融合海域多源重力数据的正则化点质量方法

泰勒级数展开是实施位场向下延拓解算的主要方法之一。该方法的有效性主要取决于位场延拓参量各阶垂向（或径向）偏导数的求取精度及其可靠性。为了避免使用封闭解析核函数在球边界面出现奇异性带来的不确定性问题,依据各类重力观测经滤波处理后均表现为一类有限频谱带宽信号的特点,提出将地球外部重力异常泊松积分式的核函数表示为球谐级数展开式,并将其截断为与重力观测值频谱范围相一致的带限求和式,进而通过直接求导方法,推导得到一组与带限核函数相对应的重力异常高阶径向导数带限计算公式,同时对该组公式进行了实用性改化,并将其应用于重力异常向下延拓泰勒级数展开式计算。使用超高阶地球位模型EGM2008设计两个阶段的数值计算检验方案,分别对重力异常高阶径向偏导数带限模型及其泰勒级数展开向下延拓模型的计算精度进行了检核评估,表明新模型具有良好的可靠性和有效性,在解算稳定性和计算精度两个方面都优于其他同类模型。

Regularization of Point-Mass Model for Multi-Source Gravity Data Fusion Processing

Taylor series expansion is often used in the downward continuation of potential field, and its performance depends on the accuracy and reliability of vertical partial derivatives or radial partial derivatives (RPDs) of potential field parameters.In order to avoid the singularity on spherical boundary and the uncertainty to the computational results by using the closed analytic kernel function to solve the partial derivative, first, this paper considers the fact that all kinds of gravity observations behave as a type of limited spectrum bandwidth signal after being filtered, and proposes to express the kernel function of the Poisson integral for the external gravity anomaly by a spherical harmonic series expansion, which is truncated into a band-limited summation with the same spectrum range as the gravity observation. Then, we derive a set of band-limited formulas to calculate the high-order RPDs, which are modified and applied to the downward continuation of the gravity anomaly by Taylor series expansion.The formulas are validated using the ultra-high-degree geopotential model EGM2008 by a two-stage procedure. The numerical tests of the band-limited formulas and the Taylor series expansion downward continuation model show that the proposed band-limited formulas have good reliability and validity, and are superior to other models in terms of stability and accuracy.