Marchan-Hernandez Juan Fernando, Camps Adriano, Rodriguez-Alvarez Nereida, Bosch-Lluis Xavier, Ramos-Perez Isaac, Valencia Enric
Remote Sensing Lab, Dept. Teoria del Senyal i Comunicacions, Campus Nord D3, Universitat Politecnica de Catalunya, 08034 Barcelona, Spain.
Sensors (Basel). 2008 May 6;8(5):3005-3019. doi: 10.3390/s8053005.
Signals from Global Navigation Satellite Systems (GNSS) were originally conceived for position and speed determination, but they can be used as signals of opportunity as well. The reflection process over a given surface modifies the properties of the scattered signal, and therefore, by processing the reflected signal, relevant geophysical data regarding the surface under study (land, sea, ice…) can be retrieved. In essence, a GNSS-R receiver is a multi-channel GNSS receiver that computes the received power from a given satellite at a number of different delay and Doppler bins of the incoming signal. The first approaches to build such a receiver consisted of sampling and storing the scattered signal for later post-processing. However, a real-time approach to the problem is desirable to obtain immediately useful geophysical variables and reduce the amount of data. The use of FPGA technology makes this possible, while at the same time the system can be easily reconfigured. The signal tracking and processing constraints made necessary to fully design several new blocks. The uniqueness of the implemented system described in this work is the capability to compute in real-time Delay-Doppler maps (DDMs) either for four simultaneous satellites or just one, but with a larger number of bins. The first tests have been conducted from a cliff over the sea and demonstrate the successful performance of the instrument to compute DDMs in real-time from the measured reflected GNSS/R signals. The processing of these measurements shall yield quantitative relationships between the sea state (mainly driven by the surface wind and the swell) and the overall DDM shape. The ultimate goal is to use the DDM shape to correct the sea state influence on the L-band brightness temperature to improve the retrieval of the sea surface salinity (SSS).
全球导航卫星系统(GNSS)的信号最初是为确定位置和速度而设计的,但它们也可以用作机会信号。给定表面上的反射过程会改变散射信号的特性,因此,通过处理反射信号,可以获取有关被研究表面(陆地、海洋、冰……)的相关地球物理数据。本质上,一个GNSS-R接收器是一个多通道GNSS接收器,它在输入信号的多个不同延迟和多普勒频段上计算来自给定卫星的接收功率。构建这种接收器的最初方法包括对散射信号进行采样和存储,以便稍后进行后处理。然而,为了获得即时有用的地球物理变量并减少数据量,需要一种实时解决该问题的方法。FPGA技术的使用使这成为可能,同时系统可以很容易地重新配置。信号跟踪和处理的限制使得必须完全设计几个新模块。这项工作中描述的已实现系统的独特之处在于能够实时计算四颗同时可见卫星或仅一颗卫星的延迟多普勒图(DDM),但具有更多的频段。首次测试是在海边的悬崖上进行的,证明了该仪器能够从测量的反射GNSS/R信号中实时计算DDM。对这些测量结果的处理将得出海况(主要由表面风和涌浪驱动)与整体DDM形状之间的定量关系。最终目标是利用DDM形状来校正海况对L波段亮度温度的影响,以改进海表面盐度(SSS)的反演。