Ionospheric Remote Sensing with GNSS

dc.contributor.authorPeng, YuXiangen
dc.contributor.authorScales, Wayne A.en
dc.date.accessioned2021-11-29T13:25:15Zen
dc.date.available2021-11-29T13:25:15Zen
dc.date.issued2021-11-22en
dc.date.updated2021-11-25T16:00:15Zen
dc.description.abstractThe Global Navigation Satellite System (GNSS) plays a pivotal role in our modern positioning, navigation and timing (PNT) technologies. GNSS satellites fly at altitudes of approximately 20,000 km or higher. This altitude is above an ionized layer of the Earth’s upper atmosphere, the so called “ionosphere”. Before reaching a typical GNSS receiver on the ground, GNSS satellite signals penetrate through the Earth’s ionosphere. The ionosphere is a plasma medium consisting of free charged particles that can slow down, attenuate, refract, or scatter the GNSS signals. Ionospheric density structures (also known as irregularities) can cause GNSS signal scintillations (phase and intensity fluctuations). These ionospheric impacts on GNSS signals can be utilized to observe and study physical processes in the ionosphere and is referred to ionospheric remote sensing. This entry introduces some fundamentals of ionospheric remote sensing using GNSS.en
dc.description.versionPublished versionen
dc.format.mimetypeapplication/pdfen
dc.identifier.citationPeng, Y.; Scales, W.A. Ionospheric Remote Sensing with GNSS. Encyclopedia 2021, 1, 1246-1256.en
dc.identifier.doihttps://doi.org/10.3390/encyclopedia1040094en
dc.identifier.urihttp://hdl.handle.net/10919/106762en
dc.language.isoenen
dc.publisherMDPIen
dc.rightsCreative Commons Attribution 4.0 Internationalen
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/en
dc.subjectGNSSen
dc.subjectionosphereen
dc.subjectremote sensingen
dc.titleIonospheric Remote Sensing with GNSSen
dc.title.serialEncyclopedia 2021en
dc.typeArticle - Refereeden
dc.type.dcmitypeTexten

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