Rosetta photoelectron emission and solar ultraviolet flux at comet 67P
arXiv:1709.03874 · doi:10.1093/mnras/stx2369
Abstract
The Langmuir Probe instrument on Rosetta monitored the photoelectron emission cur- rent of the probes during the Rosetta mission at comet 67P/Churyumov-Gerasimenko, in essence acting as a photodiode monitoring the solar ultraviolet radiation at wave- lengths below 250 nm. We have used three methods of extracting the photoelectron saturation current from the Langmuir probe measurements. The resulting dataset can be used as an index of the solar far and extreme ultraviolet at the Rosetta spacecraft position, including flares, in wavelengths that are important for photoionisation of the cometary neutral gas. Comparing the photoemission current to data measurements by MAVEN/EUVM and TIMED/SEE, we find good correlation when 67P was at large heliocentric distances early and late in the mission, but up to 50 percent decrease of the expected photoelectron current at perihelion. We discuss possible reasons for the photoemission decrease, including scattering and absorption by nanograins created by disintegration of cometary dust far away from the nucleus.
arXiv comment11 pages, 8 figures, accepted for publication in MNRAS
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Cited by in corpus (8)
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- The evolution of the electron number density in the coma of comet 67P at the location of Rosetta from 2015 November through 2016 March
- Implications from secondary emission from neutral impact on Cassini plasma and dust measurements
- Solar flares observed by Rosetta at comet 67P
- Modeling the Plasma Composition of 67P/C-G at different Heliocentric Distances