Atmospheric rivers are partly responsible for devastating floods in India | Current Affairs | Vision IAS
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    Atmospheric rivers are partly responsible for devastating floods in India

    Posted 07 Aug 2024

    2 min read

    Scientists warn that intensification and increased frequency of atmospheric rivers due to global warming is worsening extreme rainfall events and weather patterns.

    Atmospheric rivers (AR)

    • AR, also called as ‘flying rivers’, are relatively long, narrow regions in the atmosphere that transport most of the water vapour outside of tropics. 
      • An average AR is about 2,000 km long, 500 km wide and nearly 3 km deep.
    • ARs are a part of larger system of extratropical cyclones that transport heat and moisture from tropics toward the poles.
      • ARs are typically located within low-level jet, an area of strong winds in lower atmosphere.
    • They are largest transport mechanisms of freshwater on Earth, responsible for 90% of moisture transfer from tropics to poles.
    • While many ARs are weak systems, some larger and strong ARs can create extreme rainfall and floods, causing mudslides and catastrophic damage. 

    Climate Change and Atmospheric Rivers

    • With temperature increase, intensity of rain events rises because of increase in atmosphere’s moisture retention capacity.
    • By 2100, ARs are predicted to become more intense globally and will be much broader and longer.
    • Intensified ARs can produce drought like conditions by removing rainfall from rainfall-dependent regions.

    Impact of ARs on India

    • Seven of India's 10 most severe floods in monsoon seasons between 1985 and 2020 were associated with ARs.
    • Increase in extent of fog and haze in Indo-Gangetic plains (IGP) has been linked to rising pollution and water vapour (due to intrusion of ARs). 
    • Declining snow albedo in Hindukush-Karakoram-Himalayan Mountain Range as increased rainfall speeds up snow melting.
    • Tags :
    • Atmospheric River
    • Albedo
    • Extratropical Cyclone
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