Zhou Wei, Liu Lilong, Huang Liangke, Yao Yibin, Chen Jun, Li Songqing
College of Geomatic Engineering and Geoinformatics, Guilin University of Technology, Guilin, 541004, China.
Guangxi Key Laboratory of Spatial Information and Geomatics, Guilin, 541004, China.
Sci Rep. 2019 Mar 7;9(1):3814. doi: 10.1038/s41598-019-40456-2.
Snow is not only a critical storage component in the hydrologic cycle but also an important data for climate research; however, snowfall observations are only sparsely available. Signal-to-noise ratio (SNR) has recently been applied for sensing snow depths. Most studies only consider either global positioning system (GPS) L1 or L2 SNR data. In the current study, a new snow depth estimation approach is proposed using multipath reflectometry and SNR combination of GPS triple frequency (i.e. L1, L2 and L5) signals. The SNR combination method describes the relationship between antenna height variation and spectral peak frequency. Snow depths are retrieved from the SNR combination data at YEL2 and KIRU sites and validated by comparing it with in situ observations. The elevation angle ranges from 5° to 25°. The correlations for the two sites are 0.99 and 0.97. The performance of the new approach is assessed by comparing it with existing models. The proposed approach presents a high correlation of 0.95 and an accuracy (in terms of Root Mean Square Error) improvement of over 30%. Findings indicate that the new approach could potentially be applied to monitor snow depths and may serve as a reference for building multi-system and multi-frequency global navigation satellite system reflectometry models.
雪不仅是水文循环中的关键存储成分,也是气候研究的重要数据;然而,降雪观测数据却十分稀少。信噪比(SNR)最近已被用于探测雪深。大多数研究仅考虑全球定位系统(GPS)的L1或L2信噪比数据。在本研究中,提出了一种利用多径反射测量法和GPS三频(即L1、L2和L5)信号的信噪比组合来估算雪深的新方法。信噪比组合方法描述了天线高度变化与频谱峰值频率之间的关系。从YEL2和KIRU站点的信噪比组合数据中反演雪深,并通过与实地观测数据进行比较来验证。仰角范围为5°至25°。两个站点的相关性分别为0.99和0.97。通过与现有模型进行比较来评估新方法的性能。所提出的方法呈现出0.95的高相关性,并且精度(以均方根误差计)提高了30%以上。研究结果表明,新方法有可能应用于雪深监测,并可为构建多系统和多频全球导航卫星系统反射测量模型提供参考。