共查询到18条相似文献，搜索用时 109 毫秒
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电离层时空变化规律的研究对于卫星导航、航空航天等具有重要价值。本文利用国际GNSS服务(IGS)产品,分析了电离层的时空变化规律。在时间尺度上,对低阶球谐系数(0,0)、(1,0)、(1,1)、(1,-1)进行了功率谱分析,对北京地区的垂直方向总电子含量(VTEC)进行了短时傅里叶变换分析,对北京、阿克拉和墨尔本进行了季节性分析,结果表明,电离层变化具有明显的年周期和半年周期项。在空间方面,分析了零度子午线、赤道上的电离层延迟随纬度、经度的变化规律,结果表明,在纬度方向上具有明显的单峰效应,在经度方向上的峰值具有延迟变化规律。 相似文献
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利用GPS监测电离层总电子含量的季节性变化 总被引：3，自引：0，他引：3
利用Georgiadiou电离层模型计算了GPS系统硬件延迟，从而由双频伪距观测值获取绝对电离层总电子含量值。利用北京IGS站的GPS观测数据分别计算了2000年和2004年各个不同月份的总电子含量值，对两年各月份的总电子含量进行多项式拟合，发现总电子含量的季节性变化趋势一致。 相似文献
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利用GPS三频观测值监测电离层TEC及其变化率 总被引：1，自引：0，他引：1
三频观测数据为监测电离层总电子含量提供了更多的观测值选择。在双频观测值估算电离层总电子含量的原理基础上,利用不同纬度地区的三频GPS观测资料计算获得了电离层总电子含量值及其变化率。分析结果表明：由于GPS接收机码间偏差的影响,不同频率间组合获得的电离层总电子含量结果出现较大的系统差异,使用不同频率组合获得的电离层TEC变化率有很好的一致性。 相似文献
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根据高精度卫星导航和电离层活动监测的需要,利用全球238个GPS基准站的双频实测数据,通过建立球谐函数模型的同时解算电离层电子含量以及GPS与GLONASS卫星DCB及其相应的接收机DCB;将其结果与CODE、IGS分析中心的结果进行比较分析,表明该方法建立的模型是可靠的,其GPS和GLONASS卫星DCB相对于CODE精度优于0.1ns,相对于IGS精度优于0.2ns,其GPS测站DCB和GLONASS测站DCB相对于CODE和IGS精度优于1ns,垂直总电子含量相对CODE和IGS精度优于3TECU,组合结果精度高于组合前。 相似文献
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利用国际GNSS服务组织(IGS)提供的东经115°经线上不同纬度处一年的电离层总电子含量(TEC)时间序列数据,研究了如何进一步提高基于神经网络方法预测电离层TEC的效果。研究表明:电离层TEC的预测误差与电离层TEC时间序列的最大Lyapunov指数与该序列均值的乘积具有较强的相关性;而且与时间延迟和嵌入维数的选择是否恰当也有着密切关系。 相似文献
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《测绘地理信息》2017,(5)
基于国际GNSS服务(International GNSS Service,IGS)WUHN、BJFS站GPS观测数据,利用码与相位观测值联合解算北京时间2010-01-15、2012-05-21日偏食前后电离层总电子含量(total electronic content,TEC),以此探测两次日偏食过程中的电离层效应。研究分析表明,日偏食期间电离层效应微弱,电离层TEC存在异常扰动,异常过程为先减少、达到最大变化量、逐步恢复正常,该过程与测站日偏食过程具有时间一致性,电离层TEC最大变化量不足1TECU,最大变化时刻滞后食甚时刻1~13min,不存在电离层TEC长时间异常现象。 相似文献
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为了进一步研究磁暴对电离层总电子含量变化的影响,基于2017年9月6日太阳爆发X93级特大耀斑并引发磁暴现象,文中将iGMAS提供的全球电离层总电子含量格网数据与中国科学院空间环境预报中心(SEPC)提供的磁暴环电流指数进行相关性分析,并重点分析了磁暴过程中不同阶段环电流指数与全球不同纬度带电离层总电子含量变化的相关性及影响,结果表明:1) 此次特大耀斑爆发13小时后发生大磁暴,磁暴主相阶段环电流指数与滞后1 h的电离层总电子含量相关系数为-0999 7,即随着磁暴加剧电离层总电子含量迅速增加,恢复相阶段迅速减少并趋于稳定;2) 电离层总电子含量变化随磁暴环电流指数变化而变化,两者变化趋势一致,磁暴强度与电离层总电子含量变化呈强负相关性,磁暴对不同纬度带的电离层总电子含量影响趋于一致,影响程度大小由高纬至低纬逐渐递减;3) 磁暴对不同纬度带的电离层总电子含量变化影响不同步,其影响存在由高纬逐渐延伸至低纬,磁暴主相阶段对不同纬度带的影响时延约为1 h,恢复相阶段时延逐渐消失,电离层电离层总电子含量变化趋于稳定;[JP2]4) 此次磁暴恢复相阶段出现的电离层总电子含量异常变化,还有待进一步研究分析。 相似文献
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《测绘科学》2020,(8)
为了研究分析京津冀地区的电离层时空变化特性,为本地区提供高精度导航定位和授时(PNT)服务,该文以国际GNSS服务(IGS)中心提供的2000—2018年的全球电离层总电子含量(TEC)格网模型产品数据为基础,研究该区域电离层时空分布特性及太阳活动与电离层的相关性。结果表明:电离层TEC与F10.7指数相关系数为0.83,与太阳黑子数相关系数为0.78,与太阳活动呈现出高度相关性;京津冀地区TEC每日最大值出现在UTC4时左右,电离层TEC具有较明显的27 d周期特性,在太阳活动高年及TEC极大递减年会出现冬季异常现象;白天,同一经度TEC值随纬度的升高而降低;同一纬度TEC值随经度的升高没有明显变化。 相似文献
11.
The ionospheric eclipse factor method (IEFM) and its application to determining the ionospheric delay for GPS 总被引：4，自引：1，他引：3
A new method for modeling the ionospheric delay using global positioning system (GPS) data is proposed, called the ionospheric
eclipse factor method (IEFM). It is based on establishing a concept referred to as the ionospheric eclipse factor (IEF) λ
of the ionospheric pierce point (IPP) and the IEF’s influence factor (IFF) . The IEF can be used to make a relatively precise distinction between ionospheric daytime and nighttime, whereas the IFF
is advantageous for describing the IEF’s variations with day, month, season and year, associated with seasonal variations
of total electron content (TEC) of the ionosphere. By combining λ and with the local time t of IPP, the IEFM has the ability to precisely distinguish between ionospheric daytime and nighttime, as well as efficiently
combine them during different seasons or months over a year at the IPP. The IEFM-based ionospheric delay estimates are validated
by combining an absolute positioning mode with several ionospheric delay correction models or algorithms, using GPS data at
an international Global Navigation Satellite System (GNSS) service (IGS) station (WTZR). Our results indicate that the IEFM
may further improve ionospheric delay modeling using GPS data. 相似文献
12.
The anomaly phenomenon of broadcast ionospheric model coefficients of the Global Positioning System (GPS) is revealed after analyzing the navigation file data collected from all the IGS (International GNSS Service) stations worldwide over a 22-year period (1992–2013). GPS broadcast ionospheric coefficients widely used by many single-frequency users to correct the ionosphere errors for numerous GPS applications are usually believed to have only one set/version per day. However, it is found that GPS receivers from the IGS network can report as many as eight sets/versions of ionospheric coefficients in a day. In order to investigate the possible factors for such an anomalous phenomenon, the relationship between the number of coefficient sets and solar cycle, the receiver geographic locations, and receiver types/models are analyzed in detail. The results indicate that most of the coefficients show an annual variation. During the active solar cycle period from mid-1999 to mid-2001, all of the coefficients extracted from IGS navigation files behaved anomalously. Our analysis shows that the anomaly is also associated with GPS receiver types/models. Some types/models of GPS receivers report one set/version of ionospheric coefficients daily, while others report multiple sets. Our analysis also suggests that the ionospheric coefficient anomaly is not necessarily related to ionospheric scintillations. No correlation between the anomaly and geographic location of GPS receivers has been found in the analysis. Using the ionospheric coefficient data collected from 1998 to 2013, the impact of ionospheric coefficient anomaly on vertical total electron content (VTEC) calculation using the Klobuchar model has been evaluated with respect to the Global Ionospheric Maps generated by the Center for Orbit Determination in Europe. With different sets of coefficients recorded on the same day, the resulting VTEC values are dramatically different. For instance on June 1, 2000, the largest VTEC at one of our test stations can be as large as 153.3 TECu (total electron content unit) using one set of coefficients, which is 16.36 times larger than the smallest VTEC of 9.37 TECu computed from using another set of coefficients. 相似文献
13.
Single layer ionosphere models are frequently used for ionospheric modeling and estimation using GPS measurements from a network of GPS reference stations. However, the accuracies of single layer models are inherently constrained by the assumption that the ionospheric electrons are concentrated in a thin shell located at an altitude of about 350 km above Earths surface. This assumption is only an approximation to the physical truth because the electrons are distributed in the entire ionosphere region approximately from 50 to 1,000 km. To provide instantaneous ionospheric corrections for the real-time GPS positioning applications, the ionospheric corrections need to be predicted in advance to eliminate the latency caused by the correction computation. This paper will investigate ionospheric total electron content (TEC) predictions using a multiple-layer tomographic method for ionospheric modeling over a local area GPS reference network. The data analysis focuses on the accuracy evaluation of short-term (5 min in this study) TEC predictions. The results have indicated that the obtainable TEC prediction accuracy is at a level of about 2.8 TECU in the zenith direction and 95% of the total electron content can be recovered using the proposed tomography-based ionosphere model. 相似文献
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Assessment of correct fixing rate for precise point positioning ambiguity resolution on a global scale 总被引：3，自引：1，他引：2
Ambiguity resolution (AR) for a single receiver has been a popular topic in Global Positioning System (GPS) recently. Ambiguity-resolution methods for precise point positioning (PPP) have been well documented in recent years, demonstrating that it can improve the accuracy of PPP. However, users are often concerned about the reliability of ambiguity-fixed PPP solution in practical applications. If ambiguities are fixed to wrong integers, large errors would be introduced into position estimates. In this paper, we aim to assess the correct fixing rate (CFR), i.e., number of ambiguities correctly fixing to the total number of ambiguities correctly and incorrectly fixing, for PPP user ambiguity resolution on a global scale. A practical procedure is presented to evaluate the CFR of PPP user ambiguity resolution. GPS data of the first 3 days in each month of 2010 from about 390 IGS stations are used for experiments. Firstly, we use GPS data collected from about 320 IGS stations to estimate global single-differenced (SD) wide-lane and narrow-lane satellite uncalibrated phase delays (UPDs). The quality of UPDs is evaluated. We found that wide-lane UPD estimates have a rather small standard deviation (Std) between 0.003 and 0.004 cycles while most of Std of narrow-lane estimates are from 0.01 to 0.02 cycles. Secondly, many experiments have been conducted to investigate the CFR of integer ambiguity resolution we can achieve under different conditions, including reference station density, observation session length and the ionospheric activity. The results show that the CFR of PPP can exceed 98.0 % with only 1 h of observations for most user stations. No obvious correlation between the CFR and the reference station density is found. Therefore, nearly homogeneous CFR can be achieved in PPP AR for global users. At user end, higher CFR could be achieved with longer observations. The average CFR for 30-min, 1-h, 2-h and 4-h observation is 92.3, 98.2, 99.5 and 99.7 %, respectively. In order to get acceptable CFR, 1 h is a recommended minimum observation time. Furthermore, the CFR of PPP can be affected by diurnal variation and geomagnetic latitude variation in the ionosphere. During one day at the hours when rapid ionospheric variations occur or in low geomagnetic latitude regions where equatorial electron density irregularities are produced relatively frequently, a significant degradation of the CFR is demonstrated. 相似文献
15.
Experimental analysis was performed using multiplicative algebraic reconstruction technique (MART) to map the ionosphere over Brazil. Code and phase observations from the global navigation satellite system (GNSS) together with the international reference ionosphere (IRI) enabled the estimation of ionospheric profiles and total electron content (TEC) over the entire region. Twenty-four days of data collected from existing ground-based GNSS receivers during the recent solar maximum period were used to analyze the performance of the MART algorithm. The results were compared with four ionosondes. It was demonstrated that MART estimated the electron density peak with the same degree of accuracy as the IRI model in regions with appropriate geometrical coverage by GNSS receivers for tomographic reconstruction. In addition, the slant TEC, as estimated with MART, presented lower root-mean-square error than the TEC calculated by ionospheric maps available from the International GNSS Service (IGS). Furthermore, the daily variations of the ionosphere were better represented with the algebraic techniques, compared to the IRI model and IGS maps, enabling a correlation of the elevation of the ionosphere at higher altitudes with the equatorial ionization anomaly intensification. The tomographic representations also enabled the detection of high vertical gradients at the same instants in which ionospheric irregularities were evident. 相似文献
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利用GPS双频观测数据分析了仪器偏差对计算电离层TEC的影响,结果表明忽略仪器偏差的影响不能正确反映测站上空电离层总电子含量的变化规律。验证了短期内仪器偏差的稳定性,并在此基础上研究了2005年太阳活动低峰年区域电离层VTEC的周年变化规律,揭示了电离层VTEC半年变化、季节性变化及冬季异常等现象。 相似文献
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根据香港GPS永久跟踪站的长期GPS观测资料,估计出了香港地区电离层垂向电子含量,并分析了垂向电子含量的周日变化规律,对建立香港地区实用的电离层模型有重要的指导意义。 相似文献