孙昭晨

个人信息Personal Information

教授

博士生导师

硕士生导师

性别:男

毕业院校:大连理工大学

学位:博士

所在单位:水利工程系

学科:港口、海岸及近海工程

电子邮箱:sunzc@dlut.edu.cn

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OCEAN TURBULENT MIXING IN NORTHERN BOHAI STRAIT, CHINA

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论文类型:会议论文

发表时间:2013-06-09

收录刊物:EI、CPCI-S、Scopus

卷号:5

关键字:Bohai strait; turbulent energy dissipation rate; heat dissipation rate; turbulent mixing rate; thermal diffusivity coefficient

摘要:The measurements of ocean microstructure through which ocean internal mixing mechanism is revealed are taken more often recently. Free-falling turbulence microstructure profiler TurboMAP-9 is used to take a field observation on the area of northern Bohai Strait. 13 stations distributed in Bohai Sea, Yellow Sea and the "division line" between them are measured. Turbulent mixing characteristics of northern Bohai Strait for different seasons are described by analyzing the observation data of ocean turbulence microstructure profile. The results show that the northern Bohai Strait is a strong mixing area during non-stratification period. Turbulent energy dissipation rate epsilon of winter is bigger than that of autumn and it is strongest near the bottom layers which is in the order of 10(-5)W/kg. Heat dissipation rate chi(theta) is in the same order of 10(-6)-10(-5)degrees C-2/s in autumn as 6 and 2-3 orders smaller than 6 in winter. Thermal diffusivity coefficient k(theta) is a little bigger than turbulent mixing rate k(rho) in autumn and 1-2 orders smaller than k(rho) in winter. Both the k(rho) and k(theta) along the "division line" of Bohai Sea and Yellow Sea are bigger than that of the Bohai Sea and Yellow Sea. Base on the measured data and the analysis, heat dissipation rate and thermal dispersion coefficient can change 2-3 orders in nonstratification seasons which should be paid much attention to, especially for ocean model parameterization and pollutant discharge modeling.