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Impact of uncertainties of GOCE gravity model on crustal thickness estimates

机译:岩石重力模型对地壳厚度估计的影响的影响

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摘要

In the last few years many studies have applied data of satellite gravity sensors for solid Earth applications. The use of different methodologies has been shown to result in large variations in crustal thickness even when using the same data as source. It is, however, difficult to estimate what is a significant difference between such models. Up to now the impact of the inherent uncertainty of Gravity Field and steady-state Ocean Circulation Explorer (GOCE) data on solid Earth applications has never been quantified. With this study we will provide uncertainty boundaries for crustal modelling based on the GOCE TIM5 covariance matrix. Different noise realizations have been calculated using a Monte Carlo-like simulation and added to the TIM5 model coefficients. The resulting differences in crustal thickness amount to maximum +/- 0.2 km, which is less than 1 per cent of the total thickness, and much smaller than many other uncertainties involved in the inversion process.
机译:在过去的几年中,许多研究已经应用了固体地球应用的卫星重力传感器的数据。 已经显示使用不同方法的使用,即使在使用与源相同的数据时,即使在使用与源相同的数据也会导致地壳厚度的大变化。 然而,难以估计这些模型之间存在显着差异。 到目前为止,重力场和稳态海洋循环资源管理器(Goce)数据对固体地球应用的影响从未被过量化。 通过本研究,我们将为基于Goce Tim5协方差矩阵提供地壳建模的不确定性边界。 使用Monte Carlo样模拟计算了不同的噪声实现,并添加到TIM5模型系数。 产生的地壳厚度的差异为最大+/- 0.2公里,比总厚度的1%小于逆转过程中涉及的许多其他不确定性。

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