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Peer-reviewedCC BY 4.0The Astrophysical Journal

Revisiting the 2014 Camelopardalids Outburst using a Meteor Radar Chain in the Northern Hemisphere

9 affiliations
  1. 1University of Science and Technology of China
  2. 2State Key Laboratory of Environment Characteristics and Effects for Near-space
  3. 3University of Bern
  4. 4ATRAD Pty Ltd.
  5. 5University of Adelaide
  6. 6Chinese Academy of Sciences
  7. 7China Research Institute of Radiowave Propagation
  8. 8Kunming Electro-Magnetic Environment Observation and Research Station
  9. 9Hainan University

Abstract

The Camelopardalids meteor shower (#451, CAM), produced by comet 209P/LINEAR’s historic dust trails, has exhibited a strong outburst only once, on 2014 May 24, since the discovery of the parent body in 2004, and although this event was well predicted, its activity was substantially lower than forecast. Using a meteor radar chain in the northern hemisphere, consisting of five meteor radars spanning from the northeast to the southwest of China, we were able to precisely determine the shower’s radiant as being centered on a region of R.A. = 128 . ° 0 ± 8 . ° 8, decl. = 75 . ° 1 ± 2 . ° 4 (J2000) between UT 05:00 and 13:00. A detailed analysis quantified the shower radiant, duration, velocity, and height from each meteor radar. CAM shower meteors constituted around 10%–20% of the total meteor activity across the radar network with minor site-dependent variations. Orbital parameters with a semimajor axis of ∼2.83 au, eccentricity of ∼0.66, and inclination of ∼19 . ° 0 were consistently derived from the meteor radar chain, further validating the accuracy of past predictions. These joint observations confirmed the dust trail’s dynamical properties despite the shower’s flux being smaller than most of the predictions.

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BibTeX
@article{lu2026revisiting,
  title = {{Revisiting the 2014 Camelopardalids Outburst using a Meteor Radar Chain in the Northern Hemisphere}},
  author = {Maolin Lu and Wen Yi and Xianghui Xue and Gunter Stober and Iain Reid and Tingdi Chen and Guozhu Li and Baiqi Ning and Jinsong Chen and Na Li},
  journal = {The Astrophysical Journal},
  year = {2026},
  month = nov,
  doi = {10.3847/1538-4357/ae9d6d},
  url = {https://iopscience.iop.org/article/10.3847/1538-4357/ae9d6d},
  note = {CC BY 4.0},
}
RIS
TY  - JOUR
TI  - Revisiting the 2014 Camelopardalids Outburst using a Meteor Radar Chain in the Northern Hemisphere
AU  - Maolin Lu
AU  - Wen Yi
AU  - Xianghui Xue
AU  - Gunter Stober
AU  - Iain Reid
AU  - Tingdi Chen
AU  - Guozhu Li
AU  - Baiqi Ning
AU  - Jinsong Chen
AU  - Na Li
PY  - 2026
DA  - 2026/11/03
JO  - The Astrophysical Journal
DO  - 10.3847/1538-4357/ae9d6d
UR  - https://iopscience.iop.org/article/10.3847/1538-4357/ae9d6d
AB  - The Camelopardalids meteor shower (#451, CAM), produced by comet 209P/LINEAR’s historic dust trails, has exhibited a strong outburst only once, on 2014 May 24, since the discovery of the parent body in 2004, and although this event was well predicted, its activity was substantially lower than forecast. Using a meteor radar chain in the northern hemisphere, consisting of five meteor radars spanning from the northeast to the southwest of China, we were able to precisely determine the shower’s radiant as being centered on a region of R.A. = 128 . ° 0 ± 8 . ° 8, decl. = 75 . ° 1 ± 2 . ° 4 (J2000) between UT 05:00 and 13:00. A detailed analysis quantified the shower radiant, duration, velocity, and height from each meteor radar. CAM shower meteors constituted around 10%–20% of the total meteor activity across the radar network with minor site-dependent variations. Orbital parameters with a semimajor axis of ∼2.83 au, eccentricity of ∼0.66, and inclination of ∼19 . ° 0 were consistently derived from the meteor radar chain, further validating the accuracy of past predictions. These joint observations confirmed the dust trail’s dynamical properties despite the shower’s flux being smaller than most of the predictions.
SN  - 1538-4357
SN  - 0004-637X
ER  -