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Snow Depth Estimation Based on Multipath Phase Combination of GPS Triple-Frequency Signals

机译:GPS三频信号多径相位组合的雪深估计

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摘要

Snow is important to the ecological and climate systems; however, current snowfall and snow depth observations are only available sparsely on the globe. By making use of the networks of Global Positioning System (GPS) stations established for geodetic applications, it is possible to monitor snow distribution on a global scale in an inexpensive way. In this paper, we propose a new snow depth estimation approach using a geodetic GPS station, multipath reflectometry and a linear combination of phase measurements of GPS triple-frequency (L1, L2, and L5) signals. This phase combination is geometry free and is not affected by ionospheric delays. Analytical linear models are first established to describe the relationship between antenna height and spectral peak frequency of combined phase time series, which are calculated based on theoretical formulas. When estimating snow depth in real time, the spectral peak frequency of the phase measurements is obtained, and then the model is used to determine snow depth. Two experimental data sets recorded in two different environments were used to test the proposed method. The results demonstrate that the proposed method shows an improvement with respect to existing methods on average.
机译:雪对生态和气候系统很重要;然而,目前只有全球稀少的降雪和积雪深度观测资料。通过利用为大地测量应用而建立的全球定位系统(GPS)站的网络,可以以廉价的方式在全球范围内监视积雪。在本文中,我们提出了一种使用大地测量GPS站,多径反射法和GPS三频(L1,L2和L5)信号的相位测量值的线性组合的新雪深估算方法。此相位组合没有几何形状,不受电离层延迟的影响。首先建立解析线性模型,以描述天线高度与组合相位时间序列的频谱峰值频率之间的关系,并根据理论公式进行计算。在实时估算积雪深度时,获得相位测量值的频谱峰值频率,然后使用该模型确定积雪深度。在两个不同的环境中记录的两个实验数据集用于测试该方法。结果表明,所提出的方法相对于现有方法平均而言显示出改进。

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