Study of Long-term Gravity Variations, Based on Data of the GGP Co-operation

Q4 Earth and Planetary Sciences
M. Harnisch, G. Harnisch
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引用次数: 17

Abstract

Abstract The study continues a paper with the same title, presented at the Earth Tides Symposium 2000 in Mizusawa. Now data series from 12 GGP stations could be included (BE, BO, CA, CB, MB, MC, MO, PO, ST, SU, VI, WE). The length of the data series varies between 4 and 18 years. From some stations hydrological data were available. In most cases, the drift of the gravimeters was low and nearly linear. No absolute gravity measurements were available to support the estimation of the instrumental drift. Again the annual wave and the Chandler wobble were separated by fitting two sinusoidal functions with periods of 365.25 and 432 days to the residual gravity. As to be expected, the results for the individual stations move closer together and become more reliable. The δ-values of the Chandler wobble approach to 1.16. The correspondent values of the annual wobble are slightly smaller but demonstrate considerable variability. The phase lags of both phenomena are in the order of a few degrees.
基于GGP合作数据的重力长期变化研究
该研究延续了2000年在水泽举行的地球潮汐研讨会上发表的同名论文。现在可以包括12个GGP站点的数据序列(be、BO、CA、CB、MB、MC、MO、PO、ST、SU、VI、WE)。数据序列的长度在4年至18年之间。从一些站点获得了水文数据。在大多数情况下,重力仪的漂移很小,几乎是线性的。没有绝对重力测量数据可用于支持仪器漂移的估计。通过对剩余重力拟合两个周期分别为365.25天和432天的正弦函数,再次将年波和钱德勒摆动分开。正如预期的那样,各个监测站的结果更加接近,变得更加可靠。钱德勒摆动的δ值接近1.16。相应的年摆动值略小,但表现出相当大的变异性。这两种现象的相位滞后都在几度左右。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
Journal of the Geodetic Society of Japan
Journal of the Geodetic Society of Japan Earth and Planetary Sciences-Earth and Planetary Sciences (all)
CiteScore
0.20
自引率
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