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GNSS reflectometry measurement of snow depth and soil moisture in the French Alps

机译:GNSS反射法测量法国阿尔卑斯山的积雪深度和土壤湿度

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Over the last ten years Earth observing systems have grown considerably and thus allow the use of Global Navigation Satellite System (GNSS) signals for remote sensing. Several studies in the U.S. have proven the ability of existing GNSS ground networks to measure environmental parameters quantifying essential surface conditions for the understanding of the water cycle. This is possible by taking advantage of reflected signals around geodetic stations. Improved characterization of environmental disturbances in GNSS signals is also essential to increase the accuracy of future GNSS measurement for applications in Earth Sciences. GNSS reflectometry provides these surface parameters at an intermediate scale that can bridge the lack of data between in situ and satellite observations. Here we adapt and develop for the first time the GNSS reflectometry method using the existing sites of the French national GNSS permanent network (RENAG) for snow and soil moisture applications.
机译:在过去的十年中,地球观测系统得到了长足的发展,因此可以将全球导航卫星系统(GNSS)信号用于遥感。美国的几项研究证明了现有GNSS地面网络具有测量环境参数的能力,这些参数量化了必要的地面条件,以了解水循环。这可以通过利用大地测量站周围的反射信号来实现。改进GNSS信号中环境干扰的表征对于提高未来GNSS测量在地球科学中的应用的准确性也至关重要。 GNSS反射仪以中等规模提供了这些表面参数,可以弥补现场观测和卫星观测之间缺乏数据的不足。在这里,我们首次使用法国国家GNSS永久网络(RENAG)的现有站点对雪和土壤湿度应用进行调整和开发GNSS反射法。

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