海面径向重力梯度分量模拟的表层积分法

IF 0.9 Q4 REMOTE SENSING
D. Zhao, Z. Gong, J. Feng
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引用次数: 0

摘要

摘要为了模拟和确定近海面空间的地球外重力势及其二阶径向导数,本文讨论了表层积分法。讨论了该方法在海面上适用的原因。从原基于面层法的扰动势积分公式出发,导出了重力梯度张量径向分量的表达式。在此基础上,引入恒等关系对公式进行修正,减少了奇异性问题。在中国海域进行的数值实验表明,改进的表层积分法有效地提高了近海面扰动势二阶径向梯度分量的计算精度和可靠性。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
The surface layer integral method for the modelling of the radial gravity gradient component over sea surface
Abstract For the modelling and determination of the Earth’s external gravity potential as well as its second-order radial derivatives in the space near sea surface, the surface layer integral method was discussed in the paper. The reasons for the applicability of the method over sea surface were discussed. From the original integral formula of disturbing potential based on the surface layer method, the expression of the radial component of the gravity gradient tensor was derived. Furthermore, an identity relation was introduced to modify the formula in order to reduce the singularity problem. Numerical experiments carried out over the marine area of China show that, the modi-fied surface layer integral method effectively improves the accuracy and reliability of the calculation of the second-order radial gradient component of the disturbing potential near sea surface.
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来源期刊
Journal of Geodetic Science
Journal of Geodetic Science REMOTE SENSING-
CiteScore
1.90
自引率
7.70%
发文量
3
审稿时长
14 weeks
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