol-free conditions:
- Water vapour heating is strong at the surface and within the atmosphere.
- In aerosol-rich conditions:
- Water vapour effects shift more towards the top of the atmosphere.
- This shows a strong interlinkage between aerosols and water vapour.
DEPENDANCE ON SOLAR & ATMOSPHERIC CONDITIONS
- The intensity of heating depends on:
- Solar angle (position of the Sun)
- Aerosol absorption properties
- Atmospheric moisture content
- This explains seasonal variations in heating over the IGP.
CLIMATE IMPLICATIONS
- Water vapour plays a much larger role in atmospheric heating than previously emphasised.
- Ignoring aerosol–water vapour interaction can lead to:
- Errors in climate models
- Poor monsoon rainfall prediction
- Inaccurate future climate projections
SIGNIFICANCE OF INDIAN MONSOON & CLIMATE POLICY
- The Indian Summer Monsoon is highly sensitive to:
- Atmospheric heating patterns
- Vertical temperature gradients
- Since water vapour dominates heating:
- Climate models must integrate both aerosols and water vapour together
- Regional climate strategies must consider air pollution control and moisture dynamics simultaneously
CONCLUSION
- The study clearly establishes that water vapour heats the atmosphere much more than aerosols.
- Aerosols do not act alone but modify the radiative effects of water vapour.
- For reliable climate prediction—especially over pollution-heavy regions like the IGP—a combined aerosol–water vapour approach is essential.
- The findings are crucial for improving monsoon forecasts, climate models, and climate adaptation strategies for India.
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