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OCEAN-ATMOSPHERE INTERACTION: EL NINO AND THE SOUTHERN OSCILLATION. KELSEY HONIOUS AEROSPACE ENGINEERING. Meteorological Aspects of the El nino / Southern Oscillation (Eugene M. Rasmusson & John M. Wallace, 1983). Oceanographic Events

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ocean atmosphere interaction el nino and the southern oscillation

OCEAN-ATMOSPHERE INTERACTION:EL NINO AND THE SOUTHERN OSCILLATION

KELSEY HONIOUS

AEROSPACE

ENGINEERING

Meteorological Aspects of

the El nino/ Southern

Oscillation

(Eugene M. Rasmusson &

John M. Wallace, 1983)

Oceanographic Events

During El Nino (Mark A. Cane, 1983)

a normal southern winter
A Normal Southern Winter
  • The usually cold waters off the coast of Peru and Ecuador experience an increase in temperature near the beginning of the year (usually December or January).
  • The slacking of the Trade Winds causes the currents in the area to slow and the thermocline to deepen, resulting in a buildup of heat in the coastal waters.
along comes el nino
Along Comes El Nino
  • For at least 18 months before an El Nio event, the Easterlies that drive the equatorial currents to the west are stronger than usual.
  • This causes unusually high sea levels in the west Pacific and abnormally low levels in the east.
  • Thermocline in the west deepens
  • SST (Sea Surface Temperature) is warmer than average in the west and colder in the east.
  • When the Easterly winds begin to die down, warming off the South American coast begins as usual.
slide4

Westerly wind anomalies begin in the western and central pacific.

  • These cause a slowing in the equatorial currents, and sea levels begin to fall in the west and rise in the east.
  • Rise of sea levels in eastern Pacific causes flooding in regions of South America.
  • Shift in winds causes storms to move from western Pacific towards east  rain in eastern desert regions while wet regions of the tropical western Pacific experience severe droughts.

Storms

Storms

sst variation during el ni o
SST Variation During El Nio

SST anomaly in degrees Celsius during the months of March through May of an El Nio year.

SST anomalies in the following August -October

SST anomalies in the following December - February

slide6

EL NINO SEA LEVEL VARIATION

Truk, Micronesia

Callao, Peru

Top Panel: Sea level during El Nio events

Bottom Panel:

composite El Nio trend (solid line) and average for non-El Nio years (dotted line)

how the water gets there
How The Water Gets There
  • Decrease in strength of Trade Winds excites clusters of Kelvin waves.
  • Equatorial waveguide allows waves to reach South American coast in a short time without losing much energy.
slide8

By autumn, SST’s at the South American coast are only slightly above normal.

  • Another warming begins in December and peaks early in the following year.
  • The SST then drops drastically, possibly becoming colder than normal.
  • The trade winds begin to pick back up, normal cycle resumes.
the southern oscillation
The Southern Oscillation
  • Atmospheric component of the El Nio event.
  • Fluctuation of pressures over regions on opposite sides of the Pacific. During an event, pressures over west Pacific are unusually high, while pressures over the coast of South America are anomalously low.

Normal Pattern

El Nio Pattern

slide10

Causes and precursors of El Nino are not fully known or understood, nor are the connections of the Southern Oscillation to global weather anomalies associated with the El Nino/Southern Oscillation (ENSO) phenomenon.

  • The two studies shown in this presentation examine the 1982-1983 ENSO event, which was anomalous in its lack of precursors and unusual timeline.
m cane oceanographic events during the 1981 1983 el ni o
M. Cane: Oceanographic events during The 1981-1983 El Nio
  • Wind anomalies usually begin in Fall, but there were not observed Westerlies near the date line until Spring 1982.
  • However, most of the usual signs of El Nino were missing:
    • No unusually strong Easterlies
    • SST not abnormally cold in east or warm in west.
    • Sea levels did not rise in the west or sink in the east.
    • Thermocline not particularly deep in the west.
1982 it begins
1982 : It Begins
  • SST high in early summer, but not above normal variation.
  • By August, SST in east Pacific was substantial, and westerly winds replaced easterlies over much of the equatorial Pacific.
  • As usual, sea level in the west Pacific reached peak in March/April, then began to recede.
  • Instead of rising to second peak in October, western sea level continued to decline drastically.
  • Sea levels in Mid-Pacific normal in June, then rose rapidly (25 cm in less than four months)
  • Rise in sea levels began at South American coast in Sep/Oct.
slide13

In December 1982, the thermocline at the coast of Peru was twice as deep as it had been a year previously.

  • In the months of July – October 1982, the SST in the east Pacific rose 2˚C, while the temperature at depth 100m rose 8˚C.
  • Warming was significant and wide enough the reverse the pressure gradient along the equator, causing the east-flowing Equatorial Undercurrent to disappear for the first time on record.
sst anomalies
SST Anomalies

Time-Longitude Section of SST

Normal Cycle

Cannonical El Nio

1982-1983 El Nio

Off coast of Peru

Singapore

slide15

Composite El Nino wind anomalies. Redlines indicate path of Kelvin Wave. Curve on right indicates sea level change at S. American coast

SST anomaly maps.

Top: Sep-Nov 1982

Bottom: March-May 1983

1983 the e nd
1983: The End?
  • Coastal temperatures continued to rise throughout the normal warming period and beyond.
  • By June 1983 (when this paper was written), temperatures were 6˚C or more above the normal values.
  • Temperatures began the recede in July 1983, wind patterns started to return to normal.
  • SST in much of eastern Pacific still remained much warmer than average.
rasmusson w allace meteorological aspects of enso 1983
Rasmusson/Wallace: Meteorological Aspects of ENSO, 1983
  • Examines the atmospheric occurrences during an ENSO event.
  • Includes results from General Circulation Models (GCM’s), which are capable of realistic global climate simulations.
  • GCM’s have correctly simulated eastward shift of precipitation and upper level circulation patterns during El Nino, as well as teleconnections to extra tropical latitudes.
  • 1982-1983 event gave scientists the chance to check the independent accuracy of the GCM’s.
slide19

Strong SST gradient over equatorial Pacific: warm in west, cold in east. This gradient is associated with thermally direct circulation (Walker Circulation).

    • Sinking motion in the east
    • Westward flow along equator
    • Rising motion and deep convection in west
    • Eastward return flow at cirrus levels.
slide20

Normally, regions of the pacific east of date line receive almost no precipitation, while west gets constant precipitation.

  • During ENSO episode, ocean temperature rise in east and mid-Pacific causes the storms to shift eastward, producing severe droughts in Indonesia, and torrential rainfall in central Pacific.

Note the correlation between A, B, and C

Negative correlation between C and D

it s n ot j ust t he tropics
It’s Not Just The Tropics…
  • Earth’s rotation allows changes in tropical circulation to excite a wave pattern in upper troposphere than can cause anomalies in extra tropical circulation.
the 1982 1983 event
The 1982-1983 Event
  • Surface wind and sea level pressure shifts were not observed in 1981 or early 1982 as per the normal cycle.
  • SST near Peru did not begin sharp rise until Sep/Oct 1982.
  • Sea level pressure in Central Pacific did not begin drop until April 1982.
  • Surface winds shifted to westerly in June 1982.
  • Period of extreme precipitation began in central Pacific.
  • Western Pacific and southern Africa began experiencing record droughts.
slide23

SST anomalies from 1982-1983 episode

Sea level pressure anomalies over Tahiti (central Pacific), and Darwin (Australia)

slide24

Movement of precipitous regions during 1982-83 epsisode as measured by satellite-sensed outgoing long-wave radiation

peak of the episode
Peak of the episode
  • Anomalous patterns intensified from Dec 1982 to Feb 1983.
  • Droughts extended to Hawaii.
  • SST anomalies nearly twice normal ENSO values. (Temperatures above 29° C in shaded areas)
  • Southern Oscillation Index dropped to unprecedented -6
effects on extra tropical latitudes
Effects on extra tropical latitudes
  • Circulation anomalies at jet stream levels (Dec-Feb)
  • In north Pacific, mean sea level pressures reached record lows.
  • The anticycloniccirculation over Canada was associated with unusually mild winter on Canada/U.S. border
slide27

Westerly wind anomalies across subtropical Pacific and southern borders of U.S. indicated intensification and southward movement of normal westerly jet stream.

  • Abnormally high number of winter storms on California coast
  • Flooding in parts of California and Gulf states.
  • Southwest mountain ranges buried under snow in spring.
the e nd finally
The End….Finally.
  • Anomalous rainfall, low pressures in north North Pacific, and storm track across U.S. persisted through May 1983.
  • Southern Oscillation swung back to normal from February to May 1983
  • SST in east Pacific began to fall, but second increase produced peak anomalies above 8˚C in May and June. Decreased drastically in early July, then gradually through September, but still remained above normal.
proposed theory
Proposed theory:
  • ENSO episodes may be superposition of two interrelated events, which usually occur in combination about 6 months apart.
    • Enhancement of mean annual cycle. Positive SST anomalies develop in Jan/Feb and spread west, peaking in May/June, disappearing by Sep/Oct. Response to swing in Southern Oscillation associated with weakening of Trade Winds
    • Broad scale warming of equatorial Pacific starting mid-year and disappearing a few months later. Response to pressure changes caused by swing in Southern Oscillation.
theory continued
Theory Continued…
  • Typical ENSO episode may be an event of type 1 followed, with some overlap, by an event of type 2.
  • The 1982-1983 episode could have been a reverse of the normal sequence, beginning with the broad scale warming in late 1982 and then moving towards localized warming on the South American coast.
summary
Summary
  • 1982-1983 El Nino began later than normal, had much larger amplitude of anomalies, and lingered longer than usual.
  • El Nino may be linked to global scale changes in weather patterns for duration of event.
  • Examination of the ‘82-’83 episode has lead to the proposed theory that El Nino actually consists of two interrelated events, which can possibly come in arbitrary order.
the conclusions
The Conclusions:
  • It cannot currently be proven that El Nino causes consistent extra tropical anomalies.
  • It is not known which of those anomalies in 1982-83 were a direct result of the El Nino and which were simply coincidences.
future research
Future Research
  • Examination of causes behind the violent swings in the Southern Oscillation seen in certain events like the 1983 El Nino.
  • Can ENSO episodes be conclusively related to climate anomalies in other regions of the globe?
  • Is it possible to analyze the singular traits of any given El Nino in order to predict the severity of its effects, and the global reach of its deviations?
  • Will we ever be able to effectively predict an El Nino?