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Investigation of temporal gravity variations in SG-records

机译:研究SG记录中的时间重力变化

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Not all of the gravity signals commonly observed in records of superconducting gravimeters have a physically significant meaning. Instrumental noise or signal components generated by specific processing techniques can have a strong effect. This paper analyzes selected case studies from gravity data acquired during the first period of GGP and tries to give an answer to the question of which signals are significant. It is focused on small amplitude variations in the time domain, which are compared with those of conventional spring-type gravimeters. Coherent atmospheric gravity signals due to atmospheric processes associated with strong vertical convection could be observed by different sensors. The second part deals with temporal variations of main tidal parameters, which can be seen clearly in the tidal analysis results from SG data. Synthetic case studies show that they are not strongly influenced by the analysis procedure and therefore mainly reflect ocean loading processes.
机译:并非在超导重力仪的记录中通常观察到的所有重力信号都具有物理意义。由特定处理技术产生的仪器噪声或信号成分可能会产生很大的影响。本文分析了从GGP第一阶段获得的重力数据中选择的案例研究,并试图回答哪些信号很重要的问题。它着重于时域中的小幅度变化,这与传统的弹簧型重力仪相比。可以通过不同的传感器观察到由于与强垂直对流有关的大气过程而产生的连贯的大气重力信号。第二部分处理主要潮汐参数的时间变化,这在SG数据的潮汐分析结果中可以清楚地看出。综合案例研究表明,它们不受分析程序的强烈影响,因此主要反映了海洋装载过程。

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