Possible Evolution of Minifilament-Eruption-Produced Solar Coronal Jets, Jetlets, and Spicules, into Magnetic-Twist-Wave "Switchbacks" Observed by the Parker Solar Probe (PSP)
Alphonse C. Sterling, Ronald L. Moore, Navdeep K. Panesar, and Tanmoy, Samanta

TL;DR
This paper proposes that solar coronal jets, jetlets, and spicules can evolve into magnetic-twist wave switchbacks observed by the Parker Solar Probe, linking small-scale solar features to large-scale solar wind phenomena.
Contribution
It introduces a hypothesis that magnetic twist from solar jets and smaller features can generate switchbacks, connecting solar surface activity to in-situ solar wind observations.
Findings
Coronal jets can produce Alfvénic twist pulses that become switchbacks.
Jetlets and spicules may also generate shorter-duration switchbacks.
Estimated durations of switchbacks vary from a few seconds to about an hour.
Abstract
Many solar coronal jets result from erupting miniature-filament ("minifilament") magnetic flux ropes that reconnect with encountered surrounding far-reaching field. Many of those minifilament flux ropes are apparently built and triggered to erupt by magnetic flux cancelation. If that cancelation (or some other process) results in the flux rope's field having twist, then the reconnection with the far-reaching field transfers much of that twist to that reconnected far-reaching field. In cases where that surrounding field is open, the twist can propagate to far distances from the Sun as a magnetic-twist Alfvenic pulse. We argue that such pulses from jets could be the kinked-magnetic-field structures known as "switchbacks," detected in the solar wind during perihelion passages of the Parker Solar Probe (PSP). For typical coronal-jet-generated Alfvenic pulses, we expect that the switchbacks…
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