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CSIRO Marine and Atmospheric
Research
Past Seminars
Seminar Abstract
Friday 21 January 2005, 11.30am (Tas time)
CSIRO Auditorium, Hobart and via videoconference to CMR
Floreat and Cleveland
Noel Keenlyside
Leibniz Institute of Marine Sciences at Kiel University, Germany
Improving the simulation of tropical Pacific climate: the
impacts of
biology and a more accurate surface stress calculation
The elusiveness to many coupled general circulation models
(CGCMs) of a realistic simulation of the mean state of the tropical Pacific
has led to the speculation of missing physics. In this study, the effects
of two traditionally neglected processors on the simulation of tropical
Pacific climate, both of the mean and variations about it, are investigated
using the Max-Planck-Institute's climate model.
First, the impact of neglecting surface ocean currents in
the calculation of surface stress is assessed by conducting an experiment
in which they are taken into account. Compared to a control experiment,
without the shear correction, there are several significant improvements:
the model's equatorial SST cold bias is reduced by over 1 degree Celsius
in the western central Pacific; there is a reduction of equatorial interannual
variability of up to 30% to more realistic levels; the dominant period
also increases to around 4 years; and the propagation characteristics
of SST anomalies change from westward to an almost standing pattern.
Second, the impact of neglecting temporal and spatial variations
in optical penetration depth due to ocean biological processes is assessed
by performing an experiment in which the HAMOCC5 biogeochemistry model
is used in the climate model to estimate these variations. Compared to
the simulation with wind shear correction there are several further improvements:
the equatorial cold bias in the eastern Pacific is reduced by Upton 0.5
degree Celsius. The phase of the simulated annual cycle is shifted earlier
by about two weeks, improving the simulation. Interannual SST variability
weakens by a further 15-20%, to even more realistic levels. The dominant
period is lengthened further to around 5 years.
In both cases, the reasons for changes in ENSO characteristics
are due to both changes in the mean state and to changes in the relevant
feedbacks. These shall also be discussed.
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CSIRO = Marine Laboratories Auditorium, Castray Esplanade,
Hobart
For further information, or to schedule a seminar, contact:
Peter Oke,
(Oceanographic seminars) CSIRO Marine Research (03) 6232 5387
Piers Dunstan,
(Biological seminars) CSIRO Marine Research (03) 6232 5382
Katrina Nitschke,
Antarctic Climate and
Ecosystems CRC
(03) 6226 2265 & IASOS,
University of Tasmania (03) 6226 2509
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