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Thermospheric density variations during extreme geomagnetic storms and their potential impact on the orbit of the China space station

Zhang, Kun, Huang, Yanshi, Wei, Fengsi, Zuo, Pingbing, Yang, Hao, Ji, Jinlong, and Chen, Zehao, 2025. Thermospheric density variations during extreme geomagnetic storms and their potential impact on the orbit of the China space station. Frontiers in Astronomy and Space Sciences, 12:1644152, doi:10.3389/fspas.2025.1644152.

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BibTeX

@ARTICLE{2025FrASS..1244152Z,
       author = {{Zhang}, Kun and {Huang}, Yanshi and {Wei}, Fengsi and {Zuo}, Pingbing and {Yang}, Hao and {Ji}, Jinlong and {Chen}, Zehao},
        title = "{Thermospheric density variations during extreme geomagnetic storms and their potential impact on the orbit of the China space station}",
      journal = {Frontiers in Astronomy and Space Sciences},
     keywords = {thermospheric density, geomagnetic storm, orbit decay, space weather, china space station},
         year = 2025,
        month = oct,
       volume = {12},
          eid = {1644152},
        pages = {1644152},
     abstract = "{Temporal variation and spatial distribution of the thermospheric density
        can change significantly during geomagnetic storms. These
        variations in thermospheric density enhance atmospheric drag,
        posing risks to Low-Earth-Orbit (LEO) spacecraft. Therefore,
        studying the characteristics of intense storm-time thermospheric
        density perturbations and orbit decay is crucial for practical
        applications. In this study, neutral density was simulated for
        the strongest magnetic storm events of solar cycles 24, 23, and
        22, corresponding to minimum Dst indices of ‑234 nT (2015 St.
        Patrick's Day storm), ‑442 nT (20 November 2003 storm), and ‑598
        nT (1989 Quebec blackout storm). Four representative
        thermospheric models (DTM-2020, JB 2008, NRLMSIS 2.0, and TIEGCM
        2.0) were employed to evaluate their performance during extreme
        geomagnetic storms by comparing simulated densities with
        satellite observations from Swarm, CHAMP, and GRACE during the
        November 2003 and March 2015 storm events. The results indicate
        that the errors of all models exhibit larger errors in the main
        and recovery phases, with a bias toward underestimation of
        density during the main phase. It is important to note that no
        thermospheric model is perfect and each model has its own
        limitations, especially dealing with extreme space weather
        events. Although JB2008 performs relatively well, it does not
        maintain the best performance across all phases, and its
        predictions still deviate from observations by at least 20\%.
        Therefore, combining multiple model outputs is recommended for
        extreme cases. Furthermore, these thermospheric models were
        coupled with the High-Precision Orbit Propagator (HPOP) to
        examine the orbital decay of the China Space Station (CSS,
        {\ensuremath{\sim}}380{\textendash}400 km altitude) during these
        events. The effects of drag on CSS during the strongest magnetic
        storm events in the 24th, 23rd and 22nd solar cycles were
        simulated. The orbital decay is about 233\%, 300\% and 266\%
        higher than that in the quiet period, respectively. The reults
        of this study might serve as a reference for spacecraft for
        possible upcoming extreme magnetic storm events.}",
          doi = {10.3389/fspas.2025.1644152},
       adsurl = {https://ui.adsabs.harvard.edu/abs/2025FrASS..1244152Z},
      adsnote = {Provided by the SAO/NASA Astrophysics Data System}
}

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