the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Bursty bulk flow ionospheric impacts from triple-conjunctive observations
Abstract. Substorms are the regular reconfiguration of the Earth's geomagnetic space environment, and magnetosphere-ionosphere coupling is integral to the substorm chain. Bursty bulk flows (BBFs) are mesoscale fast plasma flows that are released from magnetic reconnection sites in the magnetotail during substorms, and they couple to the ionosphere through field aligned current (FAC) systems. BBFs may drive localised changes to the ionospheric plasma, such as velocity flows or changes to the local temperature, density and conductivity, but determining the specific ionospheric effects of a given BBF and their associated FAC is a complex undertaking. In this study we identify triple-conjugate observations of BBF detections within the magnetotail, FAC observations in low Earth orbit and ground-based radar stations that observe the local ionospheric plasma in order to evaluate the different components of the coupled BBF-FAC-ionosphere system. We evaluate over 11000 BBFs and identify only 13 events that satisfy our conjunctive criteria. We perform detailed analysis of one of these BBFs, which occurred in the recovery phase of a relatively weak substorm, to evaluate the FAC associated with this BBF and its ionospheric impacts. Multiple FAC signatures were observed that are associated with the BBF, in addition to variations in the ionospheric velocity and temperature. There is an ongoing need for coordinated observations of the coupled BBF-FAC-ionosphere system to further distinguish the ionospheric impacts of BBFs from broader substorm dynamics.
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Status: open (extended)
- RC1: 'Comment on egusphere-2026-3108', Anonymous Referee #1, 31 Jul 2026 reply
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Conjunctions: BBF-radar and Swarm-radar H. George, A. P. Dimmock, V. Lanabare, H. Vanhamaki, I. Virtanen, and A. Aikio https://doi.org/10.5281/zenodo.20448703
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Bursty bulk flow ionospheric impacts from triple-conjunctive observations
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George et al.
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This study combines observations from THEMIS, Swarm, the Poker Flat incoherent scatter radar, a co-located all-sky camera, and ground magnetometer stations to study the ionospheric signatures of a bursty bulk flow. Due to the requirement to have conjunctions between so many instruments, very few suitable events were found, and only one was studied in detail. The observations show that it is difficult to determine a one-to-one correspondence between the BBF observed in the tail by THEMIS and ionospheric signatures; rather, the large-scale response of the magnetosphere/ionosphere to the substorm dominates the measurements. Despite this, the paper is a useful and interesting addition to the literature on BBFs and I recommend it for publication in Annales Geophysicae. I have only a minor comment, which is that it would be useful if the paper gave some more emphasis to the MLT of the BBF footprint. This is, I believe, in the dawn sector, so away from the typical onset region of substorms