同潮 meaning in Chinese
cotidal line
high water
Examples
- The tide and the tidal current in luoyuan bay can be known from the numerica model calculation
给出了同潮时线与等振幅线、潮流椭圆、最大潮流及不同时刻潮流场分布。 - The co - current charts of main constituents show that the m2 component currents have one current - amphidromic point at 29 18 ' n , 122 46 ' e , and the co - phase lag lines rotate anti - clockwise here
主要分潮的潮流同潮图表明： m _ 2分潮流在29 18 n ， 122 46 e处有一个圆流点，同潮时线在该处以反时针旋转。 - Semi - diurnal constituent is the dominant component tides in this area . the co - tidal and co - range charts show that neither semi - diurnal constituents nor diurnal constituents have tide - free points . only the shallow constituents m4 and ms4 respectively have three and two tide - free points
各分潮的潮汐同潮图表明：在本海域内，半日和全日分潮都没有出现无潮点，唯浅海分潮m _ 4和ms _ 4分别有三个和两个无潮点。 - This method is better than the traditional method that relates the divergence of sediment transport rate to the deposition rate . the output of the tidal modelling reaches the required precision according to a comparison between the calculated tidal amplitudes / phases and the observed ones at 42 coastal tide gauge stations
潮汐潮流的模拟计算结果与沿岸42个潮汐测站的实测值结果对比达到了精度的要求，同时，计算得到的各分潮同潮图与实测结果相符。 - After validating the good agreement between simulated results and observed ones , the characteristics and the distribution rules of tides and tidal currents in the whole seas near to zhejiang are thoroughly analyzed , mainly based on the simulated results , combining with the observed conclusion . the co - tidal and co - range charts , co - current charts , types of tides and tidal currents , distribution of maximum possible tidal range and maximum possible tidal current , phenomenon of diurnal inequality , moving modes of tidal currents , tidal ellipses , distribution of tidal residual currents and the vertical structure of tidal currents and residual currents are investigated respectively . and thereout we draw a series of meaningful conclusions as follows , the main of these are : 1
在验证模拟与实测符合良好的基础上，本文以模拟计算结果为主，结合实测资料的分析结论，对整个浙江近海的潮汐、潮流特征和分布规律作了全面、深入的探讨，分别对各主要分潮的潮汐同潮图、潮流同潮图、潮汐性质、潮流性质、最大可能潮差分布、潮汐日不等现象、最大可能流速分布、潮流的运动形式、潮流椭圆、余流分布以及潮流和余流的垂向结构等进行了研究，并由此得到了一系列有意义的结论。