tidal surface

During the spring tide, the tidal current speed on surface layer reaches 190cm/ s, which is close to the theoretical value.

动态优化潮流广义潮流计算大潮期间，表层的潮流流速190cm/s已接近理论值。

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The effect of Stokes drifts can be represented as additional current on the tidal current. Surface layer is mostly influenced. The influence becomes weak with the increase of water depth.

Stokes漂流对于潮流的影响，相当于在潮流流速上添加一附加的流动，表层影响最大，随着深度的增加，影响逐渐减弱。

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Static deformation response of the earth to tidal potential, surface mass loading and shear stress

地球对引潮力位、表面负荷及切向应力的变形响应

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Ammonia nitrogen adsorption isotherm of tidal flat surface sediments from the Yangtze Estuary

河口潮滩沉积物对氨氮的等温吸附特性

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There were obviously temporal change and spatial distribution of matrix-bound phosphine in the tidal flat surface sediments of the Yangtze Estuary.

长江口滨岸潮滩表层沉积物中基质结合态磷化氢的含量存在明显的时空分布差异。

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Distribution of polychlorinated biphenyls ( PCBs) and organochlorine pesticides ( OCPs) in the tidal beach surface sediments of Yangtze estuary

长江口潮滩表层沉积物中PCBs和OCPs的分布

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The energy sources and sinks for the oceanic general circulation include tidal forces, sea surface atmospheric pressure variations, wind stress, heating and cooling at the upper surface, freshwater flux, and geothermal heat flux.

驱动大洋环流的能源和能汇包括潮汐，海表大气压力脉动，风应力，海表加热和冷却，海表淡水通量，以及海底地热。

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Small fluctuation of tidal flat surface, sediments of tidal flat surface and its cohesiveness all can influence the depositional configuration of shell sediments, especially the glomerate socket and steep chimb.

另外，潮坪表面的细微起伏、潮坪底质类型和粘结性都会对贝壳的沉积形态造成较大影响，其中尤其是以密集窝状和陡坎状为特征。

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Study on Surface Water Environmental Capacity and Quantity Control of Pollution within Tidal River Network

平原感潮河网地区地表水环境容量及污染物总量控制研究

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Recurrence relations of the surface spherical harmonics in the development of the tidal generating potential

引潮位展开中的面球谐函数及其递推公式

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The equation of continuity is then used to further get a 2-order elliptical equation satisfied by sea surface elevation, and the unpenetrable condition at the shore wall of semi-closed sea area is also derived by means of tidal level.

然后利用连续性方程进一步得到了海面升高即潮位所满足的二阶椭圆型方程，进而导出了以潮位形式给出的半封闭海区岸壁不可穿透条件。

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Altimeter data were corrected with tidal model and was interpolated in spatial domain to obtain time series data. 3D energy-frequency-time spectrum and sea surface anomaly ( SSA) were obtained by HHT from time series data.

对南海卫星高度计资料进行潮汐校正和空间插值得到时间序列数据，对这些时间序列数据进行HHT，得到了南海海平面高度变化的三维能量-频率-时间谱和海平面高度距平（SSA）。

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According to engineering arrangements which is surface drainage and deep intake, carrying out experiments systematically on different tidal range, different depths and different upstream flow run off to research the thermo-hydraulic behaviours. 4.

针对表排深取的工程布置，对不同潮差、不同水深、不同上游来流量情况下的温排放水力热力特性进行了潮位、流速和温度的物理模拟。

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