【摘要】 利用高精度卫星测高数据反演重力是获取海洋重力异常的重要方法。本文介绍了自2008年以来新一代高精度测高卫星的相关信息。在此基础上,联合多颗新型卫星,进行交叉点平差,通过中心差分代替常规Sandwell方法计算垂线偏差,利用改进的逆Vening-Meinesz法和Stokes数值反解法对西太平洋某区域进行了重力场反演。反演结果与NGDC提供的船测重力值比较表明,逆Vening-Meinesz法计算误差小于Stokes数值反解法。通过添加随机噪声数值实验,进一步证明逆Vening-Meinesz法对于测高数据误差的抗差能力更强,在研究区的重力异常计算结果可信度较高。更多还原

【Abstract】 The application of gravity anomaly inversion from high quality satellite altimeter data is an important method to acquire marine gravity.The main characteristics of newly available satellite altimeter data since 2008 are reviewed in this paper.On the basis of multi-satellite data,we apply crossover adjustment and use central difference method to calculate deflection of the vertical instead of conventional Sandwell method.After that,improved inverse Vening-Meinesz method and numerical inverse-Stokes approach are adopted to calculate the gravity filed of certain area in the West Pacific.Comparision with the shipboard-based gravity provided by NGDC shows that inverse Vening-Meinesz method has smaller errors than numerical inverse-Stokes approach.With further numerical expericment ofadding stochastic noise,we show that inverse Vening-Meinesz method is more robust so that it can provide reliable gravity estimation for the target area.更多还原