Abstract
Downward continuation is an effective technique that can be used to transform the magnetic data measured on one surface to the data that would be measured on another arbitrary lower surface. However, it suffers from amplitude attenuation and is susceptible to noise, especially when the continuation distance is large. To solve these problems, we present a stable and high-precision downward continuation method combining the ideas of equivalent source technique, Tikhonov regularization, radial logarithmic power spectrum analysis, and constrained strategy. To implement this method, the observed data is used to construct the equivalent source in the study area, and the small amount of measured magnetic data at the lower surface (relative to the original observation surface) is employed to constrain the calculation procedure simultaneously. Then the magnetic data at the target surface can be obtained by using a forward calculation procedure instead of the risky downward continuation procedure. The proposed method is tested on both synthetic model data and real magnetic data collected in the South China sea. Various obtained results demonstrate that the method reported in this study has higher accuracy and better noise resistance than the traditional downward continuation methods.
Highlights
A Stable and High-Precision Downward Continuation Method of Magnetic DataCitation: Zhou, Z.; Wang, J.; Meng, X.; Fang, Y. A Stable and High-Precision Downward Continuation Method of Magnetic Data. Appl. Sci. 2021, 11, 10881. https://doi.org/10.3390/ app112210881 Received: 28 September 2021 Accepted: 9 November 2021 Published: 18 November 2021 Publisher’s Note: MDPI stays neutral with regard to jurisdictional claims in published maps and institutional affiliations
Downward continuation of magnetic data can be used to obtain the magnetic data measured on one surface to the data that would be measured on another arbitrary lower surface, with which the high frequency information induced by the causative sources can be enhanced
The quantitativseoucrocme mpeatrhiosdonimopfroevaecshthmeeatchcuordacrye. sulted in differences with the theoretical magnetic data, as Table 2 shows, which demonstrated that the constraint equivalent source method imprToabvlees2.tThhee daicffceurernacecbye.tween the results of the downward continuation methods and the theoretical magnetic data
Summary
Citation: Zhou, Z.; Wang, J.; Meng, X.; Fang, Y. A Stable and High-Precision Downward Continuation Method of Magnetic Data. Appl. Sci. 2021, 11, 10881. https://doi.org/10.3390/ app112210881 Received: 28 September 2021 Accepted: 9 November 2021 Published: 18 November 2021 Publisher’s Note: MDPI stays neutral with regard to jurisdictional claims in published maps and institutional affiliations.
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