Generally speaking, the background shear current U（z） must be taken into account in eigenvalue problems of nonlinear internal waves in ocean, as is different from those of linear internal waves. A numerical calculat...Generally speaking, the background shear current U（z） must be taken into account in eigenvalue problems of nonlinear internal waves in ocean, as is different from those of linear internal waves. A numerical calculation method for eigenvalue problems of nonlinear internal waves is presented in this paper on the basis of the Thompson-Haskell＇s calculation method. As an application of this method, at a station （21°N, 117°15′E） in the South China Sea, a modal structure and parameters of nonlinear internal waves are calculated, and the results closely agree with the calculated results based on observation by Yang et al..展开更多
基金山东省科技发展计划项目<不同加热方式对豆浆理化功能性质的影响及其关键生产技术的研究>(2013GNC11307)+5 种基金泰安市科技发展计划欧姆加热豆浆系列产品的研究开发(201640576)"十三五"国家重点研发计划课题大宗油料适度加工与综合利用技术及智能装备研发与示范(2016YFD0401400)山东省2017年度农业重大应用技术创新项目专用植物多肽开发及在调理食品中的应用与示范(310137)山东"双一流"奖补资金资助(Funds of Shandong"Double Tops"Program)山东农业大学作物生物学国家重点实验室开放课题基金<山农糯性小麦粉的品质鉴定与产品开发>(2015KF14)山东省重点研发计划(公益类)"彩麦精深加工技术和新产品研发"(2017GNC10101)
基金supported by the National Natural Science Foundation of China (Grant No. 40706055)
文摘Generally speaking, the background shear current U（z） must be taken into account in eigenvalue problems of nonlinear internal waves in ocean, as is different from those of linear internal waves. A numerical calculation method for eigenvalue problems of nonlinear internal waves is presented in this paper on the basis of the Thompson-Haskell＇s calculation method. As an application of this method, at a station （21°N, 117°15′E） in the South China Sea, a modal structure and parameters of nonlinear internal waves are calculated, and the results closely agree with the calculated results based on observation by Yang et al..
