Near-UV OH Prompt Emission in the Innermost Coma of 103P/Hartley 2
Fiorangela La Forgia, Dennis Bodewits, Michael F. A'Hearn, Silvia, Protopapa, Michael S. P. Kelley, Jessica Sunshine, Lori Feaga, Tony Farnham

TL;DR
This study presents the first direct imaging of Near-UV prompt emission of OH in a comet's innermost coma, revealing localized water ice enrichment and jet structures, and suggesting a new method to trace water in comets.
Contribution
It introduces the first direct imaging of Near-UV OH prompt emission in a comet's coma, linking it to water dissociation processes and proposing a dedicated filter for water detection.
Findings
Detection of a blue enhancement indicating water ice enrichment.
Observation of a radial jet extending up to 12 km from the nucleus.
Identification of excess OH emission attributable to prompt emission from water photodissociation.
Abstract
The Deep Impact spacecraft fly-by of comet 103P/Hartley 2 occurred on 2010 November 4, one week after perihelion with a closest approach (CA) distance of about 700 km. We used narrowband images obtained by the Medium Resolution Imager (MRI) onboard the spacecraft to study the gas and dust in the innermost coma. We derived an overall dust reddening of 15\%/100 nm between 345 and 749 nm and identified a blue enhancement in the dust coma in the sunward direction within 5 km from the nucleus, which we interpret as a localized enrichment in water ice. OH column density maps show an anti-sunward enhancement throughout the encounter except for the highest resolution images, acquired at CA, where a radial jet becomes visible in the innermost coma, extending up to 12 km from the nucleus. The OH distribution in the inner coma is very different from that expected for a fragment species. Instead,…
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