潮汐

基本解释 (translations)

tide  ·  tiding  ·  tided  ·  tides

词组短语

morning and evening tides

与潮汐相关的网络例句 [注：此内容来源于网络，仅供参考]

The scale-value, which is converted from the bore-hole strain, by nse of the observed values in tidal frequency band of the bore-hole strain and the elastic coefficients of the bore-hole corescan can be used for coverting non-tidal variation of the bore-hole strain into variation of the non-tidal stress of the same stratum.

顾梦林 ，杨毅，骆鸣津利用钻孔应变观测值中潮汐频段部分和钻孔岩芯的弹性系数，将钻孔应变换算为地层应力的格值，用此格值可将钻孔应变的非潮汐变化换算成该地地层的非潮汐应力变化。

The cause of the earth tide force is its elliptic orbit movement. There is the tide caused by the earth on the moon because the earth is the focus of the moon moving orbit, but there is not the tide caused by the moon on the earth because the moon is not the focus of the moving orbit of the seawater on the earth.

地球的潮汐力是由椭圆轨道运动产生的，由于月球的轨道运动是以地球为焦点，所以在月球上可以产生受地球影响的潮汐，而不可以产生相反的潮汐，因为海水或岩浆没有以月球为焦点的轨道运动。

A summary of three commonly used kinds of tidegenerating potential development has been made. Different from the theoretical model of the effect of solid earth tide on station displacements recommended by the IERS1996 and IERS2000, a spectrum method is developed, independent of almanac, at the submillimeter level using precise development of TGP.

测站位移的潮汐效应是通过潮汐参数Love数hnm和Shida数lnm来表征的，而且测站的潮汐位移几乎是由二阶引潮力位引起，三阶潮汐效应很小，在毫米精度上更高阶的潮汐影响完全可以忽略[1]。

Theoretical calculation shows the anomaly of reservoir tidal gravity is measured at μGal level, while the measured data shows the observation error of such tidal gravity at 10-μGal level. This indicates that the data noise may well disguise real anomalies, and therefore that the lack of measured anomaly data does not necessarily equate to the lack of oil and gas reservoir underneath. The actual observed tidal gravity anomaly can reach tens of μGal. Though it is more than three times the observation error, we can not attribute it to the reservoir-induced tidal gravity anomaly.

理论计算表明，油藏潮汐重力异常在微伽量级，而实际资料表明潮汐重力的观测误差为10 μGal量级，油藏潮汐重力异常可能会被噪声淹没，所以没有观测到潮汐重力异常不等于地下没有油气；实际观测的潮汐重力异常可达数十μGal，即使超过观测误差的3倍，也不能将它直接归因于油藏产生的潮汐重力异常。

We adopted the spectrum analysis method and the BAYTAP_G method to analyze the geoelectric potential data at the Niijima station during 1998～2000 After the quantitative analysis of the tide response of geoelectric potential changes at the above station, we obtained some main characteristics of the tide response. Besides the tidal components with various periods such as diurnal tide, semidiurnal tide, and so on, semimonthly and semiyearly variations of tide response were also detected from the geoelectric potential data at the Niijima station.

本文通过采用频谱分析和BAYTAP-G方法对位于日本伊豆群岛的新岛台跨度达三年（1998～2000年）的地电场的观测资料进行了分析研究，对该台地电场的潮汐响应进行了定量提取与分析，得到了地电场潮汐响应的一些主要特征，例如除了存在全日分潮、半日分潮等不同周期的潮汐成分外，还呈现出明显的半月、半年等不同周期的活动规律。

In determining the power spectrum of the wind, Lomb-Scargle periodogram was used.The planetary waves with periods 120 hours,60hours and 35 hours, diurnal, semidiurnal and terdiurnal tides were found at height 86.4km in the zonal wind.

首先利用Lomb-Scargle周期图方法计算了大气纬向风场的功率谱，除了行星波和潮汐外，在行星波、潮汐的频率和与频率差处有明显的谱峰，双谱分析表明这些谱峰是行星波和潮汐相互作用形成的。

We adopted the spectrum analysis method and the BAYTAP-G method to analyze the geoelectric potential data at the Niijima station during 1998~2000. After the quantitative analysis of the tide reaponse of geoelectric potential changes at the above station, we obtained some main characteristics of the tide response. Besides the tidal components with various periods such as diurnal tide, semi-diurnal tide, and so on, semimonthly and semi-yearly variations of tide response were also detected from the geoelectric potential data at the Niijima station.

本文通过采用频谱分析和BAYTAP-G方法对位于日本伊豆群岛的新岛台跨度达三年（1998~2000年）的地电场的观测资料进行了分析研究，对该台地电场的潮汐响应进行了定量提取与分析，得到了地电场潮汐响应的一些主要特征，例如除了存在全日分潮、半日分潮等不同周期的潮汐成分外，还呈现出明显的半月、半年等不同周期的活动规律。

In order to make up for the shortage of paper "Tide Table",stable curves and TotalTide which are practically applied onboard, through collecting whole data on "Tide Table", an electronic tide diagram is developed using Windows+Visual Studio 2005 as a development platform.

中文摘要：为弥补纸质"潮汐表"、静态曲线图和TotalTide等产品在船舶驾引等实际应用中的不足，通过采集"潮汐表"上的整点数据，利用Windows+Visual Studio 2005开发平台，开发出电子潮汐图表。

Through concretely analyzing the magnitude and error of deflection of the vertical, we can get the results that the long-period, smaller-range non-tidal variations are commonly less than the tidal ones, but the short-period, larger-range non-tidal variations are comparable to the tidal ones, especially in some areas they are even bigger than the tidal ones, this state can be measured by repeated gravimetry completely.

通过对垂线偏差量级和误差大小的具体分析，得出结论：一般长周期的、幅度较小的非潮汐变化要小于潮汐变化，但短周期的、幅度较大的非潮汐变化则可能与潮汐变化相当，个别地区甚至还会超过潮汐变化，这种情况完全可以用重复重力测量的方法检测到，这也说明重复测量的方法是可行的。

Using j and v tidal models and harmonic analyses to obtain the harmonic constants of main tidal components in the China seas from TOPEX/POSDEIDON data, verifing the results with the global tidal model CSR3.0 qualitatively and data from tide gauge stations quantitatively, the paper shows that the results computed here are more reasonable and are better than the results of the global tidal model for the China seas.

基于TOPEX/POSEIDON卫星高度计资料，利用j，v潮汐模型和调和分析法提取中国浅海潮汐信息，与TOPEX/POSEIDON卫星自带的全球潮汐模式CSR3.0和验潮站资料分别进行定性和定量的对比，说明在中国浅海的计算结果优于全球潮汐模式。

与潮汐相关的网络解释 [注：此内容来源于网络，仅供参考]

tidal datum plane：潮汐基准面

tidal cycle 潮汐周期 | tidal datum plane 潮汐基准面 | tidal datum 潮汐基准面

earth tide：地球潮汐 地球潮汐

■ earth surface 地球表面 地表面 | ■ earth tide 地球潮汐 地球潮汐 | ■ earth's crust 地壳 地殻

tidal harmonic analysis：潮汐调和分析

潮汐调和常数 tidal harmonic constants | 潮汐调和分析 tidal harmonic analysis | 潮汐非调和常数 tidal nonharmonic constants

tidal harmonic analysis：潮汐调合分析

tidal harbour 潮汐港潮汐港潮汐港(无闸门 | tidal harmonic analysis 潮汐调合分析 | tidal indicator 示潮器

harmonic constant of tide：潮汐调和常数

潮汐表|tide table | 潮汐调和常数|harmonic constant of tide | 潮汐调和分析|harmonic analysis of tide

tidal nonharmonic analysis：潮汐非调和分析

潮汐非调和常数 tidal nonharmonic constants | 潮汐非调和分析 tidal nonharmonic analysis | 潮汐摄动 tidal perturbation

tidal nonharmonic constants：潮汐非调和常数

潮汐调和分析 tidal harmonic analysis | 潮汐非调和常数 tidal nonharmonic constants | 潮汐非调和分析 tidal nonharmonic analysis

tidal observatory：潮汐观测站

tidal observation 潮汐观测 | tidal observatory 潮汐观测站 | tidal oscillation 潮汐振动

Tidal Power Generation：潮汐发电,潮汐能发电

tidal power 潮汐功率 | tidal power generation 潮汐发电,潮汐能发电 | tidal power station 潮汐电站

tide lock：潮汐船闸潮汐船闸

tide lock 潮汐船闸 | tide lock 潮汐船闸潮汐船闸 | tide lock 潮闸