Determine the shear-to-magnetic-energy conversion and upward survival of photospheric KHI stress
Determine the product of the shear-to-magnetic-energy conversion efficiency and the fraction of that magnetic stress that survives upward transport through the chromosphere into the corona for DKIST-observed photospheric Kelvin–Helmholtz vortices.
References
The heating calculations in this Letter are based on energy budget estimation using DKIST observations and the recently obtained scaling laws of collisionless magnetic reconnection. However, they are not yet a proof that the DKIST observed vortices already heat the corona. The controlling unknown is the product of the shear-to-magnetic energy conversion and the upward survival of that stress through the chromosphere into corona.
I cannot yet assign a solar conversion efficiency, because the lower solar atmosphere is partially ionized, stratified, and more collisional than the magentosheath-magnetopause-magnetosphere system.
These waves can carry a substantial part of the local shear-energy surplus and can heat particles, but their solar efficiency is not known.