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Three cases: (1) La Nina event in 1989 (2) A strong El Nino in 1998

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Three cases: (1) La Nina event in 1989 (2) A strong El Nino in 1998 (3) A moderate El Nino in 1987 Three fields: (a) Surface temperatures and anomalies ( b ) Sea level pressure and anomalies ( c ) Precipitable water and anomalies. Colder than average. Lower than average pressure. - PowerPoint PPT Presentation
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Three cases: (1) La Nina event in 1989 (2) A strong El Nino in 1998 (3) A moderate El Nino in 1987 Three fields: (a) Surface temperatures and anomalies (b) Sea level pressure and anomalies (c) Precipitable water and anomalies
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Page 1: Three cases: (1) La Nina event in 1989 (2) A strong El Nino in 1998

Three cases:(1) La Nina event in 1989(2) A strong El Nino in 1998(3) A moderate El Nino in 1987

Three fields:(a) Surface temperatures and anomalies(b) Sea level pressure and anomalies(c) Precipitable water and anomalies

Page 2: Three cases: (1) La Nina event in 1989 (2) A strong El Nino in 1998

Colder than average

Page 3: Three cases: (1) La Nina event in 1989 (2) A strong El Nino in 1998
Page 4: Three cases: (1) La Nina event in 1989 (2) A strong El Nino in 1998

Lower than average pressure

Page 5: Three cases: (1) La Nina event in 1989 (2) A strong El Nino in 1998
Page 6: Three cases: (1) La Nina event in 1989 (2) A strong El Nino in 1998

Drier than average

Page 7: Three cases: (1) La Nina event in 1989 (2) A strong El Nino in 1998
Page 8: Three cases: (1) La Nina event in 1989 (2) A strong El Nino in 1998
Page 9: Three cases: (1) La Nina event in 1989 (2) A strong El Nino in 1998
Page 10: Three cases: (1) La Nina event in 1989 (2) A strong El Nino in 1998
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Page 20: Three cases: (1) La Nina event in 1989 (2) A strong El Nino in 1998

Not all events have same amplitude…best to think of an analogy between El Nino and La Nina and summer and winter: there are things common to each winter to make it a useful concept, but each one is different owing to different weather, different amplitudes of temperature extremes, etc.

El Ninos, particularly strong ones, are generally confined to a single 12 month interval. La Ninas may persist for a few consecutive years, so there the oscillation is not linear in nature.

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Page 22: Three cases: (1) La Nina event in 1989 (2) A strong El Nino in 1998

NOAA/NCEP/CPC

Page 23: Three cases: (1) La Nina event in 1989 (2) A strong El Nino in 1998

NOAA/NCEP/CPC

Page 24: Three cases: (1) La Nina event in 1989 (2) A strong El Nino in 1998

NOAA/NCEP/CPC

Page 25: Three cases: (1) La Nina event in 1989 (2) A strong El Nino in 1998
Page 26: Three cases: (1) La Nina event in 1989 (2) A strong El Nino in 1998

• Westerly Wind Bursts (like from an MJO) cause an ocean response

Page 27: Three cases: (1) La Nina event in 1989 (2) A strong El Nino in 1998

Delayed Oscillator Theory• Initially, Kelvin is

downwelling (bringing warmer SSTs), and Rossby is upwelling

• Rossby is much slower than Kelvin

• At reflection, wave type shift

• Key: The reflected Rossby from maritime continent becomes an UPWELLING Kelvin

• “Seeds of its own demise”

• If this were the only thing happening, would get a very regular oscillation

Page 28: Three cases: (1) La Nina event in 1989 (2) A strong El Nino in 1998

A real example

Page 29: Three cases: (1) La Nina event in 1989 (2) A strong El Nino in 1998

There must be more…

• Clearly there must be other companion mechanisms, with input from atmosphere, to get us to 3-5 (2-7) year irregular cycles– The original feedback theory– Recharge/discharge theory – Heat builds up in the

equatorial region, discharged eastward and poleward during El Niño

• Lots of other theories (text), and active research

Page 30: Three cases: (1) La Nina event in 1989 (2) A strong El Nino in 1998

Monitoring

• 3.4 is frequently used because of signal of both convection and SST

• 1&2 warm first!

Page 31: Three cases: (1) La Nina event in 1989 (2) A strong El Nino in 1998

SOI = Tahiti - Darwin (normalized)

Page 32: Three cases: (1) La Nina event in 1989 (2) A strong El Nino in 1998

Niño Region SST Departures (oC) Recent Evolution

The latest weekly SST departures are:

Niño 4 -1.2ºC

Niño 3.4 -1.6ºC

Niño 3 -1.8ºC

Niño 1+2 -2.0ºC

Page 33: Three cases: (1) La Nina event in 1989 (2) A strong El Nino in 1998

SOI and Nino 3-4 index

Page 34: Three cases: (1) La Nina event in 1989 (2) A strong El Nino in 1998

Jet stream configur-

ations

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Global Effects

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Mean number of days per season (November - March 1948 through 1993) in which precipitation exceeded 0.50 inches for Neutral years (top). Lower left map is the difference in this quantity between El Niño years and Neutral years. Lower right map is the difference in this quantity between La Niña years and Neutral years.

North American

Effects


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