South China Sea Isopycnal-Surface Circulation

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Authors
Chu, Peter C.
Li, Rongfeng
Subjects
Advisors
Date of Issue
2000-09
Date
September 2000
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Language
Abstract
This paper investigates the seasonal variabilities of the South China Sea isopycnal-surface circulations and of the Kuroshio intrusion through the Luzon Strait using the U.S. Navy’s climatological temperature and salinity dataset (public domain) with ½° x ½° resolution by the P-vector method. The representative pattern is a persistent basin-scale cyclonic circulation away from the surface, and a seasonally varying circulation with a weak anticylonic gyre in the summer and a strong cyclonic gyre in the winter near the surface. This pattern is consistent with a classical view of mean cyclonic circulation in large stratified lakes and semienclosed marginal seas by Emery and Csanady and with a recent numerical simulation using the navy’s Layered Ocean Model by Metzger and Hurlburt. The computed monthly volume transport through the Luzon Strait is negative (inflow) all year round with a minimum value of 213.7 Sv in February (strongest intrusion) and a maximum value of 21.4 Sv in September (weakest intrusion). The annual mean transport is 26.5 Sv (intrusion).
Type
Article
Description
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Department
Organization
Naval Postgraduate School
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Sponsors
Funder
Office of Naval Research NOMP Program
Naval Oceanographic Office
Naval Postgraduate School
Format
21 p.
Citation
Chu, Peter C., and Rongfeng Li. "South China Sea isopycnal-surface circulation." Journal of Physical Oceanography 30.9 (2000): 2419-2438.
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This 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.
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