基于人工神经网络的球谐系数数据挖掘

Muhammad Athar Javaid, W. Keller
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引用次数: 1

摘要

利用空间技术进行重力场回收在过去二十年中不断发展。为了获得更准确和最新的重力场信息,已经向太空发射了几个专用卫星任务,包括分别于2000年7月15日、2002年3月17日和2009年3月17日发射的挑战小卫星有效载荷(CHAMP)、重力恢复和气候实验(GRACE)和重力场和海洋环流探测器(GOCE)。GRACE是CHAMP的扩展版。CHAMP是高-低卫星对卫星跟踪(HL-SST)的一个例子,而GRACE是低-低卫星对卫星跟踪(LL-SST)系统的一个例子。我们利用GRACE串联卫星系统的距离速率观测资料,以SH系数的形式研究了重力场。系数集及其标准差,由GFZ-Germany恢复到度和阶为90,可通过podaac数据服务器获得。在一个月的时间里,地球上少数地区的重力场会发生变化。我们通过几个SH系数的数值变化来观察它。本文利用人工神经网络(ANN),根据SH系数的信息内容,将其分为两类,一类是表示变化重力场的基本系数类,另一类是不包含变化重力场信息的静态系数类。最后,我们表明,在恢复过程中,我们可以只关注基本系数,而不是处理整个系数集。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Data mining of spherical harmonic (SH) coefficients using artificial neural networks (ANN)
Gravity field recovery using space technology has evolved in the last two decades. Several dedicated satellite missions have been sent to the space to get more accurate and up-to-date gravity field information, including, Challenging Minisatellite Payload (CHAMP), Gravity Recovery and Climate Experiment (GRACE) and Gravity field and Ocean Circulation Explorer (GOCE), launched on 15 July 2000, 17 March 2002 and 17 March 2009, respectively. GRACE is the extended version of the CHAMP. CHAMP is an example of high-low satellite-to-satellite tracking (HL-SST) while the GRACE is an example of low-low satellite-to-satellite tracking (LL-SST) system. We study the gravity field in the form of SH coefficients using the range-rates observations from GRACE tandem satellites system. Sets of coefficients along with their standard deviation, recovered by GFZ-Germany up to degree and order 90 are available through the podaac data servers. In one month period, gravity field varies in few regions of the Earth. We observe it through the varying numerical values of few SH coefficients. In this contribution, we classify SH coefficients on the base of their information contents using artificial neural network (ANN) into two classes, one of them is the essential coefficient class which represents the varying gravity field and the other is the static coefficient class which does not have the varying gravity information. In the end we show that we can concentrate only on essential coefficients during the recovery process, rather than processing the whole set of coefficients.
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