珠江三角洲径潮相互作用下潮能的传播和衰减
[Abstract]:Due to the interaction of runoff and tide, the energy fluxes of delta waterways include net fluxes caused by runoff and tidal energy fluxes caused by tides. In this paper, a harmonic analysis model based on diameter-tide coupling is established based on synchronous measurement data of multi-section measured water level and discharge in the Pearl River Delta. The total tidal energy and M2s of each station are calculated by stripping off runoff signals. The propagation and attenuation of tidal energy in Pearl River Delta are studied by using K-1 and high frequency shallow water tidal energy. The results show that the tidal wave energy entering the Pearl River Delta through Humen accounts for about 51.2 percent, while the tidal energy through the Yamen, Jiaomen and Modaomen accounts for about 37 percent. At the same time, because of topography friction and energy dissipation effect of runoff, the total energy loss of each channel in the delta is 148.33 MW. Tidal wave energy propagates and attenuates along different positions of delta according to convergent type and dispersed type. The tidal energy of Humen Lion Ocean and Pearl River, Yamen to Tanjiang River Shizui is dispersed into different branches along the course, and the attenuation of total tidal energy in section is greater than that of single wide tide energy flux. The average attenuation rate of the kinetic energy along the course of a single wide tide is greater than that of the potential energy of the tide, and the attenuation rate of the tidal energy of the semidiurnal component is greater than that of the whole day. Due to its morphological influence, the attenuation of M2 tidal amplitude (or potential energy) is the least, and the increase of Humen to Simeng circumference section, with an average increase of 0.77 meters per kilometer. The tide energy of Xisikoumen is converged on the Tianhe section of the Xihai waterway, and the attenuation rate of the total tidal energy is smaller than that of the single wide tidal energy of the Motaiaomen waterway. Along Hengmen, Hongqimen and Jiaomen, the tidal waves entering into the river converge and disperse. The attenuation rate of the tidal energy from Hengmen to Siu Lam, South China, Nansha to Haiwei and Rongqi is smaller than that of tidal potential energy, and the single wide tidal kinetic energy and the kinetic energy of the M2K1 component are smaller than the tidal potential energy. The potential energy of high frequency tidal component increases along the range.
【作者单位】: 中山大学海洋学院河口海岸研究所;河口水利技术国家地方联合工程实验室;
【基金】:国家自然科学基金(41106015)
【分类号】:P731.23
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