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Kalman Filter Based Robust GNSS Signal Tracking Algorithm in Presence of Ionospheric Scintillations

机译:基于Kalman滤波器的鲁棒GNSS信号跟踪算法在存在电离层闪烁

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Ionospheric scintillations are created by diffraction when the transmitted propagating waves encounter a medium made of irregular structures with variable refraction indexes. The recombination of the waves after propagation can be constructive or destructive and the resulting signal at output of the receiver antenna may present rapid variations of phase and amplitude. Scintillations are essentially observed in the regions located under the geomagnetic equator, where irregularities in the ionosphere like plasma bubbles occur more frequently. They also happen over Polar Regions and are associated with the penetration of charged particles along the magnetic field lines. Under the auroral oval region, scintillations can be local or spread over a great part of the oval. According to past observations scintillations occur mainly at the period of the equinox and the solstice. During the rest of the time there are almost no observations. After sunset, the modification in the ionosphere layers generates such variations. Scintillations cause very brutal and fast fades of the received signal, and once these phenomena occur they can last from 30 minutes up to several hours.
机译:当透射的传播波遇到由具有可变折射率的不规则结构制成的介质时,通过衍射产生电离层闪烁。传播之后波的重组可以是建设性的或破坏性的,并且接收器天线输出时的所得信号可以存在相位和幅度的快速变化。在位于地磁赤道下方的区域基本上观察到闪烁,其中电离层中的不规则性更频繁地发生。它们也发生在极地区域上,并且与沿磁场线的带电粒子的穿透相关联。在极光椭圆形区域下,闪烁可以是局部的或涂抹在椭圆形的大部分中。根据过去的观察结果,闪烁主要发生在昼夜平分时间和溶剂的时期。在剩下的时间内几乎没有观察。在日落之后,电离层层中的修饰产生了这种变化。闪烁导致接收信号的野蛮和快速淡出,并且一旦这些现象发生,它们就可以持续30分钟即可达到几个小时。

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