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Study on the stable and high-precision downward extension method of airborne gravity anomaly data
The essence of the downward continuation of airborne gravity anomalies is to solve the first kind of Fredholm integral equation, which is an ill-posed problem. Stable and high-precision downward continuation methods have always been a research hotspot in
Baogui Ke +4 more
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Obtaining horizontal edges and the buried depths of geological bodies, using potential field tensor data directly is an outstanding question. The largest eigenvalue of the structure tensor is one of the commonly used edge detectors for delineating the ...
Yuan Yuan +4 more
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Downward Continuation of Airborne Gravimetry Data by Means of Spherical Radial Basis Functions
The problem of downward continuation of airborne gravimetry data is discussed. Use of spherical radial basis functions (SRBF) to solve this ill-posed problem is proposed. Gravity disturbances observed at flight high are continued downward to disturbing
Sugaipova Leyla, Neyman Yury
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One of the main applications of the gravity field and steady-state Ocean Circulation Explorer (GOCE) satellite data is their combination with local gravity anomalies for geoid and gravity field modeling purposes.
Dimitrios A. Natsiopoulos +4 more
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Downward Continuation Method for Potential Field Data Based on Physics-Informed Neural Network
Downward continuation can enhance weak anomaly signals and enable the conversion of data from different altitudes, making it a crucial technique in potential field data processing.
Yongkang Chan +5 more
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Upward and downward continuation as inverse problems [PDF]
Summary. The formalism of Backus & Gilbert is applied to the problems of upward and downward continuation of harmonic functions. We first treat downward continuation of a two-dimensional field to a level surface everywhere below the observation locations; the calculation of resolving widths and solution estimates is a straightforward application of ...
Huestis, Stephen P., Parker, Robert L.
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The downward continuation (DWC) method was used to determine the density contrast between the seawater and the ocean bottom topographic mass to estimate accurate bathymetry using the gravity-geologic method (GGM) in two study areas, which are located ...
Yu-Shen Hsiao +4 more
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The gravity gradiometric data are affected by the topographic and atmospheric masses. In order to fulfill Laplace-Poisson’s equation and to simplify the downward continuation process, these effects should be removed from the data. However, if
Mehdi ESHAGH
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Topography is a problem in geoid determination by the Stokes formula, a high degree Earth Gravitational Model (EGM), or for a combination thereof. Herein, we consider this problem in analytical/harmonic downward continuation of the external potential at ...
Sjöberg Lars E.
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A U-Net network-based downward continuation method for airborne gravity
Downward continuation of gravity data is a critical challenge in the practical applications of airborne gravity, such as global geopotential modeling and geophysical interpretation.
Zifan Ding +3 more
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