摘要
通过改进海床阻力系数和设置合适的垂向紊动背景系数,应用FVCOM模型成功再现了钱塘江河口强涌潮的演进过程。海床阻力系数采用Manning公式形式,取值随水深、地形在0.000 2~0.002 9之间变化;垂向紊动背景系数取1×10^(-4) m^2/s。模拟结果较好地复演了涌潮到达时刻、涌潮高度及涌潮抬升过程、涌潮水平流速以及其沿垂向分布规律,表明阻力系数及垂向紊动背景系数等关键参数的改进和处理是合理的,可应用于涌潮三维潮流运动特征模拟。
The evolution of tidal bore in Qiantang Estuary were successfully reproduced by applying FVCOM model through improving the sea bed roughness coefficient and setting suitable background vertical eddy viscosity.Sea bed roughness coefficient,calculated using the Manning formulation,is between 0.000 2~0.002 9 with the varying depth.The background vertical eddy viscosity is 1×10^-4 m^2/s.The simulation well reproduces the tidal bore arriving time,tidal level,setup height,horizontal velocity magnitude and vertical profile,which implies the choice of parameters such as the bed roughness coefficient and background vertical eddy viscosity are reasonable.The procedure could be extended to simulate the 3D tidal movement for tidal bores.
出处
《海洋学研究》
CSCD
北大核心
2017年第1期33-40,共8页
Journal of Marine Sciences
基金
国家自然科学基金项目资助(51379190)
水利部公益性行业专项项目资助(201001072)
浙江省省属科研院所专项计划项目资助(2016F50018)
浙江省科技厅创新团队与人才培养项目资助(2012F20031)
浙江省公益技术应用研究计划项目资助(2016C33095)