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dc.contributor.authorChen, Yuchun
dc.contributor.authorChu, Peter C.
dc.contributor.authorLu, Shihua
dc.date1998
dc.date.accessioned2013-09-11T23:03:08Z
dc.date.available2013-09-11T23:03:08Z
dc.date.issued1998
dc.identifier.citationChu, P.C., S.H. Lu, and Y.C. Chen, 1998: Wind-driven South China Sea deep basin warm-core/cool-core eddies (paper download). Journal of Oceanography, Oceanographic Society of Japan, 54, 347-360.).
dc.identifier.urihttp://hdl.handle.net/10945/36172
dc.descriptionJournal of Oceanography, Oceanographic Society of Japan, Vol. 54, pp. 347-360.).en_US
dc.description.abstractThe formation of the South China Sea (SCS) deep basin warm-core and cool-core eddies was studied numerically using the Princeton Ocean Model (POM) with 20 km horizontal resolution and 23 sigma levels conforming to a realistic bottom topography. Numerical integration was divided into pre-experimental and experimental stages. During the preexperimental stage, we integrated the POM model for three years from zero velocity and April temperature and salinity climatological fields with climatological monthly mean wind stresses, restoring type surface salt and heat fluxes, and observational oceanic inflow/outflow at the open boundaries. During the experimental stage, we integrated the POM model for another 16 months under three different conditions: one control and two sensitivity runs (no-wind and no lateral transport). We take the fields of the last 12 months for analysis. The simulation under control run agrees well with earlier observational studies on the South China Sea surface thermal variabilities. In addition, the sensitivity study further confirms that the wind effect is the key factor for generation of the SCS deep basin warm/cool eddy and that the lateral boundary forcing is the major factor for the formation of the strong western boundary currents, especially along the southeast Chinese coast during both summer and winter monsoon seasons.en_US
dc.rightsThis publication is a work of the U.S. Government as defined in Title 17, United States Code, Section 101. Copyright protection is not available for this work in the United States.en_US
dc.titleWind-driven South China Sea deep basin warm-core/cool-core eddiesen_US
dc.typeArticleen_US
dc.contributor.departmentOceanographyen_US
dc.subject.authorSouth China Sea, primitive equation model, warm-core eddy, cool-core eddy, wind effect, lateral boundary effect.en_US


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