2021
DOI: 10.1029/2021sw002858
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Real‐Time Monitoring of Ionosphere VTEC Using Multi‐GNSS Carrier‐Phase Observations and B‐Splines

Abstract: Real-time monitoring of the ionospheric plasma distribution and associated irregularities is of increasing importance for users of the Global Navigation Satellite Systems (GNSS) in various fields such as telecommunication, positioning, navigation, aviation, natural disaster monitoring and warning. It is also vital to monitor the ionosphere in real-time for forecasting space weather events. Rapid technological advances in the fast transmission of big data allow for generating and disseminating the essential ion… Show more

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Cited by 9 publications
(3 citation statements)
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“…However, considering that the final GIMs are usually provided with a time delay of 1-2 weeks, and the rapid GIMs with 1-2 days [53], their application in real-time is not possible. There are also ultra-rapid GIMs provided with latency of 2-3 h [54] and real-time (RT) GIMs [53,55]. The accuracy of RT GIMs is typically worse than final, post-processed GIMs due to the shorter span of observations, higher noise in carrier-to-code leveling, and difficulty in carrier ambiguity estimation in real-time processing mode [53].…”
mentioning
confidence: 99%
“…However, considering that the final GIMs are usually provided with a time delay of 1-2 weeks, and the rapid GIMs with 1-2 days [53], their application in real-time is not possible. There are also ultra-rapid GIMs provided with latency of 2-3 h [54] and real-time (RT) GIMs [53,55]. The accuracy of RT GIMs is typically worse than final, post-processed GIMs due to the shorter span of observations, higher noise in carrier-to-code leveling, and difficulty in carrier ambiguity estimation in real-time processing mode [53].…”
mentioning
confidence: 99%
“…The JASON-3 altimetry satellite with a mean orbital altitude of approximately 1336 km can directly obtain the JASON-3 VTEC observations using the dual-frequency signals, i.e., Ku-band (13.575 GHz) and C-band (5.3 GHz) [26,27]. The calculation formula of the JASON-3 VTEC is expressed as Equation ( 3) below [28,29]. The sampling frequency of the JASON-3 satellite is 1 Hz [12].…”
Section: Validation Against Jason Vtecmentioning
confidence: 99%
“…Thus, if one derives thermospheric variations only from TLEs, what obtained is only the integral changes with temporal resolution around 1 day along the specific orbits. However, if the number of spacecraft (and even space debris) is taken into count, and each orbital object is considered as an orbiting station to the thermosphere, the integrated usage of these stations' observations could bring new information of the thermosphere, just like the GNSS signals are used to describe the ionosphere (Erdogan et al., 2021; Jakowski et al., 2012; Mannucci et al., 1998; Ren et al., 2016).…”
Section: Introductionmentioning
confidence: 99%