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Chao Xiong

Researcher at Wuhan University

Publications -  126
Citations -  2181

Chao Xiong is an academic researcher from Wuhan University. The author has contributed to research in topics: Ionosphere & Geomagnetic storm. The author has an hindex of 21, co-authored 103 publications receiving 1290 citations. Previous affiliations of Chao Xiong include China University of Petroleum & Peking Union Medical College.

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IRI-2007 model overestimates electron density during the 23/24 solar minimum

TL;DR: In this paper, the authors compare electron density predictions of the International Reference Ionosphere (IRI-2007) model with in-situ measurements of the satellites CHAMP and GRACE for the years 2000-2009.
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Comparing plasma bubble occurrence rates at CHAMP and GRACE altitudes during high and low solar activity

TL;DR: In this paper, the authors focus on the equatorial plasma bubbles (EPBs) and show that EPBs form regions of depleted plasma along geomagnetic fluxtubes in regions of high occurrence rates.
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The Swarm satellite loss of GPS signal and its relation to ionospheric plasma irregularities

TL;DR: In this article, conditions for loss of GPS signals observed by the Swarm satellites during a 2-year period, from December 2013 to November 2015, were investigated, and the authors concluded that both lower electron density gradients and appropriate GPS receiver settings reduce the probability of GPS signal loss.
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Scale analysis of equatorial plasma irregularities derived from Swarm constellation

TL;DR: In this article, the scale sizes of equatorial plasma irregularities (EPIs) were investigated using measurements from the Swarm satellites during its early mission and final constellation phases, and they found that with longitudinal separation between Swarm satellites larger than 0.4°, no significant correlation was found any more.
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Global features of the disturbance winds during storm time deduced from CHAMP observations

TL;DR: In this article, the authors used the CHAMP zonal wind observations from 2001 to 2005 to investigate the global features of the disturbance winds during magnetically disturbed periods, and they showed that the disturbance zonal winds are mainly westward, which increases with magnetic activity and latitude.