On Energization and Loss of the Ionized Heavy Atom and Molecule in Mars' Atmosphere
J. -T. Zhao, Q. -G. Zong, Z. -Y. Liu, X. -Z. Zhou, S. Wang, W. -H. Ip,, C. Yue, J. -H. Li, Y. -X. Hao, R. Rankin, A. Degeling, S. -Y. Fu, H. Zou, and, Y. -F. Wang

TL;DR
This study reveals that Mars' crustal magnetic fields can enhance atmospheric loss by facilitating plasma wave-particle interactions, leading to increased ion escape driven by solar wind-induced ultra-low frequency waves.
Contribution
It demonstrates that crustal magnetic fields, rather than global magnetic fields, can promote atmospheric erosion through plasma wave interactions, a counterintuitive insight supported by MAVEN data and simulations.
Findings
Crustal magnetic fields cause ion resonance with ULF waves.
Resonance leads to energization and escape of O+ ions.
Solar wind drives ULF wave excitation, enhancing atmospheric loss.
Abstract
The absence of global magnetic fields is often cited to explain why Mars lacks a dense atmosphere. This line of thought is based on a prevailing theory that magnetic fields can shield the atmosphere from solar wind erosion. However, we present observations here to demonstrate a counterintuitive understanding: unlike the global intrinsic magnetic field, the remnant crustal magnetic fields can enhance atmosphere loss when considering loss induced by plasma wave-particle interactions. An analysis of MAVEN data, combined with observation-based simulations, reveals that the bulk of O+ ions would be in resonance with ultra-low frequency (ULF) waves when the latter were present. This interaction then results in significant particle energization, thus enhancing ion escaping. A more detailed analysis attributes the occurrence of the resonance to the presence of Mars' crustal magnetic fields,…
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Taxonomy
TopicsPlanetary Science and Exploration
