El Nino La Nina
El Nino La Nina
Online
Geo file 569
Paul Warburton
Causes of an El Niño
Source: The International Research Institute for Climate and Society
In the tropical Pacific, trade winds GeoFile Series 26 Issue 3
generally drive the surface waters Fig 569_01 Mac/eps/illustrator 11 s/s
NELSON THORNES PUBLISHING
westward (Figure 2). The surface Figure 2: Normal conditions in Artist:
the Pacific basin Illustration
David Russell
water becomes progressively warmer
going westward, because of its longer
North America
exposure to solar heating. El Niño is Asia
Polar jet
observed when the easterly trade Subtropical
winds weaken (Figure 3), allowing the jet
warmer waters of the western Pacific
to migrate eastward and eventually Warm
Strong trade
winds
reach the South American coast. The water
cool water normally found along the Low Equatorial currents (strong)
Cool
water Ecuador
coast of Peru is replaced by warmer pressure Peru
water. At the same time the area of Strong South
warmer water further west near Australia
High Peruvian America
pressure Current
Australia and Indonesia is replaced by
cooler water.
GeoFile Series 26 Issue 3
Figure 3: Conditions during an El Niño event
Fig 569_02 Mac/eps/illustrator 11 s/s
What is the difference NELSON THORNES PUBLISHING
between La Niña and El Artist: David Russell Illustration
Polar jet
Niño? Wetter than
average winter
Both terms refer to large-scale changes Subtropical
jet
in sea-surface temperature across the
Weak trade
central and eastern tropical Pacific. winds
Usually, sea-surface readings off South Pressure
increases
America’s west coast range from about Strong counter current Warm
15°C to 21°C, while they exceed 25°C Drier than
water
the west during La Niña. The El Niño Figure 4: Broad climate impacts of El Niño
Southern Oscillation (ENSO) is the
coupled ocean-atmosphere process Northern hemisphere winter
that includes both El Niño and La Key
Niña. Wet
Dry
Warm
What causes La Niña? 60°N
50°
Typically, a La Niña is preceded by a 40°
build-up of cooler than normal 30°
subsurface waters in the tropical 20°
Pacific. Eastward-moving 10°
atmospheric and oceanic waves help EQ
10°
bring the cold water to the surface 20°
through a complex series of events, 30°
still being studied. In time, the 40°
easterly trade winds strengthen, cold 50°S
upwelling off Peru and Ecuador 00° 20°E 40° 60° 80° 100° 120° 140° 160° 180° 160°W 140° 120° 100° 80° 60° 40° 20°
intensifies, and sea-surface
temperatures (SSTs) drop below
normal. During the 1988-89 La Niña, Northern hemisphere summer
SSTs fell to as much as 4°C below Key
normal. Both La Niña and El Niño Wet
Dry
tend to peak during the Northern Warm
Hemisphere winter. 60°N
50°
error coupled with El Niño has led to Figure 5: Australian wheat yields and SOI index (SOI is a measure of the intensity
environmental disaster in Indonesia of an El Nino event)
and other south east Asian countries.
Logging companies in Indonesia 1.6 20
have been clearing areas of forest by
deliberately setting fire to them. 15
Normally, regular rainfall would 1.4
dampen down the flames and prevent
10
the spread of fires. El Niño has the
effect of stopping rains from reaching 1.2
Indonesia, so fires have spread out of
Tonnes/hectare
control. Huge clouds of smoke have
caused unprecedented levels of smog, 1.0 0
and at times made the air in certain
areas of southeast Asia extremely –5
dangerous to breathe. There have 0.8
also been devastating effects on
–10
wildlife, with thousands of creatures
dying. 0.6
–15