TRIPLE DIP LA-NINA 

Why in the News? A recent study has revealed that the unprecedented triple dip La-Niña had peculiar impact on air quality in peninsular as well as North India.

More on News:

  • The recent triple-dip La Niña conditions (2020–2023) had widespread impacts on the ocean and climate across the globe. 
  • During the winter of 2022–23 that coincided with retreating phase of the triple dip La-Niña, India experienced a peculiar trend in Air Quality: 
    • Poor Air quality in peninsular India: The dominance of higher northerly wind in the transport level forces influx and relatively slower winds near the surface, trapping pollutants and notably increasing PM2.5 concentration. 
    • Improved Air quality in North India: Weaker western disturbances, and unique wind patterns with the absence of rain and clouds and faster ventilation led to a significant improvement in air quality in the North. 
  • Observations were contrary to trends seen in recent decades, where in winter northern parts of the country witness increased pollution levels. 

About Triple dip La Niña:

  • A triple-dip La Niña is a rare event that occurs when the La Niña effect lasts three years in a row. 
  • La Niña is a phase of the El Niño Southern Oscillation (ENSO). 
About El Niño Southern Oscillation (ENSO):

    • ENSO is a naturally occurring large-scale climatic phenomenon involving fluctuating ocean temperatures in the central and eastern equatorial Pacific (referred as El Niño and La Niña), coupled with changes in the overlying atmosphere (referred to as Southern Oscillation). 
  • ENSO has 3 phases: La Nina, El Nino and Neutral

La Niña: A cooling of the ocean surface with below-average sea surface temperatures (SST), in the central and eastern tropical Pacific Ocean.

  • La niña causes the jet stream to move northward and to weaken over the eastern pacific. 
  • The normal easterly winds along the equator become even stronger.
  • In general, the cooler the ocean temperature anomalies, the stronger the La Niña (and vice-versa). Its Impacts are:
    • It enhances the nutrient-rich cold water up-welling off the coast of Peru and Ecuador.
    • It causes better than normal Monsoon in India and sometimes may also cause floods.

El Niño: It is the reverse of La Niña. A warming of the ocean surface with above-average SST, in the central and eastern tropical Pacific Ocean.

  • Easterly winds along the equator weaken or in some cases reverse to westerly winds.
  • In general, the warmer the ocean temperature anomalies, the stronger the El Niño (and vice-versa). Its Impacts are:
    • It results in suppression of the nutrient-rich cold water up-welling off the coast of Peru and Ecuador. 
    • It weakens the Indian Monsoon and may also cause drought. 

About Neutral: 

  • Neither El Niño or La Niña. 
  • Often tropical Pacific SSTs are generally close to average.
  • However, there are some instances when the ocean can look like it is in an El Niño or La Niña state, but the atmosphere is not playing along (or vice versa).

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