I. Introduction
The ocean turbulence plays an important role in cognizing the process of ocean circulation and significantly improving climate modeling. It also has a significant impact on the study of marine ecological environment and the distribution of suspended materials [1]. The ocean turbulence has grown up to be an important subject in the marine science research. Conventionally, the measurements of turbulence and mixing are usually limited to surveys of short time’ duration and the samples are incomplete and sporadic [2]. Therefore, turbulence measurements for long-term periods are needed to improve our understanding of the ocean mixing process on ocean circulation dynamics. So the technologies for long-term measurements are becoming increasingly important.