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Objectives
learn
how El Niño and La
Niña work
emphasize that the ocean
& atmosphere are
strongly coupled
understand that one
component of the Earth’s
system can have drastic
effects on the rest of the
Earth
El Niño: The Enigma
Unusual
oceanic and atmospheric
phenomenon - an anomaly
–We don’t know everything about it
–We can’t really predict it yet
El Niño: The Term
First
discovered in 1795
Recognized by local fisherman along
Ecuador and Peru
–Warm, surface countercurrent
–North-->South
–Discovered around Christmas-time
–“The Christ Child”
El Niño Characteristics
Normally
develops in W. tropical
Pacific
Often results in natural disasters
Occurs every 2 to 10 years
Most recent and severe events in
1953, ‘57-’58, ‘65, ‘72-’73, ‘76-’77, ‘82’83, ‘91-’92, ‘97-’98, ‘02-’04, ‘06-’07,
’09’10
Slides from 1982-’83 El Niño
INDEX =
• Air temperature
• Sea surface temp
• Surface winds
• Cloudiness of sky
• Sea level pressure
-09-’10
Elevated
Sea Surface
Suppressed
Sea Surface
“Southern Oscillation” (SO)
Tradewinds
weaken or fail
Tropical winds reverse and go east
instead of west
Atmospheric pressure cells reverse
–Wet areas become dry (drought)
–Dry areas get flooded
“oscillates”
like a giant sea-saw,
taking 3-5 months
Non El Niño
El Niño
Coupled Ocean-Atmosphere
Circulation
Non El Niño
El Niño
Ocean’s Response to the SO
Warm
water moves to the east
Elevates sea surface temperatures
(SSTs) in SE Pacific
Shuts down upwelling, can induce
downwelling
Reduces available nutrients
Kills fish and sea birds - especially
bad off Peru
Animations
Ocean AND Atmosphere
El
Niño is both an oceanic and an
atmospheric phenomenon
–Often called ENSO
Scientists
knew of SO from wind and
precip. data
Scientists knew of El Niño from SST
data
Didn’t make connection until 1969
Jacob Bjerknes
Jacob
Bjerknes, a Norwegian
meteorologist made breakthrough in
1969
Combined wind, rain, AND SST data
Ocean & atm. part of “big climate
engine”
Effects of ENSO not just local to Peru
but could affect whole Pacific, whole
world
Interdisciplinarity Rules!
Bjerknes
was a meterologist who
was willing to take a good, hard look
at oceanographic data
Oceanography a versatile science
How Do We Track El Niño Today?
in
situ (on site) measurements
Satellite sea surface temperature
Computer models
Autonomous Temperature Line Acquisition System
Tropical Ocn Global Atm
Tropical Atm-Ocn
La Niña
NOT
tied to the Southern Oscillation
Tradewinds get stronger
SSTs are lowered in SE Pacific
Normal conditions are exaggerated
– Dry areas get drier (drought)
– Wet areas get wetter (floods)
Occurs
in between El Niños
INDEX =
• Air temperature
• Sea surface temp
• Surface winds
• Cloudiness of sky
• Sea level pressure
El Niño AND La Niña
Both
an ocean/atmosphere
phenomenon
Both affect wind, rain, and SST
Both occur in cycles
More Animations
El Niño VERSUS La Niña
“Southern
Oscillation”
Tradewinds fail
Reverse flow of air
Elevated SST
Upwelling decreased
Fish die
Dry areas flood
Wet areas dry up
No
oscillation
Tradewinds increase
No reverse flow
Decreased SST
Upwelling increased
Fish thrive
Dry areas get drier
Wet areas flood
Lesson to be Learned
Earth
phenomena are very much
interrelated
Ocean <----> Atmosphere
Bjerknes’
concept of “teleconnections”
We must understand in order to predict
Invest in soybean futures after an El Niño!
– No fish meal for cattle, farmers will use soy
We’re dealing with the interplay between two
very different fluids - atmosphere and ocean - in
the boundless dimensions of time and space. ...
Abnormality in one causes abnormality in the
other.... Events such as El Niños have no definite
starting point and no end. It’s a matter of where
you break into the scene, and where you leave it.
Perhaps the only thing more complex is human
behavior itself.
-- Dr. Jerome Namias, Scripps
Institution of Oceanography