李瑞浩, 陈冬生, 傅兆珠, 魏望生, 翦大西. 1984: 中国固体潮向量空间分布特征的研究. 地震学报, 6(2): 223-240.
引用本文: 李瑞浩, 陈冬生, 傅兆珠, 魏望生, 翦大西. 1984: 中国固体潮向量空间分布特征的研究. 地震学报, 6(2): 223-240.
LI RUIHAO, CHEN DONGSHENG, FU ZHAOZHU, WEI WANGSHENG, JIAN DAXIac. 1984: INVESTIGATION ON THE SPACE DISTRIBUTION CHARACTERISTIC OF TIDAL GRAVITY VECTOR IN CHINA. Acta Seismologica Sinica, 6(2): 223-240.
Citation: LI RUIHAO, CHEN DONGSHENG, FU ZHAOZHU, WEI WANGSHENG, JIAN DAXIac. 1984: INVESTIGATION ON THE SPACE DISTRIBUTION CHARACTERISTIC OF TIDAL GRAVITY VECTOR IN CHINA. Acta Seismologica Sinica, 6(2): 223-240.

中国固体潮向量空间分布特征的研究

INVESTIGATION ON THE SPACE DISTRIBUTION CHARACTERISTIC OF TIDAL GRAVITY VECTOR IN CHINA

  • 摘要: 本文对中比合作和我们独立获得的共10个台站17个仪器架次2890天的固体潮观测资料采用卡特莱特(Cartwright)的完全展开和维尼迪可夫(Venedikov)方法统一地进行了调和分析,并用中井(Nakai)方法对观测资料进行了拟合预处理以提高分析结果的信噪比,同时用线性内插方法处理了仪器灵敏度以资对比.本文着重讨论了分析结果所提供的我国大陆固体潮矢量空间分布的区域性特征及其与海洋负荷的关系.结果表明:中国大陆固体潮空间分布受到海洋负荷的明显控制.O1波尤为显着.文中讨论了仪器流变模型对观测矢量的影响.根据流变模型改正后的结果,所得到的地球对引潮力的实际响应的相位滞后,大多数发站都接近于-1,它论证了理论原则的正确性.文中还讨论了残差矢量与海洋负荷矢量的关系,它们的一致性最概括地说明了海洋负荷对固体潮的影响.文中用误差矢量的方法研究了分析结果的精度,它说明目前海潮改正的精度仍然是不够的.在上述工作基础上,文中最后得到了经海潮改正后的 M2波和 O1波的观测矢量.

     

    Abstract: In this paper the authors analyse the earth tide observation data during 2890 days at 10 stations, using Cartwright's development and Venedikob's harmonic analysis method. Nakai's fitting system is also used here for increasing the signal to noise ratio of the results of analysis. At the same time, for comparison, linear interpolation method has been employed in treating the sensitivity data of the gravimeters. The study will be centered on the space distribution characteristics of tidal gravity vector in China, and its relationship to oceanic loading. Analysis indicates that the space distributions of tidal gravity vector are obviously controlled by oceanic loading especially by the wave O1.The rheological effect of the instruments and the results of analysis in considering these effect are discussed, the phase lags amount mostly to about -1, agreeing with theory. In addition, authors examine also the relations between the residual vector and the oceanic loading vector, their conformity indicates their mutual effect. By means of the method of error vector, the accuracy of the results of analysis was examined to be not enough. Finally, based on such studies, the observed waves M2, and 1 after correction have been obtained.

     

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