Believable b values and η values were tested, and frequency seismological anomalies and fixed point tidal deformation anomalies were found before strong mining-induced earthquake in the short-term and impending stages.

1、

This paper adopts a method of numerical simulation, taking Huangmaohai estuary as calculated example, to calculate tidal deformation due to shore reclamation.

本文采用潮流数值模拟的方法，以中国华南的珠江口黄茅海河口为例，进行边摊围垦后湾内期波变形的模拟计算。

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2、

The problem of surface tidal deformation of the earth is expanded to that in the interior of the earth.

把地球表面潮汐形变问题扩展到地球内部。

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3、

The Short-Impending Anomaly Patterns of Tidal Deformation and Its Time-Space Characteristics

潮汐形变短临异常图像及其时空特征

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4、

Research on distinguishing method and mecha-nism of tidal deformation anomalies before large earthquakes

强震前形变潮汐异常判识与机理研究半个世纪前，G.术前ASE

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5、

Love functions and their derivatives and tidal deformation in the interior of the earth

Love函数与地球内部的潮汐形变

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6、

Study on the change mechanism of the digital earth tidal deformation before earthquake

地震前数字形变固体潮变化机理的研究

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7、

Tidal deformation of a self-rotating, elliptical, heterogeneous earth

自转微椭、非均匀地球的潮汐变形

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8、

At a given location, however, the strength of the tidal current is generally proportional to the relative tidal range for that day.

然而，在一定的地点，潮流强度一般与那一天的相对潮差成正比。

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9、

This paper proposed that the tidal datum near the tide station could be used to divide the suitable mudflat height for mangrove afforestation. This method avoided using some blur conceptions such as high tide flat, middle tide flat and low tide flat once used.

提出利用邻近验潮站的潮汐基面划分各树种的宜林（造林）滩涂高程的方法，克服了以往通常用高、中、低潮滩表示的模糊概念；

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10、

Doubt and Discussion on the Actual Tidal Datum of Pearl River Estuary

珠江口现行潮汐基准面的质疑与探讨

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11、

Some preliminary research and discussion for the distribution of tidal station and the application of tidal data

验潮站的布设和潮位资料应用中若干问题的初步探讨

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12、

ADI ( Alternating Direction Implicit) method is used to solve tidal wave equation and data assimilation numeric trial experimentation is performed. Compared with the results obtained by ADI method, the assimilated results have better improvement.

用有限差分隐式方向交替（Alternating Direction Implicit，ADI）法求解潮波方程，并进行数据同化的数值试验，与未经同化的ADI法计算值相比有较好的效果。

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13、

The point of this article: On the basis of the gains obtained by the former researches, the oceanic tides loading effects are obtained with the latest precise ocean tidal models and the data of china seas.

本文特点：在前人研究成果的基础之上，利用最新的由卫星测高资料所获得的高精度的海潮模型和中国近海资料研究海潮负荷效应。

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14、

The tidal effect of the data is analyzed, and the interference factors are presented.

分析了该井水位观测资料潮汐效应，同时指出了影响该井水位观测质量的干扰因素，加深了对怀4井水位资料的认识，有助于今后分析预报水平的提高。

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15、

Based on the tidal level observational data in China's coastal area in the past decade, the paper makes statistics of the annual mean processes and correlates them with the relevant meteorological data and literature for comparison and analysis.

根据我国沿海近10多年来潮位观测数据进行年均过程的统计，同时与有关气象资料和文献进行了联系比照分析。

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16、

A method is presented, by which the plane strain state on the earth's surface can be obtained with the combination of tidal line strain data and the tidal shear strain can be simulated numerically.

提出了由潮汐线应变的组合观测资料获取地表平面应变状态和对潮汐剪切应变进行数值模拟的方法。

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17、

The tidal level data from 21 tidal stations in radial sand ridge sea area of Jiangsu Province are analyzed by use of G-Godin's tidal harmonic analysis and prediction programs revised by M Foreman, and the harmonic constants of 11 constituents and corresponding mean sea level are obtained.

Foreman改进的G.Godin潮汐调和分析程序对江苏省辐射沙洲海域21个验潮站潮位资料进行调和分析，得到了11个分潮的调和常数及相应平均海平面。

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18、

The tidal height data of 16 tide surveying sites in Jiangsu radial sand ridge sea area are analysed and predicted respectively using the G · Godin ′ s tidal height analysis and prediction programs revised by Foreman.

利用MForeman改进的G·Godin潮汐调和分析及预报程序对江苏省辐射沙洲海域的16个验潮站潮位资料进行了调和分析和潮汐预报。

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19、

By using 11 global ocean tide models and tidal gauge data obtained in the East China Sea and South China Sea, the influence of the ocean loading on gravity field in China and its neighbor area is calculated in this paper.

利用11个全球海潮模型和中国东海及南海近海潮汐资料，计算了海潮负荷对中国及邻区重力场的影响，进而讨论了用近海潮汐资料修正全球海潮模型对负荷结果的影响。

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20、

In the part of calculation of current field of the system, we used POM calculation mode for tidal current data.

在系统潮流计算部分，利用POM模式计算得到南海潮流数据。

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