Publications related to the GRACE Missions (no abstracts)

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Global Observational Comparison of Large–Scale Traveling Atmospheric and Ionospheric Disturbances During the May 2024 Geomagnetic Storm

Wei, Xiaolong, Jiang, Guoying, Zhu, Yajun, Li, Yongping, Ai, Jiangzhao, Han, Tingwei, Le, Huijun, Zhang, Aibin, and Xu, Jiyao, 2026. Global Observational Comparison of Large–Scale Traveling Atmospheric and Ionospheric Disturbances During the May 2024 Geomagnetic Storm. Geophysical Research Letters, 53(12):e2026GL123318, doi:10.1029/2026GL123318.

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BibTeX

@ARTICLE{2026GeoRL..5323318W,
       author = {{Wei}, Xiaolong and {Jiang}, Guoying and {Zhu}, Yajun and {Li}, Yongping and {Ai}, Jiangzhao and {Han}, Tingwei and {Le}, Huijun and {Zhang}, Aibin and {Xu}, Jiyao},
        title = "{Global Observational Comparison of Large-Scale Traveling Atmospheric and Ionospheric Disturbances During the May 2024 Geomagnetic Storm}",
      journal = {\grl},
     keywords = {LSTADs, LSTIDs, comparison, geomagnetic storm},
         year = 2026,
        month = jun,
       volume = {53},
       number = {12},
          eid = {e2026GL123318},
        pages = {e2026GL123318},
     abstract = "{During the geomagnetic storm on 10 May 2024, neutral density
        measurements from 14 Tianmu, Swarm, and GRACE-FO satellites at
        {\ensuremath{\sim}}510 km altitude, combined with total electron
        content (TEC) observations, enabled the first global
        observational comparison of large-scale traveling atmospheric
        and ionospheric disturbances (LSTADs/TIDs) via snapshots and
        keograms. LSTADs/TIDs exhibited similar wavefronts aligned with
        geomagnetic latitude, spanning 90--180{\textdegree} in longitude,
        originating from auroral or cusp Joule heating regions on both
        day and night sides. They propagated along overlapping
        meridional trajectories at 450--1,100 m/s. LSTADs lag LSTIDs by
        {\ensuremath{\sim}}30 min due to the phase polarization and
        differing observation heights. Besides, rare instantaneous
        neutral density enhancements were detected at low to mid
        latitudes during storm onset. These findings provide near-
        continuous global observational insights into storm-time
        thermosphere-ionosphere wave coupling and demonstrate a feasible
        approach for future global LSTADs monitoring through empirical
        mode decomposition adaptive filtering of multi-satellite data.}",
          doi = {10.1029/2026GL123318},
       adsurl = {https://ui.adsabs.harvard.edu/abs/2026GeoRL..5323318W},
      adsnote = {Provided by the SAO/NASA Astrophysics Data System}
}

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