目前对潮汐的研究方法主要分为：潮汐调和分析和潮汐动力学两个方面。
At present, there are mainly two ways to study tide: one is the harmonic analysis method of tides, the other is tidal dynamics.
而河床地形变化引起的三角洲河网区潮汐动力增强，则是感潮河段低水位上升的主要原因。
The strengthening of the tidal power caused by the significant topographic change is responsible for the rise of the low water levels in the tidal reach.
找到一个方法，利用塞文河的潮汐动力很重要，因为这将意味着这对英国在2020年产生的所有35%的电力来自可再生能源的目标迈出了一大步。
Finding a way to harness the power of the Severn's tides is important as it would represent a big step towards Britain's target of generating 35% of all electricity from renewable sources by 2020.
研究结果表明：在北槽口内，最大浑浊带形成的主要动力过程是潮汐的不对称性和河口重力环流。
Results suggest that the dominant dynamic processes responsible for the formation of the turbidity maximum are tidal asymmetry and gravitational circulation at the mouth of the North Passage.
在现代动力作用和地貌形态组合研究基础上，进行了潮汐汊道动力地貌学分类。
Based on the study of modem dynamic and combination of landform, tidal inlet is classified by dynamic geomorphology system.
波浪、潮汐和风暴潮是近岸海域最重要的动力要素，在风暴潮过程中，三者通过不同的机制相互影响，互相制约。
The wave, tide and storm surge are the most important dynamic processes in nearshore zone, these three dynamic factors interact in different ways in the storm surge process.
影响长江口盐水入侵的主要动力要素是上游径流和外海潮汐。
The main dynamic factors affecting the Changjiang River mouth saltwater intrusion are upstream runoff and out sea tide.
设计的依据是河流动力学中侵蚀、沉积和潮汐的原理。
The design is based on the river water dynamics, the erosion and sedimentation process and the tides.
本文根据潮汐河网地区水体的水动力、水质特性，建立了河网一维水动力学和水质耦合模型。
A one-dimensional hydrodynamic and water quality model for river networks is developed, according to hydraulics and water quality features of water body within a tidal river network.
对其相变模式研究表明，河口湾沉积特征及岩相分布受波浪、潮汐和河流三种水动力所控制。
Study on the facies models indicates that sedimentary features and the distribution of lithofacies are controlled by the interplay between Marine processes (waves and tides) and fluvial processes.
对其相变模式研究表明，河口湾沉积特征及岩相分布受波浪、潮汐和河流三种水动力所控制。
Study on the facies models indicates that sedimentary features and the distribution of lithofacies are controlled by the interplay between Marine processes (waves and tides) and fluvial processes.
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