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Characteristics of turbulence in the Changjiang River Estuary and its adjacent waters in summer
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Kou Wang1, Bo Li1, *, Aiguo Li2, Penghao Wang3, Shengxin Pei1
Haiyang Xuebao | 2021, 43(11) : 22 - 31
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Haiyang Xuebao | 2021, 43(11): 22-31
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Characteristics of turbulence in the Changjiang River Estuary and its adjacent waters in summer
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Kou Wang1, Bo Li1, *, Aiguo Li2, Penghao Wang3, Shengxin Pei1
Affiliations
  • 1Marine Science and Technology College, Zhejiang Ocean University, Zhoushan 316022, China
  • 2Zhoushan Natural Resources Surveying and Mapping Design Center, Zhoushan 316021, China
  • 3College of Meteorology and Oceanography, National University of Defense Technology, Nanjing 211100, China
Published: 2021-11-25 doi: 10.12284/hyxb2021172
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Using the direct observation data of the MSS90L turbulence profiler obtained in the summer cruise of the Changjiang River Estuary scientific investigation and experimental study (NORC2019-03-02) in July 2019, in this paper, the distribution of the turbulent kinetic energy dissipation rate ε and the vertical turbulent diffusion coefficient Kz are calculated and analyzed. The turbulent kinetic energy dissipation rate is 1.72×10−10 W/kg to 2.95×10−5 W/kg, and the vertical turbulent diffusion coefficient is 3.24×10−7 m2/s to 4.55×10−2 m2/s. The distribution of the turbulent kinetic energy dissipation rate and the vertical turbulent diffusion coefficient are similar, both of which are the strongest in the upper layer, the next in the bottom layer and the weakest in the middle layer. In the upper layer, due to wind stress, the turbulent kinetic energy dissipation rate and vertical turbulent diffusion coefficient are larger; the stratification is stronger at the thermocline, which suppresses the dissipation of turbulent kinetic energy and vertical turbulent mixing. The secondary circulation of the salinity front will promote the separation of the low salt water mass, and the vertical circulation caused by the front will enhance the turbulent mixing of the ocean. The energy exchange between the low salt water mass and the outside world is less, and the turbulent kinetic energy dissipation rate is weaker. There are obvious upwelling and downwelling in the Changjiang River Estuary, which are produced by the secondary circulation of the front; the existence of upwelling and downwelling promotes the dissipation of turbulent kinetic energy and turbulent mixing.

Changjiang River Estuary  /  thermocline  /  turbulent kinetic energy dissipation rate  /  vertical turbulent diffusion coefficient  /  salinity front
Kou Wang, Bo Li, Aiguo Li, Penghao Wang, Shengxin Pei. Characteristics of turbulence in the Changjiang River Estuary and its adjacent waters in summer[J]. Haiyang Xuebao, 2021 , 43 (11) : 22 -31 . DOI: 10.12284/hyxb2021172
Year 2021 volume 43 Issue 11
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Article Info
doi: 10.12284/hyxb2021172
  • Receive Date:2021-01-17
  • Online Date:2026-02-26
  • Published:2021-11-25
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  • Received:2021-01-17
  • Revised:2021-05-25
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Affiliations
    1Marine Science and Technology College, Zhejiang Ocean University, Zhoushan 316022, China
    2Zhoushan Natural Resources Surveying and Mapping Design Center, Zhoushan 316021, China
    3College of Meteorology and Oceanography, National University of Defense Technology, Nanjing 211100, China
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表12种不同金属材料的力学参数

Family
属数
Number of
genus
种数
Number of
species
占总种数比例
Percentage of
total species (%)

Genus
种数
Number of
species
占总种数比例
Percentage of total
species (%)
鹅膏菌科Amanitaceae 2 11 5.26 鹅膏菌属 Amanita 10 4.78
小菇科 Mycenaceae 2 12 5.74 丝盖伞属 Inocybe 5 2.39
多孔菌科 Polyporaceae 8 14 6.70 蜡蘑属 Laccaria 5 2.39
红菇科 Russulaceae 3 23 11.00 小皮伞属 Marasmius 6 2.87
小菇属 Mycena 11 5.26
光柄菇属 Pluteus 5 2.39
红菇属 Russula 17 8.13
栓菌属 Trametes 5 2.39
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