Spectroscopic signature of Alfv\'en waves damping in a polar coronal hole up to 0.4 solar radii
Bemporad Alessandro, Abbo Lucia

TL;DR
This study uses spectroscopic data from Hinode to analyze Alfvén wave damping in a polar coronal hole, showing energy decay with altitude and suggesting wave-driven heating of the solar corona.
Contribution
First direct measurement of Alfvén wave energy flux decay in a polar coronal hole up to 0.4 solar radii using spectroscopic observations.
Findings
Alfvén wave energy flux decreases from 1.2×10^6 to 8.5×10^3 erg cm^-2 s^-1 with altitude
Spectral line broadening indicates wave damping and energy deposition in the corona
Results support Alfvén waves as a significant source of coronal heating
Abstract
Between February 24-25, 2009, the EIS spectrometer onboard the Hinode spacecraft performed special "sit & stare" observations above the South polar coronal hole continuously over more than 22 hours. Spectra were acquired with the 1" slit placed off-limb covering altitudes up to 0.48 R ( Mm) above the Sun surface, in order to study with EIS the non-thermal spectral line broadenings. Spectral lines such as Fe {\sc xii} 186.88, Fe {\sc xii} 193.51, Fe {\sc xii} 195.12 and Fe {\sc xiii} 202.04 are observed with good statistics up to high altitudes and they have been analyzed in this study. Results show that the FWHM of Fe {\sc xii} 195.12 line increases up to R, then decreases higher up. EIS stray light has been estimated and removed. Derived electron density and non-thermal velocity profiles have…
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