ORIGINAL RESEARCH article
Front. Mar. Sci.
Sec. Physical Oceanography
Volume 12 - 2025 | doi: 10.3389/fmars.2025.1643170
Variability of turbulent mixing observed by high-resolution Acoustic Doppler Current Profilers in the deep South China Sea
Provisionally accepted- 1Ocean University of China, Qingdao, China
- 2Joint Institute for Regional Earth System Science and Engineering, University of California, Los Angeles, United States
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Despite turbulent mixing plays a crucial role in sustaining the global meridional overturning circulation, direct observations of turbulent mixing are sparse, especially in the deep ocean. In this study, we used 1200 kHz Acoustic Doppler Current Profilers (ADCPs) with high temporal (O(1s)) and spatial (O(2cm)) resolution to obtain continuous measurements of turbulent mixing at a depth of 1086 m in the northeastern South China Sea. Through comparative experiments and the evaluation of four different analysis methods, we provided optimal configurations and effective methodologies for continuous observations of turbulent mixing accompanied by shear background flow in the deep ocean. Our continuous observations revealed large temporal fluctuations in the near-bottom turbulent kinetic energy dissipation rates, varying by up to two orders of magnitude within a single day. These fluctuations were dominated by shear instability associated with high-mode diurnal internal tides. These findings contribute to developing optimized observational methodologies, enhancing our understanding of deep-ocean turbulence and its implications for large-scale oceanic dynamics.
Keywords: turbulent mixing, high-resolution Acoustic Doppler Current Profiler, deep ocean observations, Elliptic Approximation Model, Internal tides, South China Sea
Received: 08 Jun 2025; Accepted: 29 Jul 2025.
Copyright: © 2025 Xun, Zhou, Xiao, Guan, Huang, Qu, Zhao and Tian. This is an open-access article distributed under the terms of the Creative Commons Attribution License (CC BY). The use, distribution or reproduction in other forums is permitted, provided the original author(s) or licensor are credited and that the original publication in this journal is cited, in accordance with accepted academic practice. No use, distribution or reproduction is permitted which does not comply with these terms.
* Correspondence: Chun Zhou, Ocean University of China, Qingdao, China
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