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全球GPS测站垂向周年变化统计改正模型的建立 总被引:1,自引:1,他引:0
对GPS测站坐标进行非线性变化的研究和建模,是削弱测站非线性运动的有效途径。由于导致测站坐标非线性变化的机制具有多样性和复杂性,目前还未能建立一个包含多种机制影响的理论改正模型来削弱测站的非线性运动。本文基于全球近500个实测的GPS测站垂向坐标残差时间序列,研究发现了测站垂向坐标周年项的全球分布规律,并分别针对南北半球构建了两个基于实测数据的周年变化统计改正模型。试验表明,本文提出的统计改正模型能削弱全球大部分GPS测站30%~50%的垂向坐标残差。 相似文献
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利用小波工具剔除噪声的思想对全球部分GPS测站坐标残差序列进行应用试验。通过选取特定的阈值和小波基函数,成功提取出GPS测站坐标残差序列的一些非线性周期规律,对于进一步深入研究GPS测站坐标非线性变化规律有重要意义。 相似文献
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GPS站坐标时间序列中存在的周期性与非周期性误差严重影响了对测站运动特征的分析及其非线性变化的物理机制解释。因此,为削弱噪声的影响,本文首先利用区域叠加滤波法去除了南加利福尼亚地区16个测站时间序列的共模误差,以此削弱时间序列中存在的包括周年和半周年误差在内的周期性误差。为去除滤波后残留的噪声,对滤波后的信号进行静态离散小波变换,提取了周期为半周年以上的信号。结果表明,联合区域叠加滤波法与小波变换对GPS站坐标时间序列进行处理,既能够削弱周期性误差对信号的影响,又能较好地提取测站的非线性运动信号。 相似文献
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利用2009-05~2010-12共20mon的GRACE时变重力场反演了山西省境内陆地水储量变化造成的地表垂直位移,并与同期的GPS高程残差进行了比较。结果显示,对大部分CORS站而言,GRACE反演的水文地壳垂向形变与GPS高程残差时间序变化量均在-6~6mm之间;由二者提取的年周期信号平均振幅均为2.5mm左右,但是相位存在较大差异。由于GPS数据处理过程未考虑周日、半周日大气潮汐,高阶电离层,及非潮汐海潮的影响,这三项误差会传播到测站坐标的时间序列,对GPS周年信号产生影响,所以可以认为GRACE与GPS结果的差异更多的是来自GPS数据处理的误差。 相似文献
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通过设立分组实验,利用GAMIT软件重新处理了全球75个并置站2003~2008年的GPS数据,初步得出了GPS周年性系统误差随纬度的分布规律,量化了天线相位中心偏差对GPS周年性系统误差的贡献,并分析了天线相位中心偏差对测站N、E、U方向时间序列中非线性变化的影响。研究结果表明,GPS周年性系统误差随着纬度减小而呈现增大的趋势;天线相位中心偏差对测站N、E、U方向周年性系统误差的贡献为20%、27%、23%;天线相位中心偏差改正能够显著削弱N、E、U方向纬度介于40°~50°、45°~60°、0°~30°测站的GPS周年性系统误差;天线相位中心偏差可能是造成全球GPS测站N、E、U方向周年、U方向半周年、与中低纬度GPS测站N方向半周年运动的原因之一。 相似文献
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Anomalous harmonics in the spectra of GPS position estimates 总被引:22,自引:3,他引:19
Prior studies of the power spectra of GPS position time series have found pervasive seasonal signals against a power-law background
of flicker noise plus white noise. Dong et al. (2002) estimated that less than half the observed GPS seasonal power can be explained by redistributions of geophysical fluid mass
loads. Much of the residual variation is probably caused by unidentified GPS technique errors and analysis artifacts. Among
possible mechanisms, Penna and Stewart (2003) have shown how unmodeled analysis errors at tidal frequencies (near 12- and 24-hour periods) can be aliased to longer periods
very efficiently. Signals near fortnightly, semiannual, and annual periods are expected to be most seriously affected. We
have examined spectra for the 167 sites of the International GNSS (Global Navigation Satellite Systems) Service (IGS) network
having more than 200 weekly measurements during 1996.0–2006.0. The non-linear residuals of the weekly IGS solutions that were
included in ITRF2005, the latest version of the International Terrestrial Reference Frame (ITRF), have been used. To improve
the detection of common-mode signals, the normalized spectra of all sites have been stacked, then boxcar smoothed for each
local north (N), east (E), and height (H) component. The stacked, smoothed spectra are very similar for all three components.
Peaks are evident at harmonics of about 1 cycle per year (cpy) up to at least 6 cpy, but the peaks are not all at strictly
1.0 cpy intervals. Based on the 6th harmonic of the N spectrum, which is among the sharpest and largest, and assuming a linear
overtone model, then a common fundamental of 1.040 ± 0.008 cpy can explain all peaks well, together with the expected annual
and semiannual signals. A flicker noise power-law continuum describes the background spectrum down to periods of a few months,
after which the residuals become whiter. Similar sub-seasonal tones are not apparent in the residuals of available satellite
laser ranging (SLR) and very long baseline interferometry (VLBI) sites, which are both an order of magnitude less numerous
and dominated by white noise. There is weak evidence for a few isolated peaks near 1 cpy harmonics in the spectra of geophysical
loadings, but these are much noisier than for GPS positions. Alternative explanations related to the GPS technique are suggested
by the close coincidence of the period of the 1.040 cpy frequency, about 351.2 days, to the “GPS year”; i.e., the interval
required for the constellation to repeat its inertial orientation with respect to the sun. This could indicate that the harmonics
are a type of systematic error related to the satellite orbits. Mechanisms could involve orbit modeling defects or aliasing
of site-dependent positioning biases modulated by the varying satellite geometry. 相似文献
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This article describes a methodology to monitor dynamic vertical sub-centimeter displacement, of a GPS antenna. The dynamic
movement of an antenna is determined by choosing the appropriate reference satellite for measurement differencing and by applying
a FFT filter on the double-difference phase residuals. The validity of the method depends on the time variations of the GPS
residuals and errors, such as, receiver noise, atmospheric contribution, multipath effects, and the antenna movement. This
research is under development and results for simulated motion are presented here. ? 2002 Wiley Periodicals, Inc. 相似文献
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矿区GPS变形监测与变形分析 总被引:3,自引:3,他引:3
对矿区DPS变形监测网的建立、实时监测、基线平差、变形分析及分形特征等问题,进行了较系统深入的探讨。经对GPS实时监测变表数据分析可知,地表点的移动具有较强的分形增长规律,GPS变形监测技术能够揭示地表移动的非线性特征,为变形分析与预测提供了新的途径。 相似文献
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对于GPS精密单点定位,天线相位转绕误差无法通过星间求差法消除或者减弱,因此必须通过适当的模型加以改正。本文详细分析该误差的特性及其改正方法,并采用自编软件通过计算实例分析其对GPS精密单点定位的精度影响。 相似文献
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详细阐述了利用GLAS数据和GPS数据生成Dome-A地区DEM的方法。首先进行GLAS数据转化, 便于与GPS数据结合, 提出一种快速搜索GLAS和其光斑(Footprint)覆盖GPS点的算法, 比较GLAS数据和GPS数据发现, 均值差异最大为1.118 m, 最小为0.997 m, 而标准差稳定为5-6 cm, 在进行椭球变换修正之后, 差值最大为0.405 m, 最小为0.284 m;之后利用改进的角度限差法沿测线对GPS数据进行特征点提取, 得到抽稀之后的数据;再利用抽稀之后的GPS数据和处理后的GLAS数据使用克里金插值方法生成研究区DEM。利用1199个GPS点和53个GLAS检验点对最后生成的DEM进行了精度分析, 残差中误差为5 cm, 最大残差绝对值为12 cm。利用原始GPS数据, 原始GPS数据和GLAS数据, 处理后GPS数据利用克立金插值方法分别生成了研究区的DEM, 通过等高线提取分析以及检验点的误差分析, 处理后的GPS数据生成的DEM要优于原始GPS数据的, 证明GPS处理的必要性。 相似文献
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基于经验模态分解的GPS基线解算模型 总被引:1,自引:1,他引:0
非建模系统误差是影响高精度GPS基线解算精度的一个重要因素,文章给出基于经验模态分解的GPS基线解算模型,有效消弱系统误差对基线解的影响。在现有经验模态分解理论的基础上,定义经验模态分解的多尺度分解与重构结构,并由此给出基于经验模态的系统趋势分离模型,依据累积标准化模量的均值随尺度的变化确定系统误差与噪声分离尺度的选择标准。给出基于经验模态分解的GPS基线解算的技术路线,首先计算GPS相位双差观测方程的浮点解残差序列,分离出系统误差并用于修正GPS双差观测值,重新计算双差浮点解,采用Lambda算法固定整周模糊度,计算固定基线解,从而消弱系统误差对基线解算的影响,提高基线固定解的可靠性。并采用实测GPS数据验证模型,F-ratio指数与W-ratio指数表明系统误差消弱后,基线固定解可靠性得到明显提高,重新计算的残差序列表明系统误差得到很好的消弱。 相似文献
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本文根据弹性位错理论和顾及先验信息的断层运动参数反演方法,通过数值试验研究了断层区域的GPS监测点布设方案及其对断层运动参数反演结果的影响,检验了不同形式的GPS网对于探测断层活动的效果,讨论了GPS观测的点位随机误差和粗差对探测断层活动的影响。 相似文献
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Multipath error is considered one of the major errors affecting GPS observations. One can benefit from the repetition of satellite
geometry approximately every sidereal day, and apply filtering to help minimize this error. For GPS data at 1 s interval processed
using a double-difference strategy, using the day-to-day coordinate or carrier-phase residual autocorrelation determined with
a 10-h window leads to the steadiest estimates of the error-repeat lag, although a window as short as 2 h can produce an acceptable
value with > 97% of the optimal lag’s correlation. We conclude that although the lag may vary with time, such variation is
marginal and there is little advantage in using a satellite-specific or other time-varying lag in double-difference processing.
We filter the GPS data either by stacking a number of days of processed coordinate residuals using the optimum “sidereal”
lag (23 h 55 m 54 s), and removing these stacked residuals from the day in question (coordinate space), or by a similar method
using double-difference carrier-phase residuals (observational space). Either method results in more consistent and homogeneous
set of coordinates throughout the dataset compared with unfiltered processing. Coordinate stacking reduces geometry-related
repeating errors (mainly multipath) better than carrier-phase residual stacking, although the latter takes less processing
time to achieve final filtered coordinates. Thus, the optimal stacking method will depend on whether coordinate precision
or computational time is the over-riding criterion. 相似文献
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