Skip to main content

Geography

El Niño–Southern Oscillation (ENSO) and Climate Variability

Climate: Insolation, Atmospheric Circulation, Humidity, Precipitation

Paper II · Unit 3 Section 8 of 12 0 PYQs 32 min

Public Section Preview

El Niño–Southern Oscillation (ENSO) and Climate Variability

7.1 Normal Pacific Circulation

Under normal (La Niña-like) conditions:

  • Trade winds blow strongly westward across the tropical Pacific
  • Warm water piles up in the western Pacific (Indonesia, Australia) — sea surface temperature (SST) 28–30°C
  • Cold, nutrient-rich water upwells along Peru-Ecuador coast — supports world's richest fishery
  • Walker Circulation: Air rises over warm western Pacific → moves eastward at altitude → descends over cool eastern Pacific → surface trades complete the cell
  • Result: Heavy rainfall over Indonesia/Australia; dry Peru coast

7.2 El Niño ("The Child" in Spanish)

Occurs every 2–7 years, roughly around Christmas (hence the name "El Niño" — the Christ child):

  • Trade winds weaken or reverse
  • Warm water spreads eastward across central and eastern Pacific
  • Eastern Pacific SST rises 2–5°C above normal
  • Walker Circulation disrupted or reversed

Global Impacts of El Niño

Region Impact
India Weakened monsoon → drought (1987, 2002, 2009 El Niño years coincided with monsoon deficiency)
Australia Drought; increased wildfire risk (SE Australia); reduced rainfall
Indonesia Drought; forest fires; haze over SE Asia
Peru/Ecuador Heavy rainfall; floods (normally arid coast becomes wet)
East Africa Above-normal rainfall in Kenya, Tanzania
NE Brazil Drought in the semi-arid Nordeste
Global temperature El Niño years are typically warmest years globally (1997–98, 2015–16 — both record-breaking warmth)

7.3 La Niña ("The Girl")

Opposite of El Niño — trade winds strengthen, warm water piles even more in western Pacific, and eastern Pacific SST drops below normal.

Global Impacts of La Niña

  • India: Stronger monsoon → above-average rainfall (good for agriculture)
  • Australia: Severe flooding (2010–11 La Niña — Queensland floods)
  • East Africa: Drought
  • Global: Slightly cooler than El Niño years

Southern Oscillation Index (SOI): Measures atmospheric pressure difference between Tahiti (eastern Pacific) and Darwin, Australia (western Pacific). Positive SOI = La Niña; Negative SOI = El Niño.