Abstract

Wave–particle interactions are fundamental processes in space plasma, and some plasma waves, including electrostatic solitary waves (ESWs), are recognised as broadband noises (BBNs) in the electric field spectral data. Spacecraft observations in recent decades have detected BBNs around the Moon, but the generation mechanism of the BBNs is not fully understood. Here, we study a wake boundary traversal with BBNs observed by Kaguya, which includes an ESW event previously reported by Hashimoto et al. Geophys Res Lett 37:L19204 https://doi.org/10.1029/2010GL044529 (2010). Focusing on the relation between BBNs and electron pitch-angle distribution functions, we show that upward electron beams from the nightside lunar surface are effective for the generation of BBNs, in contrast to the original interpretation by Hashimoto et al. Geophys Res Lett 37:L19204 https://doi.org/10.1029/2010GL044529 (2010) that high-energy electrons accelerated by strong ambipolar electric fields excite ESWs in the region far from the Moon. When the BBNs were observed by the Kaguya spacecraft in the wake boundary, the spacecraft’s location was magnetically connected to the nightside lunar surface, and bi-streaming electron distributions of downward-going solar wind strahl component and upward-going field-aligned beams (at sim124 eV) were detected. The interplanetary magnetic field was dominated by a positive B_Z (i.e. the northward component), and strahl electrons travelled in the antiparallel direction to the interplanetary magnetic field (i.e. southward), which enabled the strahl electrons to precipitate onto the nightside lunar surface directly. The incident solar wind electrons cause negative charging of the nightside lunar surface, which generates downward electric fields that accelerate electrons from the nightside surface toward higher altitudes along the magnetic field. The bidirectional electron distribution is not a sufficient condition for the BBN generation, and the distribution of upward electron beams seems to be correlated with the BBNs. Ambipolar electric fields in the wake boundary should also contribute to the electron acceleration toward higher altitudes and further intrusion of the solar wind ions into the deeper wake. We suggest that solar wind ion intrusion into the wake boundary is also an important factor that controls the BBN generation by facilitating the influx of solar wind electrons there.Graphical

Highlights

  • Direct observations in orbit around the Moon in the last decades have revealed the plasma environment including plasma waves that are excited due to interactions between the Moon and surrounding space plasmas (e.g. Harada and Halekas 2016; Nakagawa 2016)

  • Together with the fact that one of the strong broadband noises in the current study corresponds to the electrostatic solitary wave (ESW) period reported by Hashimoto et al (2010), we suggest that the Broadband noise (BBN) observed by Kaguya between 04:17 and 04:21 Universal time (UT) are likely to be electrostatic waves, we cannot judge whether these waves are electrostatic or electromagnetic due to the limitation of the magnetic field sample rate (32 Hz)

  • In this paper, we studied a lunar wake boundary traversal with BBNs in the electric field spectral data observed by Kaguya, focusing on electron pitch-angle distributions around the time of the ESW detection previously reported by Hashimoto et al (2010)

Read more

Summary

Graphical Abstract

Introduction Direct observations in orbit around the Moon in the last decades have revealed the plasma environment including plasma waves that are excited due to interactions between the Moon and surrounding space plasmas (e.g. Harada and Halekas 2016; Nakagawa 2016). Hashimoto et al (2010) examined the Kaguya LRS/ WFC waveform data obtained at ∼120 km altitude from the lunar surface and found that ESWs are excited in the lunar wake boundary (which they called Type-A), above magnetic anomalies (Type-B), and over the unmagnetised lunar surface (Type-C). Kaguya observation revealed that BBNs are generated even in the centre of the deep lunar wake These BBNs are caused by bi-streaming electron distributions along the magnetic field that result from intrusion of solar wind ions reflected at the lunar surface or crustal magnetic anomalies on the dayside (Type-II entry) (Nishino et al 2010, 2013). We revisit the Hashimoto et al.’s (2010) Type-A ESW event in the wake boundary on April 2, 2008, under the condition that the magnetic field at the observed location is connected to the nightside lunar surface.

B C D-G H
Discussion
Conclusions
Full Text
Published version (Free)

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call