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Numerical Simulation of Coastal Oceanic Response to Typhoon Forcing
Error propagation from winds to ocean models was numerically investigated using
the Princeton Ocean Model (POM) for the South China Sea with 20-km horizontal
resolution and 23 sigma levels conforming to a realistic bottom topography during the
lifetime of tropical cyclone Ernie (November 4-18, 1996). Numerical integration was
divided into preexperimental and experimental stges. The preexperiment phase generates the initial
conditions on November 1 for the sensitivity experiment. During the experimental stage the POM
was integrated from November 1 to 30, 1996 under National Centers for Environmental Prediction (NCEP)
reanalyzed surface fluxes along with two surface wind data sets, namely, the daily averaged interpolated
NASA scatterometer winds and the NCEP winds. The relative root-mean-square differences fluctuate from 0.5
to 1.0 for winds, 0.25 to 0.7 for surface elevations, 0.47 to 1.02 for surface currents, and
0 to 0.23 for surface temperatures. This indicates that the model has less uncertainty overall
than the wind fields used to drive it, which in turn suggests that the ocean modeling community
may progress without waiting for the atmospheric modelers to build the perfact forecast model.
Dr. Chu is developing methodology to examine the impact of high
resolution coastal winds (see Section on Data System) on Navy's
operational Shallow Water Analysis and Forecast System (SWAFS) which
was developed from POM.
Reference:
Chu, P., J.M. Veneziano, C. Fan, M.J. Carron, W.T. Liu, 2000: Response
of the South China Sea to tropical cyclone Ernie 1996. J. Geophys. Res.,
105, 13,991-14,009.
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Last Updated: 06 Sep 2005 JPL Clearance: CL 03-0447 |
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