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内潮
    A NUMERICAL STUDY ON DYNAMIC MECHANISM OF INTERNAL TIDE
    内潮动力机制的数值研究
    Estimates of M_2 internal tide energy fluxes in the Pacific Ocean using TOPEX/Poseidon altimeter data
    利用TOPEX/Poseidon高度计资料提取的太平洋M_2内潮能通量分布
    The intense of internal tide in the Luzon Strait is due to topographic features and the characteristic of M2 tide.
    吕宋海峡M_2内潮响应强烈是由于其地形和M_2潮波的特征所决定的;
    A nonlinear three-dimensional numerical model is used to simulate the distribution of the internal tide( M_2, S_2, K_1, O_1 )in the Bohai Sea, the Yellow Sea and the East China Sea. The result show that semidiurnal frequence internal tides mainly in two areas, one side of the west of Korean Peninsula waters, another is the north-east of Taiwan (Okinawa Haicao) waters.
    使用三维非线性数值模型(将海洋分为2层)研究了潮汐( M_2, S_2, K_1,O_1分潮)作用下渤黄东海的内潮,揭示了整个海区内潮起伏的空间分布,结果半日内潮主要分布2个区域:一个是朝鲜半岛西侧海域,一个是台湾东北(冲绳海槽)海域。
    The characters of ocean internal waves (IWs) are obtained by analyzing the ASIAEX2001 temperature data. The M2 internal tide, internal solitary wave packets with “periods”of 10-30min, and a couple of internal solitary wave packets are observed.
    为探讨声学方法监测 (反演 )海洋内波的可行性 ,分析ASIAEX2 0 0 1亚洲海海洋声学实验定点温度链实验数据 ,结果表明 :实验期间存在M 2内潮波、周期 10~ 3 0min非线性内波现象 ,并观测到双温跃层同相传播“双非线性内波”。
    The Study of the Internal Tide 3-D Numerical Simulation with Assimilation in the South China Sea
    南海内潮三维数值同化模拟
    A PRELIMINARY ANALYSIS ON INTERNAL TIDE CHARACTERISTICS AT AN OBSERVATION POINT IN NORTHERN SOUTH CHINA SEA
    南海北部—观测点内潮特征的初步分析
    Progress in the Observational Studies of Internal Tide over Continental Shelf
    近海陆架区内潮观测研究进展
    It has handsome progress about ocean internal tide studying and surface tide assimilation model based on TOPEX/POSEIDON satellite altimeter data.
    近年来,已有学者开始高度计资料提取大洋内潮和表面潮的数值同化研究,并取得了许多成果。
    Then we get internal tide signals from them based on the characteristic of internal tide.
    基于内潮的特征,把内潮在海面响应的信息分离出来;
    The semi-diurnal and diurnal internal tide energy densities are large on the continental shelf and in the thermocline of the deep sea.
    较强内潮在陆坡区超临界地形上生成,并沿波射线方向传播,导致半日潮和全日潮的能量密度在陆坡区温跃层上较强。
    The East China Sea and adjacent seas are one of the most significant generation regions of the internal tide in the world’s oceans.
    在全球的海洋中,中国东海和临近海域是最显著的内潮生成地之一。
    Mainly caused by the influence of diurnal tidal constituent, it has the characteristics of diurnal internal tide, a period of about 24 hours, and a propagation direction to the north in general.
    结果表明,观测点存在着一种内潮现象,其波动的周期在24h左右,它传播的方向大体是偏北。
    A two-layer mathematical model on generation and propagation of internal solitary waves indued by tide is derived based on the two-layer model of internal tide and considering non-static balance of perturbation pressure.
    在二层内潮数学模型的基础上,考虑非静力平衡扰动压力的影响,导出潮频内孤立波产生、传播的数学模型。
    (3) The strongest abrupt current appears when the internal tide has the largest amplitude,which is 4 or 5 days later than the occurrence of spring tide.
    ( 3)最强的突发性海流发生于斜压内潮强盛期 ,比天文大潮落后 4— 5d。
    In the paper, based on the hydrologic background of the existence of internal tide inthe Nansha Islands sea area, a two layer model is set up, and some numerical experiments are done to study the generation mechanism of internal tide forced by a barotropic tide wave;
    本文结合南沙群岛海域出现内潮的水文背景 ,建立了一个两层数值模式 ,并通过数值试验来探讨由正压潮波作用下的内潮产生机制。
    The results show that bottom topographic effect is an important factor for generation of internal tide;
    结果表明 :底形效应是促使内潮产生的重要因子 ;
    internal tide propagates in the direction of continental shelf and abyssal plain after forming in the continnental slope;
    内潮主要在大陆坡产生 ,然后分别沿着大陆架和深海平原两个方向传播 ;
    Internal solition is the large amplitude wave existing in the pycnocline induced by internal tide in the condition of special bottom topography.
    孤立子内波是由内潮在特殊地形条件下所激发的存在于密度跃层中的大振幅波动。
    For the later, it is shown that an internal tide causes adjacent (acoustic) mode coupling, but nonadjacent mode coupling can be caused by internal solitary wave packets.
    平行于内波传播方向的声传播计算结果表明 :内潮波主要导致相邻简正波间耦合 ;
 

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