Analysis on the vertical mixing structure of Xiangxi River during early winter
YANG Zhong-yong1,2, QIAN Men-liang1, JI Dao-bin1,2, ZHOU Zhe-xuan1, YAO Shi-min3, FAN Zhong-ya4
1. College of Hydraulic & Environmental Engineering, China Three Gorges University, Yichang 443002, China; 2. Three Gorges Reservoir Ecosystem Hubei Province Field Scientific Observation and Research Station, Three Gorges University, Yichang 443002, China; 3. Key Labratory of River Regulation and Flood Control, Ministry of Water Resources, Changjiang River Scientific Research Institute, Wuhan 430010, China; 4. Water Environment Research Center, South China Institute of Environmental Sciences, Ministry of Ecology and Environment, Guangzhou 510665, China
Abstract:Based on the measured data of hydrology and meteorology at the Xiangxi River Xiakou site from November 29 to December 15, 2018, the vertical mixed structure of the water body during a typical cooling process in the early winter of the Xiangxi River and the heat at the water-air interface were discussed, including the contribution mechanism of flux and wind stress. The vertical mixing structure of Xiangxi River during this period showed significant weak layering during the day and strong mixing at night, and the daytime layering period was quite short, only occurred around noon within 4 hours. The contribution of the energy input or dissipation process at the water-air interface to the stratified mixing process of the water body was significantly greater than the mechanical disturbance effect of the wind stress on the water body. Solar short-wave radiation was the main contribution for the surface water body to absorb heat during the day and thereby stratify the driving force, long-wave radiation was dominant in the heat release process during night. The latent heat and sensible heat processes also played a non-negligible role in the heat release process of the water body. The influence of wind stress on the mixing mode of the water body by mechanical disturbance was mainly concentrated in the surface water body has extremely limited impact on the middle and lower layers, but it could significantly enhance the mixing characteristics of the water body by affecting the latent heat and sensible heat. Due to the low water temperature of the Xiangxi River during the study period, the evaporation heat release was small, and the water-temperature difference was relatively low. Larger, the turbulent energy flux driven by wind stress through sensible heat was slightly larger than latent heat.
杨忠勇, 钱门亮, 纪道斌, 周哲轩, 姚仕明, 范中亚. 香溪河初冬降温过程中垂向混合结构特征分析[J]. 中国环境科学, 2021, 41(6): 2862-2870.
YANG Zhong-yong, QIAN Men-liang, JI Dao-bin, ZHOU Zhe-xuan, YAO Shi-min, FAN Zhong-ya. Analysis on the vertical mixing structure of Xiangxi River during early winter. CHINA ENVIRONMENTAL SCIENCECE, 2021, 41(6): 2862-2870.
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