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CSIRO Marine and Atmospheric
Research
Past Seminars
Seminar Abstract
Friday 9 December 2005, 11.30am (Tas time)
CSIRO Auditorium, Hobart
Jaci Brown
CSIRO Marine and Atmospheric Research
Using sea level to understand El Nino
Previous studies have used warm water volume in the
Pacific Ocean to predict ENSO with a seven month lead time. Warm
water volume data however is only available back to 1980. Sea level
shows a similar performance to warm water volume in predicting ENSO
and now a reconstructed data set of sea level is available back
to 1950 and earlier (Church and White et al. 2004).
Warm water volume is used to understand the recharge/discharge
mechanism of ENSO (Meinen and McPhaden 2000). Sea level can be used
in the same way. Studying this recharge/discharge mechanism back
to 1950 in sea level shows that the formation of El Niño
events altered around the time of the climate regime shift in 1975,
when El Niño events became more intense. It appears that
the recharge/discharge mechanism was less important during this
earlier period and El Niño events began their development
in the east of the basin rather than the central Pacific.
The question then is, has ENSO changed due to natural decadal or
multidecadal variability, or has global warming changed the background
state on which ENSO lies? If global warming is responsible for the
change in ENSO, we may continue to see the intense El Niño
events that have dominated the last twenty years.
We explore the reconstructed sea level data to try to shed light
on these questions, comparing it with other data sets such as SST
and windstress and comparing our results with SODA sea level and
thermocline depths.
References:
Church, J. A., White, N. J., Coleman, R., Lambeck, K. and Mitrovica,
J.X. 2004 'Estimates of the Regional Distribution of Sea Level Rise
over the 1950-2000 Period.' Journal of Climate.17, 2609-2625.
Meinen, C.S. and McPhaden, M.J. 2000 'Observations of Warm
Water Volume Changes in the Equatorial Pacific and Their Relationship
to El Niño and La Niña.' Journal of Climate 13, 3551-3559.
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CSIRO = Marine Laboratories Auditorium, Castray Esplanade,
Hobart
For further information, or to schedule a seminar,
contact:
Karen
Wild-Allen, (Oceanographic seminars) CSIRO Marine and Atmospheric
Research (03) 6232 5010
Piers
Dunstan, (Biological seminars) CSIRO Marine Research (03) 6232
5382
Kerrie Bidwell,
Antarctic Climate
and Ecosystems CRC
(03) 6226 2265 &
IASOS, University of Tasmania (03) 6226 2509
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