Equatorial plasma bubbles observed by DMSP satellites during a full solar cycle: Toward a global climatology
By Chao-Song Huang, W. J. Burke, J. Machuzak, L. Gentile, P. J. Sultan. 2002
167 citations recorded by the source corpus.
Subfields: Aerospace Engineering, Astronomy and Astrophysics
View Paper: https://www.semanticscholar.org/paper/b2aaf9ba004a98cfbf4efd9cb5160858ddf2677d
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In Aerospace Engineering
In Astronomy and Astrophysics
- Michi Nishioka
- Takuya Tsugawa
- M. Denton
- J. Borovsky
- Akinori Saito
- W. J. Burke
- L. Gentile
- Yuichi Otsuka
Citations in the corpus
- Differences between CME‐driven storms and CIR‐driven storms (2006, background): “[30] Large equatorial bubbles, which appear in the topside ionosphere when Dst is increasing in magnitude [Huang et al., 2002; Basu et al., 2005], have been reported for many CME-driven magnetic storms [e.g., Huang et al., 2001; Abdu et al., 2003; Basu et al., 2005].”
- Occurrence characteristics of plasma bubble derived from global ground‐based GPS receiver networks (2007, methodology): “Atlantic regions. (1), (2), (3), and (4) after probabilities indicate that the results come from Huang et al. [2002] , Makela et al. [2004], Kim et al. [2002], and Sahai et al. [2000], respectively.”
- Seasonal-longitudinal variability of equatorial plasma bubbles (2004, methodology): “1 of Huang et al. (2002) demonstrates more than an order of magnitude range in rates of EPB occurrence between solar maximum and minimum, the annual variation ofα at a given longitude is independent of the solar cycle.”