GPS监测地壳形变漂移速度的计算
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摘要
根据动态卡尔曼滤波理论,结合GPS监测地壳形变数据处理的特点,构建了动态卡尔曼滤波计算地壳运动漂移速度的数学模型.结合IGS的GPS连续观测网络部分站点的多期数据,使用精密定位定轨软件GAMIT进行定位计算,获得高精度的站点坐标.将坐标作为具有先验方差信息的准观测值,设置站点漂移速度为未知数,进行卡尔曼滤波漂移速度的估计.计算结果与已有结果的比较表明,卡尔曼滤波漂移速度估计可以达到mm级的精度,可用于GPS监测地壳形变进行漂移速度的估计.
Based on the dynamic Kalman Filter theory and the characteristics of data processing of GPS crustal deformation monitoring,a calculation model of floating velocity with a dynamic Kalman Filter was established.At first,the highly precise coordinates were calculated using many periods of data from some IGS stations and GAMIT software.Then,the obtained coordinates were considered as quasi-observations,and the velocities were considered as unknown variations and were computed with a Kalman Filter.A comparison of calculated and measured data shows that the presented model has a precision of several millimeters.So the model can be used for floating velocity estimation in GPS crustal deformation monitoring.
引文
[1]顾国华,申旭辉,王敏,等.中国大陆现今地壳水平运动基本特征[J].地震学报,2001,23(4):362-369.
    [2]牛之俊,游新兆.中国地壳运动速度场——GAMIT和GISPY解算结果对比[J].大地测量学与地球动力学,2003,23(3):4-8.
    [3]王解先.GPS精密定轨定位[M].上海:同济大学出版社,1998.
    [4]兰孝奇.GPS精密变形监测数据处理方法及其应用研究[D].南京:河海大学,2005.
    [5]崔希璋,於宗木寿,陶本藻,等.广义测量平差[M].武汉:武汉测绘科技大学出版社,2000.
    [6]刘大杰,陶本藻.实用测量数据处理方法[M].北京:测绘出版社,2000.
    [7]Department of Earth,Atmospheric,and Planetary Sciences.Documentation for the GAMIT GPS analysis software[R].Cambridge:Massachusetts Institute of Technology,1999.
    [8]孟国杰,赵承坤,顾国华,等.中国地壳运动观测网络首期观测数据处理[J].地震,2001,21(1):63-68.
    [9]葛恒年.GPS地壳形变监测数据处理及大气水汽含量反演计算的研究[D].南京:河海大学,2006.
    [10]陆彩平,王解先.GPS监测地壳数据处理[J].大地测量学与地球动力学,2002,22(4):56-60.

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