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海洋内波能量耗散的数值研究
引用本文:刘国涛,尚晓东.海洋内波能量耗散的数值研究[J].海洋石油,2019,39(1):82-87.
作者姓名:刘国涛  尚晓东
作者单位:中海石油(中国)有限公司深圳分公司,广东深圳,518067;中国科学院南海海洋研究所热带海洋环境国家重点实验室,广东广州,510301
基金项目:国家自然科学基金(编号:41630970、41676022、41876022)和中国科学院科研装备项目(编号:YZ201432)。
摘    要:为了研究单频内波在白噪声的干扰下传播时的能量耗散率问题,采用高精度谱方法对其进行数值计算,分析了内波传播过程中内波振幅大小和海水的普朗特数(Pr)对能量耗散率及内波破碎期持续时间的影响。结果显示,内波振幅越大,三个时期(破碎前期、破碎期和破碎后期)的平均能量耗散率越大,内波越早破碎,破碎时间越短;内波在海水中传播,Pr越大,破碎前期平均能量耗散率越小,而破碎期平均能量耗散率越大,破碎时间越短。研究成果可为内波能量耗散率和破碎时间的量化提供理论指导。

关 键 词:能量耗散  内波  连续层化流体  谱方法
收稿时间:2018-10-22

Numerical Study on Energy Dissipation of Ocean Internal Wave
LIU Guotao,SHANG Xiaodong.Numerical Study on Energy Dissipation of Ocean Internal Wave[J].Offshore Oil,2019,39(1):82-87.
Authors:LIU Guotao  SHANG Xiaodong
Affiliation:1.Shenzhen Branch of CNOOC Ltd., Shenzhen 518067, China;2.State Key Laboratory of Tropical Oceanography, South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou 510301, China
Abstract:In order to study the energy dissipation rate of the single frequency internal wave when it is propagated under the interference of white noise,the numerical calculation is carried out by using the high-precision general method.The influence of amplitude and Prandtl number (Pr) on dissipation rate during internal waves propagating and the lasting time of internal waves breaking is analyzed. The results show that the larger the amplitude of internal wave is, the greater the average energy dissipation rate in the three stages (before breaking, breaking, after breaking) is. The earlier the internal waves breaks, the shorter the breaking time is.The internal wave propagates in seawater, the greater Pr is, the smaller the average energy dissipation rate is in the early stage of breaking.The greater the average energy dissipation rate is in the breaking stage, the shorter the breaking time is. The research results can provide theoretical guidance for the quantification of internal wave energy dissipation rate and breaking time.
Keywords:dissipation rate  internal wave  continual stratified fluids  spectral method
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