Abstract

AbstractAuroral Kilometric Radiation (AKR) is terrestrial radio emission that originates in particle acceleration regions along magnetic field lines, coinciding with discrete auroral arcs. AKR viewing geometry is complex due to the confinement of the source regions to nightside local times (LTs) and the anisotropy of the beaming pattern, so observations are highly dependent on spacecraft viewing position. We present a novel, empirical technique that selects AKR emission from observations made with the spin‐axis aligned antenna of the Wind/WAVES instrument, based on the rapidly varying amplitude of AKR across spacecraft spin timescales. We apply the technique to Wind/WAVES data during 1999 day of year 227–257, when the Cassini spacecraft flew past Earth and provided an opportunity to observe AKR from two remote locations. We examine the AKR flux and power, with observations made from LTs of 1700–0300 hr having an average power up to 104 Wsr‐1 larger than those on the dayside and an increasing AKR power observed at higher magnetic latitudes. We perform a linear cross‐correlation between the Wind AKR power and the spacecraft magnetic latitude, showing positive then negative correlation as Wind travels from the Northern to Southern magnetic hemisphere. Statistically significant diurnal modulations are found in the whole 30‐day period and in subsets of the data covering different local time sectors, indicative of a predominantly geometrical effect for remote AKR viewing. The reproduction of well‐known features of the AKR verifies the empirical selection and shows the promise of its application to Wind/WAVES observations.

Highlights

  • Auroral kilometric radiation (AKR) describes amplified radio emission from the Earth that is generated from relativistic, precipitating electrons along magnetic field lines in the auroral zone and resonates at the electron cyclotron frequency (Wu & Lee, 1979)

  • Once wind crosses the magnetic equator at the start of day of year (DOY) 231, the Auroral Kilometric Radiation (AKR) power becomes anti-correlated with Wind's magnetic latitude after perigee; whilst the AKR power decreases as Wind travels away from the nightside and into the dawn sector, the time series clearly shows the dominant emission from the Southern magnetic hemisphere after Wind crosses the magnetic equator

  • We have described a new method of selecting AKR emission from the complex radio environment observed by Wind, using a statistical measure of the variability of radio flux across the spin-axis-aligned Z antenna during a spacecraft spin

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Summary

Introduction

Auroral kilometric radiation (AKR) describes amplified radio emission from the Earth that is generated from relativistic, precipitating electrons along magnetic field lines in the auroral zone and resonates at the electron cyclotron frequency (Wu & Lee, 1979). The instrument was used to retrieve the circular polarization state of the AKR, allowing the general emission characteristics, such as the emission power and the temporal modulation to be studied (Lamy et al, 2010) For this month-long period, the Wind spacecraft was traveling on orbits that carried it through the nightside magnetosphere at perigee, allowing it to make remote observations of the AKR source region, as well as other opportunities to observe AKR from other LTs. it is not possible to apply previously developed GP techniques for spinning spacecraft to AKR observations with Wind, a selection technique based on the observed variability on timescales of seconds has been developed and applied.

Instrumentation and Empirical Data Selection Technique
Radio Background
Calibration
Empirical Selection of AKR
Spacecraft Ephemerides
AKR Flux Density and Power
AKR Viewing Geometry
AKR Temporal Modulation
Conclusion
Findings
Data Availability Statement
Full Text
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