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WATER VAPOUR HEATS ATMOSPHERE MORE THAN AEROSOLS

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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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