Spectroscopic signature of Alfvén waves damping in a polar coronal hole up to 0.4 solar radii
arXiv:1204.2544 · doi:10.1088/0004-637X/751/2/110
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 been used to estimate the total energy flux transported by Alfvén waves off-limb in polar coronal hole up to R. The computed Alfvén wave energy flux density progressively decays with altitude from erg cm s at 0.03 R down to erg cm s at 0.4 R, with an average energy decay rate erg cm s. Hence, this result suggests energy deposition by Alfvén waves in a polar coronal hole, thus providing a significant source for coronal heating.
arXiv commentPhysical units of the Alfvén wave Energy Decay Rate revised with respect to the published version. Scientific results and conclusions unchanged
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