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mass of warm surface water moving west to
east across equatorial Pacific Ocean
part of larger phenomenon called El Niño –
Southern Oscillation (ENSO)
• El Niño occurs every 3 to 8 years
• Usually lasts about 1 year
• Scientists do not know why pressure
changes causing winds to shift
• Warm water arrives at South America
around Christmas – hence El Niño –
for the Christ Child
NORMAL SITUATION OVER PACIFIC
OCEAN
(NON-El Niño YEAR)
• Low pressure over Asia
• High pressure over South America
• Winds blow east to west
• Shallow thermocline along South
America, lots of upwelling, cold water
at surface
• Deeper thermocline near Asia, warm
surface water piles up
EL NINO YEARS OVER PACIFIC
OCEAN:
• Pressure change = Southern Oscillation
• Higher pressure over Asia
• Lower pressure over South America
• Winds weaken or blow west to east
• Thermocline deepens along South
America, little upwelling, warmer
water at surface
• Warm surface water sloshes back along
equatorial Pacific
SEA SURFACE TEMPERATURE IN
PACIFIC OCEAN
EFFECTS OF EL NINO

• upwelling along Peru reduced
• warm water with few nutrients rises
• fisheries decline
EFFECTS OF EL NINO
• increased precipitation over parts of
South America, western and
southern U.S.
• can result in severe flooding
• drought in Australia, Indonesia,
Phillipenes
• reduction in annual monsoons in India
• can result in severe crop damage
• severe property damage and thousands
of deaths

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El niño

  • 1. mass of warm surface water moving west to east across equatorial Pacific Ocean part of larger phenomenon called El Niño – Southern Oscillation (ENSO)
  • 2. • El Niño occurs every 3 to 8 years • Usually lasts about 1 year • Scientists do not know why pressure changes causing winds to shift • Warm water arrives at South America around Christmas – hence El Niño – for the Christ Child
  • 3. NORMAL SITUATION OVER PACIFIC OCEAN (NON-El Niño YEAR) • Low pressure over Asia • High pressure over South America • Winds blow east to west • Shallow thermocline along South America, lots of upwelling, cold water at surface • Deeper thermocline near Asia, warm surface water piles up
  • 4.
  • 5. EL NINO YEARS OVER PACIFIC OCEAN: • Pressure change = Southern Oscillation • Higher pressure over Asia • Lower pressure over South America • Winds weaken or blow west to east • Thermocline deepens along South America, little upwelling, warmer water at surface • Warm surface water sloshes back along equatorial Pacific
  • 6.
  • 7.
  • 8. SEA SURFACE TEMPERATURE IN PACIFIC OCEAN
  • 9. EFFECTS OF EL NINO • upwelling along Peru reduced • warm water with few nutrients rises • fisheries decline
  • 10. EFFECTS OF EL NINO • increased precipitation over parts of South America, western and southern U.S. • can result in severe flooding • drought in Australia, Indonesia, Phillipenes • reduction in annual monsoons in India • can result in severe crop damage • severe property damage and thousands of deaths