The CO2 production rate has been derived in comets using Cameron-band (a3Π → X1Σ) emission of CO molecules, assuming that photodissociative excitation of CO2 is the main production mechanism of CO in the a3Π metastable state. We have developed a model for the production and loss of CO(a3Π), which has been applied to comet 103P/Hartley 2: the target of the EPOXI mission. Our model calculations show that photoelectron impact excitation of CO and dissociative excitation of CO2 can together contribute about 60-90 per cent to Cameronband emission. The modelled brightness of (0-0) Cameron-band emission on comet Hartley 2 is consistent with Hubble Space Telescope observations for 3-5 per centCO2 (depending on the model input solar flux) and 0.5 per cent CO relative to water, where the photoelectron impact contribution is about 50-75 per cent. We suggest that estimation of CO2 abundances on comets using Cameron-band emission may be reconsidered. We predict a height-integrated column brightness of the Cameron band of ~1300 Rayleigh during the EPOXI mission encounter period. © 2011 The Authors. Monthly Notices of the Royal Astronomical Society © 2011 RAS.
CITATION STYLE
Bhardwaj, A., & Raghuram, S. (2011). Model for Cameron-band emission in comets: A case for the EPOXI mission target comet 103P/Hartley 2. Monthly Notices of the Royal Astronomical Society: Letters, 412(1). https://doi.org/10.1111/j.1745-3933.2010.00998.x
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