Evidence of Subproton‐Scale Magnetic Holes in the Venusian Magnetosheath
Abstract
Depressions in magnetic field strength, commonly referred to as magnetic holes, are
observed ubiquitously in space plasmas. Subproton-scale magnetic holes with spatial scales smaller
than or on the order of a proton gyroradius, are likely supported by electron current vortices, rotating
perpendicular to the ambient magnetic field. While there are numerous accounts of subproton-scale
magnetic holes within the Earth’s magnetosphere, there are few, if any, reported observations in other
space plasma environments. We present the first evidence of subproton-scale magnetic holes in the
Venusian magnetosheath. During Parker Solar Probe’s first Venus Gravity Assist, the spacecraft crossed
the planet’s bow shock and subsequently observed the Venusian magnetosheath. The FIELDS instrument
suite onboard the spacecraft achieved magnetic and electric field measurements of magnetic hole
structures. The electric fields associated with magnetic depressions are consistent with electron current
vortices with amplitudes on the order of 1µA/m2
.
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