A case study of near-inertial oscillation in the South China Sea using mooring observations and satellite altimeter data |
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| Authors: | Lu Sun Quanan Zheng Dongxiao Wang Jianyu Hu Chang-Kuo Tai Zhenyu Sun |
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| Institution: | (1) State Key Laboratory of Tropical Oceanography, South China Sea Institute of Oceanography, Chinese Academy of Sciences, Guangzhou, 510301, Guangdong, China;(2) South China Sea Environment Monitoring Center, South China Sea Branch of State Oceanic Administration, Guangzhou, 510301, Guangdong, China;(3) Department of Atmospheric and Oceanic Science, University of Maryland, College Park, MD 20742, USA;(4) State Key Laboratory of Marine Environmental Science, Xiamen University, Xiamen, 361005, Fujian, China;(5) NOAA NESDIS, WWBG, Camp Springs, MD 20746, USA; |
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| Abstract: | A near-inertial oscillation (NIO) burst event in the west South China Sea (SCS) was observed by an upward-looking mooring
Acoustic Doppler Current Profiler (ADCP) in summer 2004. The mooring station was located at 13.99°N, 110.52°E. The spectral
analysis reveals that typhoon Chanchu is a major mechanism in triggering the NIO burst event. Before typhoon Chanchu passed
over, the NIO signals were quite weak. The NIO band becomes the most energetic constituent of the circulation during the typhoon-wake
period. The average peak power density (PD) reaches (5.3 ± 2.6) × 102 cm2 s−2 (cycles per hour, cph)−1 with a maximum value of 9.0 × 102 cm2 s−2 cph−1, i.e., 3.1 times higher than that of diurnal tide (DT), (1.7 ± 0.5) × 102 cm2 s−2 cph−1. At the upper (80 m) and sub-upper (208 m) layers, the central frequency of the NIO band is 0.022 cph with a blueshift of
about 9% above the inertial frequency f (0.02015 cph). At the lower layer (400 m), the central frequency of the NIO band is 0.021 cph with a blueshift of about 4%
above the inertial frequency. The blueshifts are explained partially by the Doppler shift induced by the vorticity of mesoscale
eddies. During the after-typhoon period, a resonance-like process between NIO and DT is observed in the upper layer. As the
NIO frequency approaches the DT subharmonic frequency (0.5K1), the PD of the NIO band rises sharply accompanied by a sharp drop of the PD of the DT band. The PD ratio of the two bands
increases from 4.5 during the typhoon-wake period to 8 during the after-typhoon period, indicating the effect of the parametric
subharmonic instability (PSI) mechanism. |
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