首页> 外文会议>Progress in electromagnetics research symposium >Analysis of Speed and Acceleration of GPS/GLONASS Phase in the Polar Ionosphere
【24h】

Analysis of Speed and Acceleration of GPS/GLONASS Phase in the Polar Ionosphere

机译:极地电离层中GPS / GLONASS相的速度和加速度分析

获取原文

摘要

Currently polar ionosphere is of great interest. This is connected with creation of global model of ionospheric storms and providing stable navigation in polar region. Currently dual- and multi-frequency GNSS phase measurements have been utilized widely and these measurements combination yields us current TEC-values along all SV's linc-of-sights in view. One of the main parameters is stability of phase measurements and their noise level. We carry out the GNSS signal monitoring campaign under the polar ionosphere condition (in Taimyr cape. Russia) in 2013. JAVAD Dclta-G3T receiver was used. We observed amount of the rapid and sharp phase acceleration variations. The absolute value of these variations were as much as 30-40% up to 2-2.5 times higher in comparison the background level for both GPS and GLONASS signals. In some cases we found a strong positive correlation between the phase acceleration variations and TEC variations in the variation frequency band of 0.08-1 Hz. It is well known that this frequency band relates to the 1-st Fresnel zone sized ionospheric irregularities. On the other hand we found some cases when there was no an obvious correlation between the 0.08-1 Hz TEC-variations and the phase acceleration variations. In these cases the phase acceleration variations could be inspired by the SV's reference oscillator frequency drift. In order to separate all the observed phase acceleration variations according to they physical origin we arranged a new measurement campaign of both GPS and GLONASS signals in Norilsk (69°N. 88°E) and Irkutsk (52°N, 104°E). Additionally we used Moscow (55°N, 37°E) data. This report is devoted to discussion of the main results of the campaign data treatment.
机译:目前极地电离层非常兴趣。这与建立电离层风暴的全局模型相连,并在极地区域提供稳定的导航。目前频繁使用双和多频率GNSS相测量,并且这些测量组合在视野中沿着所有SV的景点沿着所有SV的景点产生了美国当前的TEC值。主要参数之一是相位测量的稳定性及其噪声水平。我们在极地电离层条件下进行了GNSS信号监测活动(在Taimyr Cape。俄罗斯).Mavad DCLTA-G3T接收器使用。我们观察到了快速和尖锐的相加速变化的数量。与GPS和GLONASS信号的背景电平相比,这些变化的绝对值高达2-2.5倍。在某些情况下,我们发现了0.08-1Hz的变化频带的相加速度变化和TEC变化之间的强烈正相关。众所周知,该频带涉及1-ST菲涅耳区尺寸尺寸的电离层不规则性。另一方面,当0.08-1 Hz Tec变化和相加速度变化没有明显相关性时,我们发现了一些情况。在这些情况下,可以通过SV的参考振荡器频率漂移激发相加速度变化。为了根据它们的物理来源分离所有观察到的相加速度变化,我们在Norilsk(69°N.8°E)和Irkutsk(52°N,104°E)中布置了GPS和Glonass信号的新测量运动。此外,我们使用莫斯科(55°N,37°E)数据。本报告致力于讨论竞选数据处理的主要结果。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号