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Assessment of ionosphere tomographic modeling performance using GPS data during the October 2003 geomagnetic storm event

机译:在2003年10月的地磁风暴事件中使用GPS数据对电离层层析成像建模性能进行评估

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摘要

Precise ionospheric modeling is important for single-frequency Global Positioning System (GPS) users to achieve optimal positioning accuracy because the ionospheric signal delay is now the largest error source for positioning and navigation with GPS. The ionospheric modeling during ionospheric storms is particularly critical since the signal delay may be higher than normal and may differ significantly from the broadcast ionosphere model (currently employed by single-frequency users). In this study, a tomographic technique is used to model the ionosphere over North America using data collected from a network of dual-frequency GPS receivers. In support of real-time applications of the ionosphere model, short-term (5-min) forecasts of ionospheric total electron content (TEC) are also performed. To validate the accuracy of the forecast ionospheric TEC, a comparison of the TEC predictions with the observed TEC data (which are inferred from dual-frequency GPS observations) is carried out. Analyses are conducted using GPS data recorded during a 2003 geomagnetic storm event (29-31 October). Results indicate that under less disturbed conditions, an average accuracy of 5 ~ 6.5 total electron content units (TECU, 1 TECU = 10~(16) el m~(-2)) can be obtained for the vertical TEC prediction and that 80% of slant TEC can be recovered by the model predictions. During extreme ionospheric storm periods (Kp = 9), the vertical TEC forecasting accuracy has a degradation of 2 ~ 3 TECU from the 3-day mean value, and the relative error is several percent to 10% larger than the 3-day average level.
机译:精确的电离层建模对于单频全球定位系统(GPS)用户获得最佳定位精度至关重要,因为电离层信号延迟现在是GPS定位和导航的最大误差源。电离层风暴期间的电离层建模尤为重要,因为信号延迟可能会比正常情况高,并且可能与广播电离层模型(当前由单频用户采用)有显着差异。在这项研究中,层析成像技术用于使用从双频GPS接收器网络收集的数据对北美电离层进行建模。为了支持电离层模型的实时应用,还对电离层总电子含量(TEC)进行了短期(5分钟)预测。为了验证预测的电离层TEC的准确性,将TEC预测与观测到的TEC数据(由双频GPS观测推断出)进行了比较。使用2003年地磁风暴事件(10月29日至31日)期间记录的GPS数据进行分析。结果表明,在较少干扰的条件下,垂直TEC预测的平均精度为5〜6.5个总电子含量单位(TECU,1 TECU = 10〜(16)el m〜(-2))。倾斜TEC可以通过模型预测来恢复。在极端电离层风暴期间(Kp = 9),垂直TEC预报精度从3天平均值下降了2〜3 TECU,相对误差比3天平均值大了几个百分点到10%。 。

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