Features of internal tides observed near the shelf break in the northern South China Sea

• Published in: Ocean dynamics Vol. 69; no. 3; pp. 353 - 365
• Main Authors: Chen, Shengli, Chen, Daoyi, Xing, Jiuxing, Hu, Jianyu, Sun, Zhenyu
• Format: Journal Article
• Language: English
• Published: Berlin/Heidelberg Springer Berlin Heidelberg 11.03.2019; Springer Nature B.V
• Subjects: Atmospheric Sciences; Barotropic mode; Barotropic tides; Diurnal variations; Earth and Environmental Science; Earth Sciences; Fluid- and Aerodynamics; Geophysics/Geodesy; Inertial currents; Internal tides; Monitoring/Environmental Analysis; Mooring; Oceanography; Shear; Summer; Tidal dynamics; Tides; South China Sea; Nonlinear interaction; Internal tides; South China Sea; Near-inertial motions; Mode structure; Fortnight cycle
• ISSN: 1616-7341; 1616-7228
• DOI: 10.1007/s10236-019-01248-4

Features of internal tides in the northern South China Sea are investigated using measurements of two moorings at 506 m (MR1) and 260 m (MR2) working between April and November of 2014. The diurnal internal tides at MR1 are significantly enhanced in June–July and display a regular fortnight modulation, whereas at shallower MR2, the June–July intensification is absent and the fortnight cycle becomes irregular. Fortnight cycle peaks of diurnal internal tides have a regular time-lag of ~ 2.8 days after those of diurnal barotropic tides (at MR1). We derive a mathematical relationship indicating that this time-lag of fortnight cycle peaks is around twice the time for the diurnal internal tides propagating from the generation place to the mooring site. Semidiurnal internal tides are dominated by the mode-1 (~ 70%), while diurnal internal tides exhibit multi-modal structures, with the contribution of ~ 20–30% for each of the first three modes. The diurnal mode-1 contribution varies fortnightly, and eddy passages are highly correlated with the increasing contribution of semidiurnal high modes (at MR1). Furthermore, we find that the nonlinear interaction between internal tides and near-inertial motions is weak in summer, even during periods of strong near-inertial motions (at MR2), because in summer, the shear of near-inertial currents is maximum at a depth shallower than the depth of maximum internal tide shear.