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Study on tidal gravity observations obtained at stations Zhongshan and Changcheng, Antarctic

机译:南极中山站和长城站的潮汐重力观测研究

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摘要

Based on the international tidal gravity reference values at station Wuhan, the tidal gravity parameters, including the amplitude factors and phase differences are determined accurately by using the observations with three La-Coste-Romberg (LCR) gravimeters (G-589, ET-20 and ET-21) at stations Zhongshan and Changcheng in the Ant-arctic, respectively. The standard deviations of the determined amplitude factors of the main tidal waves are better than 0.5%. The amplitude of each tidal wave observed at station Zhongshan is much less than that of the same wave at station Changcheng. The differences of amplitude factors in the diurnal band (O1) at these two stations are less than 7% while those in the semi-diurnal band (M2) are larger than 40%. The influences of meteorology factors, such as atmospheric pressure and temperature, on the tidal gravity observations are very obvious. The oceanic loading effects on the tidal gravity are also very prominent. It is found that the amplitude of the final residual vec-tor of every tidal wave reduces significantly after oceanic correction based on the Schwiderski's global co-tides. However, because the local oceanic loading is not taken into account, the discrepancies of amplitude factors of wave O1 observed at Zhongshan from the corresponding values of theoretical tidal model are about 4%, and 9% at Changcheng.
机译:根据武汉站的国际潮汐重力参考值,使用三台La-Coste-Romberg(LCR)重力仪(G-589,ET-20)的观测值,准确确定包括振幅因子和相位差的潮汐重力参数。和ET-21)分别位于南极的中山站和长城站。确定的主要潮汐振幅因子的标准偏差优于0.5%。在中山站观测到的每个潮汐的振幅都比在长城站观测到的同一波的振幅小得多。在这两个站的日波段(O1)中振幅因子的差异小于7%,而在半日波段(M2)中,振幅因子的差异大于40%。大气压力和温度等气象因素对潮汐重力观测的影响非常明显。海洋负荷对潮汐重力的影响也非常突出。我们发现,在根据施维德斯基的整体潮汐进行海洋校正之后,每个潮汐的最终残留矢量的振幅都会显着降低。但是,由于未考虑当地的海洋负荷,因此在中山观测到的O1波的振幅因子与理论潮汐模型的相应值的差异约为4%,而在长城约为9%。

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  • 来源
    《地震学报(英文版)》 |2001年第3期|325-332|共8页
  • 作者

  • 作者单位

    Laboratory of Dynamic Geodesy, Institute of Geodesy and Geophysics, Chinese Academy of Sciences,;

    Laboratory of Dynamic Geodesy, Institute of Geodesy and Geophysics, Chinese Academy of Sciences,;

    Laboratory of Dynamic Geodesy, Institute of Geodesy and Geophysics, Chinese Academy of Sciences,;

    Laboratory of Dynamic Geodesy, Institute of Geodesy and Geophysics, Chinese Academy of Sciences,;

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  • 正文语种 chi
  • 中图分类 P223.9;
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  • 入库时间 2022-08-19 03:55:27
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