Variability of coherent and incoherent features of internal tides in the north South China Sea

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作者
Bingtian Li
Zexun Wei
Xinyi Wang
You Fu
Qingjun Fu
Juan Li
Xianqing Lv
机构
[1] Shandong University of Science and Technology,College of Ocean Science and Engineering
[2] First Institute of Oceanography,Key Laboratory of Marine Science and Numerical Modeling
[3] Ministry of Natural Resources of China,College of Computer Science and Engineering
[4] Qingdao National Laboratory for Marine Science and Technology,Key Laboratory of Physical Oceanography, Qingdao Collaborative Innovation Center of Marine Science and Technology
[5] Shandong University of Science and Technology,undefined
[6] Ocean University of China,undefined
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Scientific Reports | / 10卷
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摘要
The coherent and incoherent features of internal tides (ITs) in the north South China Sea (SCS) are investigated based on observations and numerical simulations. The 11-month (from May 2011 to March 2012) moored current observations indicate that coherent semidiurnal ITs are obviously amplified, which can be attributed to the interference of ITs. Interference enhances coherent motions of semidiurnal ITs, but weakens those of diurnal ITs. Moreover, observations also show that semidiurnal ITs are more incoherent than diurnal ITs. Variations of vertical stratification and surface tide forcing can hardly affect the incoherence of ITs. The increase of incoherent signal is largely due to the influence of mesoscale eddies. Mesoscale eddies affect both amplitude and phase of ITs, making them more incoherent. Mesoscale eddies not only increase the intensity of background currents, but also induce horizontal variations of density. Variations of horizontal density and the influence of background currents lead to the increase of incoherent signals. And semidiural ITs are more sensitive to the influence of mesoscale eddies, making them more incoherent than diurnal counterparts. Incoherent ITs, which induce strong current shear, play essential roles in cascading tidal energy to small-scale motions, and contribute to turbulent mixing eventually. The findings help to better understand ITs and may offer reference for the improvement of parameterization of ocean turbulent mixing in the northern SCS.
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