Observations of [O I] emission in Comets C/2014 Q2 (Lovejoy) and C/2007 N3 (Lulin): Possible Influence of Solar Activity on Oxygen Line Ratios
Pith reviewed 2026-05-17 04:26 UTC · model grok-4.3
The pith
An empirical model for inferring CO2 from oxygen line ratios matches direct measurements better for a comet observed near solar maximum than near minimum.
A machine-rendered reading of the paper's core claim, the machinery that carries it, and where it could break.
Core claim
The central claim is that the accuracy of release rates used to convert oxygen line ratios into CO2 abundances depends on solar activity. Specifically, the empirical model developed from comet observations near solar maximum reproduces the directly measured CO2 abundances better for Lovejoy, observed near solar maximum; neither the empirical nor the theoretical model accurately reproduces the direct measurement for Lulin, observed near solar minimum. The authors conclude that solar-cycle phase influences the photochemistry governing [O I] release in the coma.
What carries the argument
The oxygen line ratio, formed from the intensities of the [O I] 5577 Å green line and the 6300/6364 Å red lines, converted to CO2 production rates using either empirical or theoretical release rates.
If this is right
- The oxygen line ratio method would require separate release-rate calibrations for different phases of the solar cycle to remain accurate.
- Direct space-based CO2 measurements stay necessary for validation, especially during solar minimum conditions.
- Comet composition surveys that rely on this proxy may carry systematic offsets if solar activity is ignored.
- Observers planning future ground-based [O I] studies should record and account for the prevailing solar cycle phase when choosing a model.
Where Pith is reading between the lines
- Photochemical models of the cometary coma may need to incorporate time-varying solar UV flux to predict oxygen emission rates correctly across the cycle.
- Reanalysis of existing comet spectra could apply solar-phase-specific corrections to improve past CO2 abundance estimates.
- Similar solar-cycle dependencies might appear in other remote-sensing proxies used for planetary and cometary atmospheres.
Load-bearing premise
The difference in model performance between the two comets is caused primarily by their different solar-activity levels rather than by comet-specific chemistry, viewing geometry, or other unaccounted factors.
What would settle it
Direct CO2 measurements paired with oxygen line ratio observations for one or more additional comets observed at solar maximum or minimum that either repeat or contradict the Lovejoy-versus-Lulin pattern.
Figures
read the original abstract
Observing [O I] emission to calculate an "oxygen line ratio" has been proposed as a potential proxy for direct CO$_2$ measurement in comets. However, the photochemistry governing [O I] release into the coma is not well understood, and using theoretical release rates often yields different results than using empirical release rates determined in conjunction with direct space-based measurements of CO$_2$. We hypothesize that the accuracy of the release rates could depend on the level of solar activity at the time the comet is observed, which will be influenced by the solar cycle. We present observations and analysis of [O I] emission in one comet observed near solar maximum, C/2014 Q2 (Lovejoy), and one near solar minimum, C/2007 N3 (Lulin). Our [O I] measurements were obtained using two high spectral resolution optical spectrographs: the Tull Coud\'e spectrometer at McDonald Observatory and the ARCES spectrometer at Apache Point Observatory. We use empirical and theoretical models for [O I] emission from the literature to derive multiple sets of inferred CO$_2$ abundances for these comets and compare to contemporaneous space-based measurements of CO$_2$. We find that the empirical model, which was developed based on comet observations obtained near solar maximum, reproduces the directly measured CO$_2$ abundances better for Lovejoy. Neither model accurately reproduces the direct measurement for Lulin. We discuss the implications of our findings for the accuracy and dependencies of the oxygen line ratio method for inferring CO$_2$ abundances in cometary comae.
Editorial analysis
A structured set of objections, weighed in public.
Referee Report
Summary. The paper reports high-resolution spectroscopic observations of [O I] emission in comets C/2014 Q2 (Lovejoy), observed near solar maximum, and C/2007 N3 (Lulin), observed near solar minimum. Using empirical and theoretical release-rate models from the literature, the authors derive CO2 abundances via the oxygen line ratio and compare the results to contemporaneous direct spacecraft CO2 measurements. They conclude that the empirical model (developed from observations near solar maximum) reproduces the direct CO2 values better for Lovejoy, while neither model accurately matches the direct measurement for Lulin, and discuss possible solar-activity dependence of the method.
Significance. If the result holds, the work would provide initial evidence that solar-cycle phase affects the reliability of the [O I] oxygen-line-ratio proxy for CO2, with implications for interpreting ground-based cometary spectra and for the development of activity-dependent release-rate models. The direct comparison to independent spacecraft CO2 data is a clear strength of the analysis.
major comments (2)
- [Abstract and Results] Abstract and results description: the claim of a clear performance difference between models for the two comets is presented without quantitative error bars on the inferred CO2 abundances, without reported sample sizes or integration times for the spectral data, and without explicit details on how model parameters (e.g., release rates) were applied or varied; this leaves the central comparison outcome difficult to assess quantitatively.
- [Discussion] Discussion: the attribution of the model-performance difference primarily to solar activity level is not supported by any quantitative assessment or control for confounding variables such as the comets' differing heliocentric distances at observation, intrinsic CO2/H2O ratios, outgassing patterns, or slit-filling factors in the high-resolution spectra. With only two comets, the data cannot isolate solar UV flux as the driver.
minor comments (2)
- [Observations] Clarify the precise rest wavelengths adopted for the [O I] lines and any telluric or continuum subtraction procedures applied to the Tull Coudé and ARCES spectra.
- [Figures/Tables] Add error bars to any tabulated or plotted comparisons of model-derived versus spacecraft CO2 abundances.
Simulated Author's Rebuttal
We thank the referee for their constructive comments, which highlight areas where the manuscript can be clarified and strengthened. We respond to each major comment below.
read point-by-point responses
-
Referee: [Abstract and Results] Abstract and results description: the claim of a clear performance difference between models for the two comets is presented without quantitative error bars on the inferred CO2 abundances, without reported sample sizes or integration times for the spectral data, and without explicit details on how model parameters (e.g., release rates) were applied or varied; this leaves the central comparison outcome difficult to assess quantitatively.
Authors: We agree that the results section and abstract would benefit from greater quantitative detail to allow readers to assess the comparisons more rigorously. In the revised manuscript we will add error bars to all reported CO2 abundances derived from the oxygen line ratios. We will also report the number of individual spectra and total integration times used for each comet. In addition, we will expand the methods description to specify the exact release-rate values adopted from the literature for both the empirical and theoretical models and to clarify how these rates were applied to the observed line fluxes. revision: yes
-
Referee: [Discussion] Discussion: the attribution of the model-performance difference primarily to solar activity level is not supported by any quantitative assessment or control for confounding variables such as the comets' differing heliocentric distances at observation, intrinsic CO2/H2O ratios, outgassing patterns, or slit-filling factors in the high-resolution spectra. With only two comets, the data cannot isolate solar UV flux as the driver.
Authors: We accept that observations of only two comets cannot fully isolate solar activity from other variables. In the revised discussion we will add explicit quantitative information on the heliocentric distances at the epochs of observation, compare the spacecraft-measured CO2/H2O ratios for the two comets, and discuss possible effects of outgassing patterns and slit-filling factors. We will also qualify the interpretation by stating that the present results are suggestive of a solar-cycle dependence and that a larger sample is required to confirm the role of solar UV flux. These additions will make the limitations of the current dataset transparent while preserving the value of the direct spacecraft comparison. revision: yes
Circularity Check
No circularity; analysis rests on direct comparison to independent spacecraft CO2 data
full rationale
The paper presents spectroscopic observations of two comets and derives CO2 abundances using empirical and theoretical [O I] release-rate models taken from the literature. These inferred abundances are then compared to contemporaneous direct spacecraft measurements of CO2. No equations or steps reduce a fitted quantity to a prediction by construction, no self-citation chain is invoked to justify a uniqueness claim, and the central result is an empirical performance difference evaluated against external benchmarks rather than an internal re-derivation of the input models themselves. The derivation chain is therefore self-contained.
Axiom & Free-Parameter Ledger
axioms (1)
- domain assumption Literature empirical and theoretical [O I] release rates remain valid when applied to the observed comets.
Reference graph
Works this paper leans on
-
[1]
Astropy Collaboration, Robitaille, T. P., Tollerud, E. J., et al. 2013, Astropy: A community Python package for astronomy, A&A, 558, A33, doi: 10.1051/0004-6361/201322068 Astropy Collaboration, Price-Whelan, A. M., Sip˝ocz, B. M., et al. 2018, The Astropy Project: Building an Open-science Project and Status of the v2.0 Core Package, AJ, 156, 123, doi: 10....
- [2]
-
[3]
Morphology, Numerical Modeling, and Production Rates for Comet C/Lulin (2007 N3), The Astronomical Journal, 156, 159, doi: 10.3847/1538-3881/aad549
-
[4]
Bhardwaj, A., & Raghuram, S. 2012, A COUPLED CHEMISTRY-EMISSION MODEL FOR ATOMIC OXYGEN GREEN AND RED-DOUBLET EMISSIONS IN THE COMET C/1996 B2 HY AKUTAKE, The Astrophysical Journal, 748, 13, doi: 10.1088/0004-637x/748/1/13
-
[5]
Biver, N., Bockelée-Morvan, D., Moreno, R., et al. 2015, Ethyl alcohol and sugar in comet C/2014 Q2 (Lovejoy), Science Advances, 1, doi: 10.1126/sciadv.1500863
-
[6]
Biver, N., Moreno, R., Bockelée-Morvan, D., et al. 2016, Isotopic ratios of H, C, N, O, and S in comets C/2012 F6 (Lemmon) and C/2014 Q2 (Lovejoy), Astronomy & Astrophysics, 589, A78, doi: 10.1051/0004-6361/201528041
-
[7]
1989, The nature of the 2.8-micron emission feature in cometary spectra, A&A, 216, 278
Bockelee-Morvan, D., & Crovisier, J. 1989, The nature of the 2.8-micron emission feature in cometary spectra, A&A, 216, 278
work page 1989
-
[8]
Bodewits, D., Villanueva, G. L., Mumma, M. J., et al. 2010, SWIFT-UVOT GRISM SPECTROSCOPY OF COMETS: A FIRST APPLICATION TO C/2007 N3 (LULIN), The Astronomical Journal, 141, 12, doi: 10.1088/0004-6256/141/1/12
-
[9]
Budzien, S. A., Festou, M. C., & Feldman, P. D. 1994, Solar Flux Variability and the Lifetimes of Cometary H 2O and OH, Icarus, 107, 164, doi: 10.1006/icar.1994.1014
-
[10]
Cochran, A. 2001, Observations of O (1S) and O (1D) in Spectra of C/1999 S4 (LINEAR), Icarus, 154, 381, doi: 10.1006/icar.2001.6718
-
[11]
Cochran, A. L. 2008, Atomic oxygen in the comae of comets, Icarus, 198, 181, doi: 10.1016/j.icarus.2008.06.007
-
[12]
Cochran, A. L., & Schleicher, D. G. 1993, Observational Constraints on the Lifetime of Cometary H 2O, Icarus, 105, 235, doi: 10.1006/icar.1993.1121
-
[13]
Combi, M., Mäkinen, T., Bertaux, J.-L., et al. 2018, Water production activity of nine long-period comets from SOHO/SW AN observations of hydrogen Lyman-alpha: 2013–2016, Icarus, 300, 33–46, doi: 10.1016/j.icarus.2017.08.035
-
[14]
Ferron, S. 2019, A survey of water production in 61 comets from SOHO/SW AN observations of hydrogen Lyman-alpha: Twenty-one years 1996-2016, Icarus, 317, 610, doi: 10.1016/j.icarus.2018.08.031
-
[15]
Debout, V ., Bockelée-Morvan, D., & Zakharov, V . 2016, A radiative transfer model to treat infrared molecular excitation in cometary atmospheres, Icarus, 265, 110, doi: 10.1016/j.icarus.2015.10.013
-
[16]
Decock, A., Jehin, E., Hutsemékers, D., & Manfroid, J. 2013, Forbidden oxygen lines in comets at various heliocentric distances, Astronomy & Astrophysics, 555, A34, doi: 10.1051/0004-6361/201220414
-
[17]
Decock, A., Jehin, E., Rousselot, P., et al. 2014, Forbidden oxygen lines at various nucleocentric distances in comets, Astronomy & Astrophysics, 573, A1, doi: 10.1051/0004-6361/201424403 Dello Russo, N., Vervack, R. J., Kawakita, H., et al. 2022, V olatile
-
[18]
Abundances, Extended Coma Sources, and Nucleus Ice Associations in Comet C/2014 Q2 (Lovejoy), The Planetary Science Journal, 3, 6, doi: 10.3847/psj/ac323c
-
[19]
Delsemme, A. 1980, Photodissociation of CO2 into CO + O(1D), The spectra of simple molecules in the laboratory and in astrophysics. articles.adsabs.harvard.edu/pdf/1980LIACo..21..515D
work page 1980
-
[20]
Faggi, S., Villanueva, G. L., Mumma, M. J., et al. 2016, DETAILED ANALYSIS OF NEAR-IR W ATER (H2O) EMISSION IN COMET C/2014 Q2 (LOVEJOY) WITH THE GIANO/TNG SPECTROGRAPH, The Astrophysical Journal, 830, 157, doi: 10.3847/0004-637x/830/2/157
-
[21]
Fazio, G. G., Hora, J. L., Allen, L. E., et al. 2004, The Infrared Array Camera (IRAC) for the Spitzer Space Telescope, ApJS, 154, 10, doi: 10.1086/422843 16
-
[22]
Russo, N. D. 2018, Far-ultraviolet Spectroscopy of Recent Comets with the Cosmic Origins Spectrograph on the Hubble Space Telescope, The Astronomical Journal, 155, 193, doi: 10.3847/1538-3881/aab78a
-
[23]
Festou, M. C., & Feldman, P. D. 1981, The Forbidden Oxygen Lines in Comets, Astronomy and Astrophysics. https://articles.adsabs.harvard.edu/pdf/1981A%26A...103..154F
work page 1981
-
[24]
Fink, U. 2009, A taxonomic survey of comet composition 1985-2004 using CCD spectroscopy, Icarus, 201, 311, doi: 10.1016/j.icarus.2008.12.044
-
[25]
Gibb, E. L., Bonev, B. P., Villanueva, G., et al. 2012, CHEMICAL COMPOSITION OF COMET C/2007 N3 (LULIN): ANOTHER ‘“ATYPICAL”’ COMET, The Astrophysical Journal, 750, 102, doi: 10.1088/0004-637x/750/2/102
-
[26]
Ginsburg, A., Sokolov, V ., de Val-Borro, M., et al. 2022, Pyspeckit: A Spectroscopic Analysis and Plotting Package, The Astronomical Journal, 163, 291, doi: 10.3847/1538-3881/ac695a
-
[27]
2021, in AAS/Division for Planetary Sciences Meeting Abstracts, V ol
Hall, K., McKay, A., Kelley, M., et al. 2021, in AAS/Division for Planetary Sciences Meeting Abstracts, V ol. 53, AAS/Division for Planetary Sciences Meeting Abstracts #53, 210.07
work page 2021
-
[28]
Haser, L. 1957, Distribution d’intensité dans la tête d’une comète, Bulletins de l’Académie Royale de Belgique, 43, 740
work page 1957
-
[29]
Huebner, W. F., Keady, J. J., & Lyon, S. P. 1992, Solar photo rates for planetary atmospheres and atmospheric pollutants, Astrophysics and Space Science, 195, 1–294, doi: 10.1007/bf00644558 IRSA. 2022, Spitzer Heritage Archive (SHA), IPAC, doi: 10.26131/IRSA543
-
[30]
Kelley, M. S., Bodewits, D., Feaga, L. M., et al. 2017, in AAS/Division for Planetary Sciences Meeting Abstracts, V ol. 49, AAS/Division for Planetary Sciences Meeting Abstracts #49, 414.15 Laboratory for Atmospheric and Space Physics. 2005, LASP Interactive Solar Irradiance Datacenter, Laboratory for Atmospheric and Space Physics, doi: 10.25980/L27Z-XD34
-
[31]
2010, IRAC Instrument Handbook (Pasadena: Spitzer Science Center)
Laine, S., ed. 2010, IRAC Instrument Handbook (Pasadena: Spitzer Science Center). http://ssc.spitzer.caltech.edu/irac/iracinstrumenthandbook/
work page 2010
-
[32]
2005, in Astronomical Society of the Pacific Conference Series, V ol
Makovoz, D., & Khan, I. 2005, in Astronomical Society of the Pacific Conference Series, V ol. 347, Astronomical Data Analysis Software and Systems XIV , ed. P. Shopbell, M. Britton, & R. Ebert, 81
work page 2005
-
[33]
2020, in AAS/Division for Planetary Sciences Meeting
McKay, A., Kelley, M., Cochran, A., DiSanti, M., & Bauer, J. 2020, in AAS/Division for Planetary Sciences Meeting
work page 2020
-
[34]
McKay, A. J., Chanover, N. J., DiSanti, M. A., et al. 2014, Rotational variation of daughter species production rates in Comet 103P/Hartley: Implications for the progeny of daughter species and the degree of chemical heterogeneity, Icarus, 231, 193, doi: 10.1016/j.icarus.2013.11.029
-
[35]
McKay, A. J., Chanover, N. J., Morgenthaler, J. P., et al. 2012, Forbidden oxygen lines in Comets C/2006 W3 Christensen and C/2007 Q3 Siding Spring at large heliocentric distance: Implications for the sublimation of volatile ices, Icarus, 220, 277, doi: 10.1016/j.icarus.2012.04.030
-
[36]
McKay, A. J., Chanover, N. J., Morgenthaler, J. P., et al. 2013, Observations of the forbidden oxygen lines in DIXI target Comet 103P/Hartley, Icarus, 222, 684, doi: 10.1016/j.icarus.2012.06.020
-
[37]
McKay, A. J., Cochran, A. L., DiSanti, M. A., et al. 2018, Evolution of H2O production in comet C/2012 S1 (ISON) as inferred from forbidden oxygen and OH emission, Icarus, 309, 1, doi: 10.1016/j.icarus.2018.02.024
-
[38]
McKay, A. J., Kelley, M. S., Cochran, A. L., et al. 2016, The CO 2 abundance in Comets C/2012 K1 (PanSTARRS), C/2012 K5 (LINEAR), and 290P/Jäger as measured with Spitzer, Icarus, 266, 249, doi: 10.1016/j.icarus.2015.11.004
-
[39]
McKay, A. J., Cochran, A. L., DiSanti, M. A., et al. 2015, Evolution of H2O, CO, and CO2 production in Comet C/2009 P1 Garradd during the 2011–2012 apparition, Icarus, 250, 504, doi: 10.1016/j.icarus.2014.12.023
-
[40]
McKay, A. J., DiSanti, M. A., Cochran, A. L., et al. 2021, Quantifying the Hypervolatile Abundances in Jupiter-family Comet 46P/Wirtanen, PSJ, 2, 21, doi: 10.3847/PSJ/abd71d
-
[41]
Meech, K., & Svoren, J. 2004, Using cometary activity to trace the physical and chemical evolution of cometary nuclei, Comets II
work page 2004
-
[42]
Mommert, M., Kelley, M., de Val-Borro, M., et al. 2019, sbpy: A Python module for small-body planetary astronomy, The Journal of Open Source Software, 4, 1426, doi: 10.21105/joss.01426
-
[43]
Morgenthaler, J. P., Harris, W. M., & Combi, M. R. 2007, Large Aperture O I 6300 Å Observations of Comet Hyakutake: Implications for the Photochemistry of OH and O I Production in Comet Hale-Bopp, ApJ, 657, 1162, doi: 10.1086/511062
-
[44]
Morgenthaler, J. P., Harris, W. M., Scherb, F., et al. 2001, Large-Aperture [O I] 6300 Å Photometry of Comet Hale-Bopp: Implications for the Photochemistry of OH, ApJ, 563, 451, doi: 10.1086/323773
-
[45]
2021, in AAS/Division for Planetary Sciences Meeting Abstracts, V ol
Nelson, T., & Cochran, A. 2021, in AAS/Division for Planetary Sciences Meeting Abstracts, V ol. 53, AAS/Division for Planetary Sciences Meeting Abstracts #53, 102.03
work page 2021
-
[46]
Ootsubo, T., Usui, F., Kawakita, H., et al. 2010, DETECTION OF PARENT H2O AND CO2MOLECULES IN THE 2.5–5µm SPECTRUM OF COMET C/2007 N3 (LULIN) OBSERVED
work page 2010
-
[47]
WITHAKARI, The Astrophysical Journal, 717, L66–L70, doi: 10.1088/2041-8205/717/1/l66 17
-
[48]
Ootsubo, T., Kawakita, H., Hamada, S., et al. 2012, AKARI NEAR-INFRARED SPECTROSCOPIC SURVEY FOR CO2IN 18 COMETS, The Astrophysical Journal, 752, 15, doi: 10.1088/0004-637x/752/1/15
-
[49]
Paganini, L., Mumma, M. J., Gibb, E. L., & Villanueva, G. L. 2017, Ground-based Detection of Deuterated Water in Comet C/2014 Q2 (Lovejoy) at IR Wavelengths, The Astrophysical Journal Letters, 836, L25, doi: 10.3847/2041-8213/aa5cb3
-
[50]
Raghuram, S., & Bhardwaj, A. 2014, Photochemistry of atomic oxygen green and red-doublet emissions in comets at larger heliocentric distances, Astronomy & Astrophysics, 566, A134, doi: 10.1051/0004-6361/201321921
-
[51]
Raghuram, S., Hutsemékers, D., Opitom, C., et al. 2020, Forbidden atomic carbon, nitrogen, and oxygen emission lines in the water-poor comet C/2016 R2 (Pan-STARRS), Astronomy & Astrophysics, 635, A108, doi: 10.1051/0004-6361/201936713
-
[52]
Reach, W. T., Kelley, M. S., & Vaubaillon, J. 2013, Survey of cometary CO2, CO, and particulate emissions using the Spitzer Space Telescope, Icarus, 226, 777, doi: 10.1016/j.icarus.2013.06.011
-
[53]
Reach, W. T., Megeath, S. T., Cohen, M., et al. 2005, Absolute Calibration of the Infrared Array Camera on the Spitzer Space
work page 2005
-
[54]
Telescope, PASP, 117, 978, doi: 10.1086/432670
-
[55]
Sharpee, B. D., & Slanger, T. G. 2006, O(1D2 −3 P2,1,0) 630.0, 636.4, and 639.2 nm Forbidden Emission Line Intensity Ratios Measured in the Terrestrial Nightglow, The Journal of Physical Chemistry A, 110, 6707, doi: 10.1021/jp056163x
-
[56]
Slanger, T. G., Sharpee, B. D., Pejakovi´c, D. A., et al. 2011, Atomic oxygen emission intensity ratio: Observation and theory,
work page 2011
-
[57]
Eos, Transactions American Geophysical Union, 92, 291, doi: 10.1029/2011eo350005
-
[58]
Storey, P. J., & Zeippen, C. J. 2000, Theoretical values for the [OIII] 5007/4959 line-intensity ratio and homologous cases, Monthly Notices of the Royal Astronomical Society, 312, 813, doi: 10.1046/j.1365-8711.2000.03184.x
-
[59]
Tull, R. G., MacQueen, P. J., Sneden, C., & Lambert, D. L. 1995, The High-Resolution Cross-Dispersed Echelle White Pupil Spectrometer of the McDonald Observatory 2.7-m Telescope, PASP, 107, 251, doi: 10.1086/133548
-
[60]
Virtanen, P., Gommers, R., Oliphant, T. E., et al. 2020, SciPy 1.0: fundamental algorithms for scientific computing in Python, Nature Medicine, 17, 261, doi: 10.1038/s41592-019-0686-2
-
[61]
Wang, S.-i., Hildebrand, R. H., Hobbs, L. M., et al. 2003, in Instrument Design and Performance for Optical/Infrared Ground-based Telescopes, ed. M. Iye & A. F. M. Moorwood (SPIE), doi: 10.1117/12.461447
-
[62]
Werner, M. W., Roellig, T. L., Low, F. J., et al. 2004, The Spitzer Space Telescope Mission, ApJS, 154, 1, doi: 10.1086/422992
discussion (0)
Sign in with ORCID, Apple, or X to comment. Anyone can read and Pith papers without signing in.