A State-Based Method to Simultaneously Reduce Cycle Slips and Noise in Coherent GNSS-R Phase Measurements From Open-Loop Tracking

The carrier phase measurements of coherent Global Navigation Satellite Systems Reflectometry (GNSS-R)signals have demonstrated the potential for high-accuracy altimetry applications. However, the coherent components in the reflected signal are often accompanied by noncoherent scattered signals, whic...

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Bibliographic Details
Published in:IEEE transactions on geoscience and remote sensing 2021-10, Vol.59 (10), p.8873-8884
Main Authors: Wang, Yang, Breitsch, Brian, Morton, Yu T. Jade
Format: Article
Language:English
Subjects:
Altimetry
Cycle slips
Earth orbit
Earth orbits
Extraterrestrial measurements
Global navigation satellite system
Global Navigation Satellite Systems Reflectometry (GNSS-R)
Ionosphere
Ionospheric propagation
Low earth orbits
Navigation
Navigation satellites
Navigational satellites
Oceans
open loop (OL)
Phase measurement
Radio occultation
Radio signals
Satellite tracking
Satellites
Sea ice
Sea measurements
Sea surface
sea surface height (SSH)
Signal to noise ratio
Troposphere
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Summary:The carrier phase measurements of coherent Global Navigation Satellite Systems Reflectometry (GNSS-R)signals have demonstrated the potential for high-accuracy altimetry applications. However, the coherent components in the reflected signal are often accompanied by noncoherent scattered signals, which may cause numerous cycle slips in the conventional open-loop (OL) tracking and postprocessing approach. These cycle slips can lead to meter-level errors in the altimetry retrieval. This article presents a simultaneous cycle slip and noise filtering (SCANF) method for dual-frequency GNSS-R phase measurements generated by OL tracking. The performance of this method is demonstrated using real GNSS-R phase measurements recorded by receivers on board Spire's low-Earth orbit (LEO) satellites. The retrieved sea surface height anomaly (SSHA) has an average root mean square (rms) of 7.3 cm for sea and sea ice surface reflections relative to the mean sea surface (MSS). The technique presented in this article is also applicable to GNSS carrier phase measurements obtained under other challenging conditions, such as signals propagating through ionosphere plasma structures, radio occultation (RO) signals traversing lower troposphere, and multipath-rich environments.
ISSN:0196-2892
1558-0644
DOI:10.1109/TGRS.2020.3036031