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Measurement and Analysis of Vertical Mixing and Stratification Within the Plume Outside the Changjiang River Estuary
NI Zhi-Hui-1, CHEN Hui-1, DONG Li-Xian-2, SHI Zhong-1, WANG Dian-Zhi-1, DI Qiang-1
2012, 46 (11):
1862-1873.
A field study was conducted at Station E4 (122°40′8″E, 30°59′17″N) within the plume outside the Changjiang River estuary from 17:00, Sept. 17 to 17:00, Sept. 18, 2002. Based on the relevant equations available in the literature, density, buoyancy frequency and the gradient Richardson number were estimated from flow velocity (speed and direction),conductivity (salinity) and temperature obtained by 300 kHz Acoustic Doppler Current Profiler (ADCP) and ConductanceTemperatureDepth Probe (CTD). Vertical profiles of velocity components, salinity, temperature, density, buoyancy frequency and the gradient Richardson number were plotted so as to elucidate the vertical mixing and stratification within the plume outside the Changjiang River estuary. Results show that ① the WE component of velocity varies from -0.36 to 0.61 m/s, the NS component of velocity varies from -0.59 to 0.39 m/s. Velocity components vertically vary little during maximum flood tide, maximum ebb tide and low slack water while during high slack water velocity components show significant difference from the surface layer to the bottom layer. ② Salinity increases while temperature decreases with water depth during maximum flood tide and high slack water from the surface layer to the bottom layer. Maximum temperature occurs at the middepth during low slack water. A significant pycnocline appears during maximum ebb tide. ③ Waters within the plume of the Changjiang River estuary seem to be wellmixed with small values of the buoyancy frequency (in the order of 10-3 s-1) at the upper layer and weaklymixed with relative large values (in the order of 10-2 s-1) at the mid and lower layers. ④ The intensity of vertical mixing displays flood/ebb tidal variability: relative weaklymixed with the gradient Richardson number in the order of 10-2~101 during maximum flood tide and high slack water, intense stratification with large values of gradient Richardson number (in the order of 102) at the mid and lower layers during maximum ebb tide. Most values of the gradient Richardson number are smaller than the critical value 0.25, suggesting that waters within the plume are well mixed during low slack water.
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