Coupled Chemistry-Emission Model for Atomic Oxygen Green and Red-doublet Emissions in Comet C/1996 B2 Hyakutake
Anil Bhardwaj, Susarla Raghuram

TL;DR
This study develops a coupled chemistry-emission model to analyze the production of atomic oxygen green and red-doublet emissions in comet Hyakutake, revealing the contributions of different parent molecules and the dependence on observational parameters.
Contribution
The paper introduces a comprehensive model that accounts for photochemistry and observational geometry to better understand oxygen emission lines in cometary comae.
Findings
H2O photodissociation contributes 30-70% to green and 60-90% to red emissions.
CO2 and CO contribute 25-50% to green and less than 5% to red emissions.
The O(1S) yield from H2O photodissociation is less than 1%.
Abstract
The green (5577 \AA) and red-doublet (6300, 6364 \AA) lines are prompt emissions of metastable oxygen atoms in the S and D states, respectively, that have been observed in several comets. The value of intensity ratio of green to red-doublet (G/R ratio) of 0.1 has been used as a benchmark to identify the parent molecule of oxygen lines as HO. A coupled chemistry-emission model is developed to study the production and loss mechanisms of O(S) and O(D) atoms and the generation of red and green lines in the coma of C/1996 B2 Hyakutake. The G/R ratio depends not only on photochemistry, but also on the projected area observed for cometary coma, which is a function of the dimension of the slit used and geocentric distance of the comet. Calculations show that the contribution of photodissociation of HO to the green (red) line emission is 30 to 70% (60 to 90%), while…
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