Abstract
AbstractOne of the most important modes of planet/solar wind interaction are “foreshock transients” such as hot flow anomalies (HFAs). Here we present early observations by the NASA Mars Atmosphere and Volatile EvolutioN spacecraft, confirming their presence at Mars and for the first time at an unmagnetized planet revealing the underlying ion perturbations that drive the phenomenon, finding them to be weaker than at magnetized planets. Analysis revealed the HFA to be virtually microscopic: the smallest on record at ∼2200 km across and commensurate with the local proton gyroradius, resulting in a much stronger perturbation in solar wind protons than alpha particles. As at Venus, despite being physically diminutive, the HFA is still large (0.66 RM) when compared to the relative size of the induced magnetosphere. Given the associated order of magnitude decrease in solar wind dynamic pressure (411 pPa 
 70 pPa), we find that HFAs at Mars have the potential to directly impact the topside ionosphere. We thus hypothesize that the loss of a planetary magnetic dynamo left Mars far more vulnerable to the pressure pulses resulting from HFAs and related foreshock transients.
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References
40
[2]
Ball R. S. (1901)
[29]
Comprehensive study of the magnetospheric response to a hot flow anomaly
Journal of Geophysical Research: Oceans 10.1029/1998ja900021
[31]
In Situ Evidence for an Ancient Aqueous Environment at Meridiani Planum, Mars

S. W. Squyres, J. P. Grotzinger, R. E. Arvidson et al.

Science 10.1126/science.1104559
[33]
Hybrid simulation of the formation of a hot flow anomaly

V. A. Thomas, D. Winske, M. F. Thomsen et al.

Journal of Geophysical Research: Oceans 10.1029/91ja01092
Cited By
32
Martian Atmospheric Loss Through Foreshock Transient Events

Alexandros C. Cooke‐Politikos, Sergey Shuvalov · 2026

Geophysical Research Letters
Planetary and Space Science
Metrics
32
Citations
40
References
Details
Published
Nov 05, 2015
Vol/Issue
42(21)
Pages
9121-9127
License
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Cite This Article
Glyn Collinson, Jasper Halekas, Joseph Grebowsky, et al. (2015). A hot flow anomaly at Mars. Geophysical Research Letters, 42(21), 9121-9127. https://doi.org/10.1002/2015gl065079
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