Statistical Characteristics of Nighttime ULF Waves Observed on the Surface of Mars by InSight

IF 2.6 2区 地球科学 Q2 ASTRONOMY & ASTROPHYSICS
K. Webster, Y. Ma, S. Joy, P. J. Chi
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Abstract

Interior Exploration using Seismic Investigations, Geodesy and Heat Transport (InSight) Fluxgate Magnetometer returned data from the Martian surface throughout the course of the InSight mission, between November 2018 and May 2022. Ultra-low frequency (ULF) electromagnetic waves are commonly observed by InSight during nighttime hours. We present a collection of 444 nighttime ULF wave events with characteristic frequencies ranging from 1 to 16 mHz (periods from about 1 to 17 min), with a median frequency of about 7 mHz (period of about 140 s). Ultra-low frequency wave activity is found across all nighttime hours, but the activity is more commonly observed after midnight local time. A subset of 104 InSight ULF wave events occur while Mars Atmosphere and Volatile EvolutioN (MAVEN) is located in the solar wind. During these events, the interplanetary magnetic field (IMF) deviates from its nominally expected orientation. We suggest that ULF waves are likely produced in the Martian magnetosphere by at least two different mechanisms and that the occurrence of the ULF waves on the surface is sensitive to the solar wind interaction with the Martian crustal fields. Further measurements by lander or orbiter missions will provide more information about the origin of ULF waves, how they reach the surface during the nighttime, and whether or not ULF waves can be used to perform magnetic sounding to study the subsurface of Mars.

Abstract Image

洞察号在火星表面观测到的夜间极低频波的统计特征
在2018年11月至2022年5月的洞察号任务期间,利用地震调查、大地测量和热传输(InSight)磁通门磁力计从火星表面发回了数据。“洞察号”通常在夜间观测到超低频(ULF)电磁波。我们收集了444个夜间极低频波事件,其特征频率范围为1到16 mHz(周期约为1到17分钟),中位数频率约为7 mHz(周期约为140秒)。超低频波活动在所有夜间时间都可以发现,但在当地时间午夜之后更常见。104个InSight ULF波事件的一个子集发生在火星大气和挥发性演化(MAVEN)位于太阳风中的时候。在这些事件中,行星际磁场(IMF)偏离了其名义上预期的方向。我们认为,极低频波可能在火星磁层中至少通过两种不同的机制产生,并且极低频波在火星表面的发生对太阳风与火星地壳场的相互作用很敏感。着陆器或轨道飞行器的进一步测量将提供更多关于超高频波起源的信息,它们如何在夜间到达火星表面,以及超高频波是否可以用来进行磁探来研究火星地下。
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来源期刊
Journal of Geophysical Research: Space Physics
Journal of Geophysical Research: Space Physics Earth and Planetary Sciences-Geophysics
CiteScore
5.30
自引率
35.70%
发文量
570
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