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arxiv: 2606.22267 · v1 · pith:GDBL4O2Anew · submitted 2026-06-20 · 🌌 astro-ph.IM · astro-ph.EP· physics.optics

Reassessment of ammonia self- and air-broadened half-widths in the HITRAN database

Pith reviewed 2026-06-26 11:04 UTC · model grok-4.3

classification 🌌 astro-ph.IM astro-ph.EPphysics.optics
keywords ammoniaNH3HITRANpressure broadeninghalf-widthsLorentz widthspectroscopic databaserotational dependence
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The pith

Compiled NH3 measurements yield new polynomial correlations that cut HITRAN broadening errors from 11-24% down to 7-11%.

A machine-rendered reading of the paper's core claim, the machinery that carries it, and where it could break.

The paper compiles 1317 self-broadened and 1231 air-broadened NH3 half-width measurements at 296 K across multiple bands to create updated empirical correlations. Current HITRAN values rely on older rotational correlations that clamp or assign defaults beyond measured ranges, limiting accuracy especially at high rotational states. New weighted, positivity-constrained third-degree polynomials in the branch-dependent index m and K'' reduce mean absolute percentage errors to 6.80% for air broadening and 10.89% for self broadening. Validation against independent PNNL and pure-NH3 spectra confirms improved absorption simulations. Accurate broadening parameters support reliable line-by-line modeling in atmospheric sensing, combustion diagnostics, and planetary atmosphere studies.

Core claim

Published NH3 self- and air-broadened Lorentz half-widths were compiled and reassessed to develop updated HITRAN-ready empirical correlations. The analysis shows that linewidths are governed mainly by rotational dependence rather than branch, band, or vibration-inversion effects. Weighted, positivity-constrained third-degree polynomial fits were developed for gamma_self and gamma_air as functions of the branch-dependent index m and K''. The new correlations reduce the MAPE from 10.95% to 6.80% for air broadening and from 23.61% to 10.89% for self broadening relative to HITRAN2024, providing a physically constrained replacement for the current HITRAN NH3 broadening treatment.

What carries the argument

Weighted, positivity-constrained third-degree polynomial fits for gamma_self and gamma_air as functions of the branch-dependent index m and K''.

If this is right

  • Line-by-line radiative transfer calculations for NH3 will match measured spectra more closely across wider rotational ranges.
  • High-J'' states will use physically constrained values instead of database clamps or defaults.
  • Atmospheric sensing and combustion diagnostics gain improved accuracy in simulated absorption.
  • Planetary and exoplanet atmosphere models benefit from more reliable NH3 line parameters.
  • The correlations serve as a direct, ready-to-implement replacement for existing HITRAN NH3 broadening data.

Where Pith is reading between the lines

These are editorial extensions of the paper, not claims the author makes directly.

  • The same compilation-and-polynomial method could be tested on other molecules where rotational trends dominate broadening.
  • Extending the fits to additional temperatures would test whether separate temperature exponents suffice or if new terms are required.
  • Direct comparison of the fitted trends against quantum scattering calculations could reveal the underlying collision physics.

Load-bearing premise

The third-degree polynomial form in the branch-dependent index m and K'' is adequate to describe the rotational dependence across all bands and branches without systematic biases in the compiled dataset.

What would settle it

A new high-precision measurement of NH3 self- or air-broadened half-widths at high J'' values that deviates substantially from the third-degree polynomial predictions would falsify the correlations.

read the original abstract

Accurate NH3 pressure-broadening parameters are essential for reliable line-by-line simulations in atmospheric sensing, combustion diagnostics, and planetary/exoplanet studies. Current HITRAN NH3 self- and air-broadened half-widths rely largely on the Nemtchinov rotational correlation and database rules that clamp or assign default values beyond the validated range, limiting the representation of measured rotational trends, especially at high J''. Here, published NH3 self- and air-broadened Lorentz half-widths were compiled and reassessed to develop updated HITRAN-ready empirical correlations. The dataset includes 1317 self-broadened and 1231 air-broadened widths at, or reduced to, 296 K across multiple bands, branches, and rotational states. The analysis shows that linewidths are governed mainly by rotational dependence rather than branch, band, or vibration-inversion effects. Weighted, positivity-constrained third-degree polynomial fits were developed for gamma_self and gamma_air as functions of the branch-dependent index m and K''. The new correlations reduce the MAPE from 10.95% to 6.80% for air broadening and from 23.61% to 10.89% for self broadening relative to HITRAN2024. Comparisons with PNNL and pure-NH3 spectra further confirm improved absorption simulations, providing a physically constrained replacement for the current HITRAN NH3 broadening treatment.

Editorial analysis

A structured set of objections, weighed in public.

Desk editor's note, referee report, simulated authors' rebuttal, and a circularity audit. Tearing a paper down is the easy half of reading it; the pith above is the substance, this is the friction.

Referee Report

3 major / 2 minor

Summary. The manuscript compiles 1317 self-broadened and 1231 air-broadened NH3 Lorentz half-widths at 296 K from the literature. It concludes that rotational dependence dominates over branch, band, and vibration-inversion effects, then derives weighted positivity-constrained third-degree polynomial correlations for gamma_self(m, K'') and gamma_air(m, K'') as a replacement for the Nemtchinov-based rules and clamping in HITRAN2024. The new fits reduce MAPE from 10.95% to 6.80% (air) and 23.61% to 10.89% (self) on the compiled data, with supporting comparisons to PNNL and pure-NH3 spectra.

Significance. If the polynomial form proves adequate across the full rotational range, the work supplies an improved, physically constrained set of empirical broadening parameters for the HITRAN database that is directly relevant to atmospheric remote sensing and exoplanet spectroscopy. The scale of the compiled dataset and the inclusion of independent spectral validation are clear strengths; the positivity constraint is also a positive methodological choice.

major comments (3)
  1. [§4] §4 (polynomial fits): the third-degree form in branch-dependent m and K'' is asserted to capture the dominant rotational dependence, yet no residual plots versus |m| (especially for |m| > 15 where high-J'' data exist) or comparison against quartic fits are shown. Without this, it is unclear whether the reported MAPE reductions are robust or whether the cubic underfits at the edges of the domain, undermining the claim that the correlations reliably replace HITRAN rules.
  2. [§2] §2 (dataset): the selection and quality-weighting criteria applied to arrive at the final 1317 self and 1231 air widths are not stated with sufficient detail to evaluate possible systematic biases inherited from the original measurements. This directly affects the reliability of the fitted coefficients and the MAPE comparison to HITRAN2024.
  3. [§5] §5 (spectral validation): the PNNL and pure-NH3 comparisons are cited as confirming improved absorption simulations, but the specific bands, pressure ranges, and quantitative metrics (e.g., integrated residual or line-by-line RMS) used in those tests are not reported, limiting the strength of the non-circular validation.
minor comments (2)
  1. [Introduction] The definition of the branch-dependent index m should be stated explicitly (with the conventional sign convention for P, Q, R branches) at first use rather than assumed known.
  2. [Results] Table 1 (or equivalent summary table of fit coefficients) should include the number of data points per branch and the reduced chi-squared of each fit to allow readers to judge over- or under-fitting.

Simulated Author's Rebuttal

3 responses · 0 unresolved

We thank the referee for the constructive comments, which help clarify the presentation of our dataset, fitting methodology, and validation. We address each major point below and will revise the manuscript accordingly to strengthen the justification for the proposed correlations.

read point-by-point responses
  1. Referee: [§4] §4 (polynomial fits): the third-degree form in branch-dependent m and K'' is asserted to capture the dominant rotational dependence, yet no residual plots versus |m| (especially for |m| > 15 where high-J'' data exist) or comparison against quartic fits are shown. Without this, it is unclear whether the reported MAPE reductions are robust or whether the cubic underfits at the edges of the domain, undermining the claim that the correlations reliably replace HITRAN rules.

    Authors: We agree that explicit residual analysis versus |m| (including the high-J regime) and a direct comparison to quartic polynomials would better demonstrate that the cubic form is adequate. In the revised manuscript we will add (i) residual plots of the cubic fits versus |m| for both self- and air-broadening, highlighting the |m| > 15 region, and (ii) a short quantitative comparison (MAPE and reduced-χ²) showing that quartic terms yield only marginal improvement while risking unphysical oscillations or negativity at the domain edges. The positivity constraint and the physical expectation that broadening varies smoothly with rotational quantum numbers continue to favor the cubic representation. revision: yes

  2. Referee: [§2] §2 (dataset): the selection and quality-weighting criteria applied to arrive at the final 1317 self and 1231 air widths are not stated with sufficient detail to evaluate possible systematic biases inherited from the original measurements. This directly affects the reliability of the fitted coefficients and the MAPE comparison to HITRAN2024.

    Authors: We acknowledge that the current description of data curation is insufficiently detailed. The revised §2 will explicitly list the inclusion criteria (measurement technique, reported uncertainty threshold, temperature range for reduction to 296 K, and rejection of duplicate or inconsistent entries) together with the precise weighting scheme (inverse-variance weighting augmented by a quality factor based on experimental method) used both for the polynomial fits and for the MAPE statistics. This will allow readers to assess potential systematic biases. revision: yes

  3. Referee: [§5] §5 (spectral validation): the PNNL and pure-NH3 comparisons are cited as confirming improved absorption simulations, but the specific bands, pressure ranges, and quantitative metrics (e.g., integrated residual or line-by-line RMS) used in those tests are not reported, limiting the strength of the non-circular validation.

    Authors: We will expand the validation section to report the exact spectral bands examined, the pressure ranges covered in the PNNL and pure-NH3 measurements, and the quantitative metrics (line-by-line RMS residuals and integrated absolute residuals) obtained with both the new correlations and the current HITRAN2024 parameters. These additions will make the independent validation fully reproducible and strengthen the claim of improved performance. revision: yes

Circularity Check

1 steps flagged

MAPE reductions are in-sample fit quality on the compiled dataset

specific steps
  1. fitted input called prediction [Abstract]
    "The new correlations reduce the MAPE from 10.95% to 6.80% for air broadening and from 23.61% to 10.89% for self broadening relative to HITRAN2024."

    The correlations are obtained by fitting the polynomials to the compiled widths; the quoted MAPE values therefore quantify how closely the fitted functions reproduce the same measurements they were trained on, rather than demonstrating predictive performance on held-out data.

full rationale

The paper compiles 1317 self and 1231 air widths, fits weighted positivity-constrained third-degree polynomials in branch-dependent m and K'', then reports that these correlations reduce MAPE relative to HITRAN2024. Because the MAPE figures are computed on the identical data used to determine the coefficients, the reported improvement is a direct measure of in-sample fit error rather than an independent test. The abstract also cites comparisons to PNNL and pure-NH3 spectra as further confirmation, supplying limited non-circular support, which keeps the overall circularity moderate rather than total.

Axiom & Free-Parameter Ledger

2 free parameters · 1 axioms · 0 invented entities

The central claim depends on the compiled measurements being accurate and representative, and on the chosen polynomial degree and variables being sufficient without additional terms.

free parameters (2)
  • third-degree polynomial coefficients for gamma_self(m, K'')
    Determined by weighted positivity-constrained fits to the 1317 self-broadened widths.
  • third-degree polynomial coefficients for gamma_air(m, K'')
    Determined by weighted positivity-constrained fits to the 1231 air-broadened widths.
axioms (1)
  • domain assumption NH3 linewidths are governed mainly by rotational dependence (via m and K'') rather than branch, band, or vibration-inversion effects.
    This is presented as a finding from the analysis of the compiled dataset.

pith-pipeline@v0.9.1-grok · 5793 in / 1401 out tokens · 46442 ms · 2026-06-26T11:04:13.910712+00:00 · methodology

discussion (0)

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Reference graph

Works this paper leans on

52 extracted references · 50 canonical work pages

  1. [2]

    Changes in ammonia and its effects on PM2.5 chemical property in three winter seasons in Beijing, China

    Meng Z, Wu L, Xu X, Xu W, Zhang R, Jia X, et al. Changes in ammonia and its effects on PM2.5 chemical property in three winter seasons in Beijing, China. Science of The Total Environment 2020;749:142208. https://doi.org/10.1016/J.SCITOTENV.2020.142208

  2. [3]

    Estimation of global NH3 volatilization loss from synthetic fertilizers and animal manure applied to arable lands and grasslands

    Bouwman AF, Boumans LJM, Batjes NH. Estimation of global NH3 volatilization loss from synthetic fertilizers and animal manure applied to arable lands and grasslands. Global Biogeochem Cycles 2002;16:8–1. https://doi.org/10.1029/2000GB001389;JOURNAL:JOURNAL:19449224;PAGE:STRING:ARTICLE/CHAP TER

  3. [4]

    Ammonia and Nitric Acid Demands for Fertilizer Use in 2050

    Lim J, Fernández CA, Lee SW, Hatzell MC. Ammonia and Nitric Acid Demands for Fertilizer Use in 2050. ACS Energy Lett 2021;6:3676–85. https://doi.org/10.1021/ACSENERGYLETT.1C01614

  4. [5]

    Projections of NH3 emissions from manure generated by livestock production in China to 2030 under six mitigation scenarios

    Xu P, Koloutsou -Vakakis S, Rood MJ, Luan S. Projections of NH3 emissions from manure generated by livestock production in China to 2030 under six mitigation scenarios. Science of The Total Environment 2017;607–608:78–86. https://doi.org/10.1016/J.SCITOTENV.2017.06.258

  5. [6]

    Emissions of NH3, CO2 and H2S during swine wastewater management: Characterization of transient emissions after air -liquid interface disturbances

    Blanes-Vidal V, Guàrdia M, Dai XR, Nadimi ES. Emissions of NH3, CO2 and H2S during swine wastewater management: Characterization of transient emissions after air -liquid interface disturbances. Atmos Environ 2012;54:408–18. https://doi.org/10.1016/J.ATMOSENV.2012.02.046

  6. [7]

    Global emissions of NH3, NOx, and N2O from biomass burning and the impact of climate change

    Bray CD, Battye WH, Aneja VP, Schlesinger WH. Global emissions of NH3, NOx, and N2O from biomass burning and the impact of climate change. J Air Waste Manage Assoc 2021;71:102 –14. https://doi.org/10.1080/10962247.2020.1842822

  7. [8]

    Urban NH3 levels and sources in six major Spanish cities

    Reche C, Viana M, Karanasiou A, Cusack M, Alastuey A, Artiñano B, et al. Urban NH3 levels and sources in six major Spanish cities. Chemosphere 2015;119:769 –77. https://doi.org/10.1016/J.CHEMOSPHERE.2014.07.097

  8. [9]

    Ammonia in the atmosphere: A review on emission sources, atmospheric chemistry and deposition on terrestrial bodies

    Behera SN, Sharma M, Aneja VP, Balasubramanian R. Ammonia in the atmosphere: A review on emission sources, atmospheric chemistry and deposition on terrestrial bodies. Environmental Science and Pollution Research 2013;20:8092–131. https://doi.org/10.1007/S11356-013-2051-9/TABLES/16

  9. [10]

    , year = 2013, month = nov, volume = 130, pages =

    Rothman LS, Gordon IE, Babikov Y, Barbe A, Chris Benner D, Bernath PF, et al. The HITRAN2012 molecular spectroscopic database. J Quant Spectrosc Radiat Transf 2013;130:4 –50. https://doi.org/10.1016/j.jqsrt.2013.07.002

  10. [11]

    Fast responsive, optical trace level ammonia sensor for environmental monitoring

    Abel T, Ungerböck B, Klimant I, Mayr T. Fast responsive, optical trace level ammonia sensor for environmental monitoring. Chemistry Central Journal 2012 6:1 2012;6:124 -. https://doi.org/10.1186/1752 - 153X-6-124

  11. [12]

    Ammonia sensors and their applications —a review

    Timmer B, Olthuis W, Van Den Berg A. Ammonia sensors and their applications —a review. Sens Actuators B Chem 2005;107:666–77. https://doi.org/10.1016/J.SNB.2004.11.054

  12. [13]

    A calibration-free ammonia breath sensor using a quantum cascade laser with WMS 2f/1f

    Owen K, Farooq A. A calibration-free ammonia breath sensor using a quantum cascade laser with WMS 2f/1f. Applied Physics B 2013 116:2 2013;116:371–83. https://doi.org/10.1007/S00340-013-5701-1

  13. [14]

    Field-Deployable Ammonia Sensor for Assessment of Wastewater Feedstocks and Their Utilization for Ammonia Synthesis

    Goyal I, Gande VV, Savitha R, Singh MR. Field-Deployable Ammonia Sensor for Assessment of Wastewater Feedstocks and Their Utilization for Ammonia Synthesis. Advanced Sensor Research 2025;4:e00095. https://doi.org/10.1002/ADSR.202500095;JOURNAL:JOURNAL:27511219;WGROUP:STRING:PUBLICA TION

  14. [15]

    Interaction chemistry of ammonia and formaldehyde: Multi -species measurements and kinetic modeling

    Zou J, Adil M, Elkhazraji A, Farooq A. Interaction chemistry of ammonia and formaldehyde: Multi -species measurements and kinetic modeling. Proceedings of the Combustion Institute 2024;40. https://doi.org/https://doi.org/10.1016/J.PROCI.2024.105424. 42

  15. [16]

    Interaction of ammonia with nitric oxide and nitrous oxide: Multi - species time-history measurements and comprehensive kinetic modeling

    Zou J, Adil M, Elkhazraji A, Farooq A. Interaction of ammonia with nitric oxide and nitrous oxide: Multi - species time-history measurements and comprehensive kinetic modeling. Combust Flame 2025;276:114135. https://doi.org/10.1016/J.COMBUSTFLAME.2025.114135

  16. [17]

    A shock -tube study of NH3 and NH3/H2 oxidation using laser absorption of NH3 and H2O

    Alturaifi SA, Mathieu O, Petersen EL. A shock -tube study of NH3 and NH3/H2 oxidation using laser absorption of NH3 and H2O. Proceedings of the Combustion Institute 2023;39:233 –41. https://doi.org/10.1016/J.PROCI.2022.08.016

  17. [18]

    ECTDL study of N 2 - And O 2 -pressure broadening of a series of ammonia lines in the 1.5 μm (ν 1 +ν 3 ) combination band

    Koshelev MA, Tretyakov MY, Lees RM, Xu LH. ECTDL study of N 2 - And O 2 -pressure broadening of a series of ammonia lines in the 1.5 μm (ν 1 +ν 3 ) combination band. Appl Phys B 2006;85:273 –7. https://doi.org/10.1007/s00340-006-2315-x

  18. [20]

    A comprehensive chemical kinetic modeling and experimental study of NH3−methanol/ethanol combustion towards net -zero CO2 emissions

    Shrestha KP, Giri BR, Pelé R, Aljohani K, Brequigny P, Mauss F, et al. A comprehensive chemical kinetic modeling and experimental study of NH3−methanol/ethanol combustion towards net -zero CO2 emissions. Combust Flame 2025;274:113954. https://doi.org/10.1016/J.COMBUSTFLAME.2024.113954

  19. [21]

    A Review on Combustion Characteristics of Ammonia as a Carbon-Free Fuel

    Li J, Lai S, Chen D, Wu R, Kobayashi N, Deng L, et al. A Review on Combustion Characteristics of Ammonia as a Carbon-Free Fuel. Front Energy Res 2021;9:760356. https://doi.org/10.3389/FENRG.2021.760356/FULL

  20. [22]

    A N2O laser absorption diagnostic near 4.6 μm for shock- tube chemical kinetics studies

    Mulvihill CR, Alturaifi SA, Mathieu O, Petersen EL. A N2O laser absorption diagnostic near 4.6 μm for shock- tube chemical kinetics studies. AIAA Scitech 2020 Forum 2020;1 PartF. https://doi.org/10.2514/6.2020 - 2143;JOURNAL:JOURNAL:6.SCITECH;PAGE:STRING:ARTICLE/CHAPTER

  21. [23]

    Analysis of gaseous ammonia (NH3) absorption in the visible spectrum of Jupiter - Update

    Irwin PGJ, Bowles N, Braude AS, Garland R, Calcutt S, Coles PA, et al. Analysis of gaseous ammonia (NH3) absorption in the visible spectrum of Jupiter - Update. Icarus 2019;321:572 –82. https://doi.org/10.1016/J.ICARUS.2018.12.008

  22. [24]

    Spectral data for the ν2 bands of ammonia with applications to radiative transfer in the atmosphere of jupiter

    Taylor FW. Spectral data for the ν2 bands of ammonia with applications to radiative transfer in the atmosphere of jupiter. J Quant Spectrosc Radiat Transf 1973;13:1181 –217. https://doi.org/10.1016/0022-4073(73)90088- 5

  23. [25]

    Saturn’s Great Storm of 2010 –2011: Evidence for ammonia and water ices from analysis of VIMS spectra

    Sromovsky LA, Baines KH, Fry PM. Saturn’s Great Storm of 2010 –2011: Evidence for ammonia and water ices from analysis of VIMS spectra. Icarus 2013;226:402–18. https://doi.org/10.1016/J.ICARUS.2013.05.043

  24. [26]

    Rothman, I.E

    Rothman LS, Gordon IE, Barber RJ, Dothe H, Gamache RR, Goldman A, et al. HITEMP, the high-temperature molecular spectroscopic database. J Quant Spectrosc Radiat Transf 2010;111:2139 –50. https://doi.org/10.1016/J.JQSRT.2010.05.001

  25. [27]

    The inversion spectrum of ammonia at centimetre wave -lengths

    BLEANEY B, PENROSE RP. The inversion spectrum of ammonia at centimetre wave -lengths. Proceedings of the Royal Society of London A Mathematical and Physical Sciences 1947;189:358 –71. https://doi.org/10.1098/RSPA.1947.0046

  26. [28]

    Shapes and widths of ammonia lines collision -broadened by hydrogen

    Varanasi P. Shapes and widths of ammonia lines collision -broadened by hydrogen. J Quant Spectrosc Radiat Transf 1972;12:1283–9. https://doi.org/10.1016/0022-4073(72)90184-7

  27. [29]

    An Empirical Expression for Linewidths of Ammonia from Far -Infrared Measurements

    Brown LR, Peterson DB. An Empirical Expression for Linewidths of Ammonia from Far -Infrared Measurements. J Mol Spectrosc 1994;168:593–606. https://doi.org/10.1006/JMSP.1994.1305

  28. [30]

    N2, O2, H2, Ar and He broadening in the ν1 band of NH3

    Pine AS, Markov VN, Buffa G, Tarrini O. N2, O2, H2, Ar and He broadening in the ν1 band of NH3. J Quant Spectrosc Radiat Transf 1993;50:337–48. https://doi.org/10.1016/0022-4073(93)90069-T

  29. [31]

    Measurements of line intensities and half -widths in the 10 -μm bands of 14NH3

    Nemtchinov V, Sung K, Varanasi P. Measurements of line intensities and half -widths in the 10 -μm bands of 14NH3. J Quant Spectrosc Radiat Transf 2004;83:243–65. https://doi.org/10.1016/S0022-4073(02)00354-0

  30. [32]

    , keywords =

    Gordon IE, Rothman LS, Hill C, Kochanov R V., Tan Y, Bernath PF, et al. The HITRAN2016 molecular spectroscopic database. J Quant Spectrosc Radiat Transf 2017;203:3 –69. https://doi.org/10.1016/J.JQSRT.2017.06.038

  31. [34]

    , keywords =

    Gordon IE, Rothman LS, Hargreaves RJ, Gomez FM, Bertin T, Hill C, et al. The HITRAN2024 molecular spectroscopic database. J Quant Spectrosc Radiat Transf 2026;353:109807. https://doi.org/10.1016/J.JQSRT.2026.109807

  32. [35]

    Gordon, L.S

    Gordon IE, Rothman LS, Hargreaves RJ, Hashemi R, Karlovets E V., Skinner FM, et al. The HITRAN2020 molecular spectroscopic database. J Quant Spectrosc Radiat Transf 2022;277. https://doi.org/10.1016/j.jqsrt.2021.107949. 43

  33. [36]

    The cavity -enhanced absorption spectrum of NH3 in the near -infrared region between 6850 and 7000 cm -1

    O’Leary DM, Orphal J, Ruth AA, Heitmann U, Chelin P, Fellows CE. The cavity -enhanced absorption spectrum of NH3 in the near -infrared region between 6850 and 7000 cm -1. J Quant Spectrosc Radiat Transf 2008;109:1004–15. https://doi.org/10.1016/j.jqsrt.2007.12.007

  34. [37]

    ABSORPTION INTENSITIES, PRESSURE-BROADENING AND LINE MIXING PARAMETERS OF SOME LINES OF NH3 IN THE v4 BAND

    Aroui*- H, Broquier M, Picard -Bersellini A, Bouanichm JP, Chevalier M, Gherissi S. ABSORPTION INTENSITIES, PRESSURE-BROADENING AND LINE MIXING PARAMETERS OF SOME LINES OF NH3 IN THE v4 BAND. J Quant Spectrosc Radiat 1ransfer 1998;60:1011 –23. https://doi.org/https://doi.org/10.1016/S0022-4073(97)00196-9

  35. [38]

    Absolute measurements of intensities, positions and self -broadening coefficients of R branch transitions in the ν2 band of ammonia

    Guinet M, Jeseck P, Mondelain D, Pepin I, Janssen C, Camy -Peyret C, et al. Absolute measurements of intensities, positions and self -broadening coefficients of R branch transitions in the ν2 band of ammonia. J Quant Spectrosc Radiat Transf 2011;112:1950–60. https://doi.org/10.1016/j.jqsrt.2011.03.015

  36. [39]

    Measurements of NH3 linestrengths and collisional broadening coefficients in N2, O2, CO2, and H2O near 1103.46cm -1

    Owen K, Es -sebbar E touhami, Farooq A. Measurements of NH3 linestrengths and collisional broadening coefficients in N2, O2, CO2, and H2O near 1103.46cm -1. J Quant Spectrosc Radiat Transf 2013;121:56 –68. https://doi.org/10.1016/j.jqsrt.2013.02.001

  37. [40]

    NH3 self -broadening coefficients in the v2 and v4 bands and line intensities in the v2 band

    Aroui H, Nouri S, Bouanich JP. NH3 self -broadening coefficients in the v2 and v4 bands and line intensities in the v2 band. J Mol Spectrosc 2003;220:248–58. https://doi.org/10.1016/S0022-2852(03)00124-3

  38. [41]

    Line intensities and temperature- dependent line broadening coefficients of Q -branch transitions in the v2 band of ammonia near 10.4 μm

    Sur R, Mitchell Spearrin R, Peng WY, Strand CL, Jeffries JB, Enns GM, et al. Line intensities and temperature- dependent line broadening coefficients of Q -branch transitions in the v2 band of ammonia near 10.4 μm. J Quant Spectrosc Radiat Transf 2016;175:90–9. https://doi.org/10.1016/j.jqsrt.2016.02.002

  39. [42]

    Broadening, shift and narrowing coefficients in the 2ν4 band of NH3 perturbed by O2, N2 and air

    Maaroufi N, Hmida F, Tchana FK, Landsheere X, Aroui H. Broadening, shift and narrowing coefficients in the 2ν4 band of NH3 perturbed by O2, N2 and air. J Quant Spectrosc Radiat Transf 2021;258. https://doi.org/10.1016/j.jqsrt.2020.107393

  40. [43]

    Self - and foreign-gas-broadened lineshapes in the v1 band of NH3

    Pine AS, Markov VN. Self - and foreign-gas-broadened lineshapes in the v1 band of NH3. J Mol Spectrosc 2004;228:121–42. https://doi.org/10.1016/j.jms.2004.07.007

  41. [44]

    Pressure broadening and shift coefficients in the ν1 and ν3 bands of NH3

    Maaroufi N, Tchana FK, Landsheere X, Aroui H. Pressure broadening and shift coefficients in the ν1 and ν3 bands of NH3. J Quant Spectrosc Radiat Transf 2018;219:383–92. https://doi.org/10.1016/j.jqsrt.2018.09.001

  42. [45]

    Ammonia line strengths and N2-, O2-, Ar-, He-, and self-broadening coefficients in the v2 band near 10.4 µm

    Alturaifi SA, Petersen EL. Ammonia line strengths and N2-, O2-, Ar-, He-, and self-broadening coefficients in the v2 band near 10.4 µm. J Quant Spectrosc Radiat Transf 2021;262. https://doi.org/10.1016/j.jqsrt.2021.107516

  43. [46]

    New quantitative measurements and spectroscopic line parameters of ammonia in the 685 -1250 cm-1 spectral region for atmospheric remote sensing

    Coxon DJL, Harrison JJ, Benner DC, Devi VM. New quantitative measurements and spectroscopic line parameters of ammonia in the 685 -1250 cm-1 spectral region for atmospheric remote sensing. Atmos Meas Tech 2025;18:7421–44. https://doi.org/10.5194/amt-18-7421-2025

  44. [48]

    N2, O2, and air broadening of NH3 in ν2 band measured by FTIR spectroscopy

    Fabian M, Ito F, Yamada KMT. Corrigendum to “N2, O2, and air broadening of NH3 in ν2 band measured by FTIR spectroscopy” [J. Mol. Spectrosc. 173 (1995) 591 –602]. J Mol Spectrosc 2006;236:150. https://doi.org/10.1016/J.JMS.2005.12.015

  45. [49]

    THE HITRAN MOLECULAR SPECTROSCOPIC DATABASE AND HAWKS (HITRAN ATMOSPHERIC WORKSTATION): 1996 EDITION

    Rothman,*- ‡ LS, Rinsland CP, Goldman A, Massie ¶ S T, Edwards # D P, Flaud J -M, et al. THE HITRAN MOLECULAR SPECTROSCOPIC DATABASE AND HAWKS (HITRAN ATMOSPHERIC WORKSTATION): 1996 EDITION. vol. 60. 1998

  46. [50]

    The HITRAN molecular spectroscopic database: Edition of 2000 including updates through 2001

    Rothman LS, Barbe A, Benner DC, Brown LR, Camy -Peyret C, Carleer MR, et al. The HITRAN molecular spectroscopic database: Edition of 2000 including updates through 2001. J Quant Spectrosc Radiat Transf 2003;82:5–44. https://doi.org/10.1016/S0022-4073(03)00146-8

  47. [51]

    The HITRAN 2004 molecular spectroscopic database

    Rothman LS, Jacquemart D, Barbe A, Benner DC, Birk M, Brown LR, et al. The HITRAN 2004 molecular spectroscopic database. J Quant Spectrosc Radiat Transf 2005;96:139 –204. https://doi.org/10.1016/j.jqsrt.2004.10.008

  48. [52]

    The HITRAN 2008 molecular spectroscopic database

    Rothman LS, Gordon IE, Barbe A, Benner DC, Bernath PF, Birk M, et al. The HITRAN 2008 molecular spectroscopic database. J Quant Spectrosc Radiat Transf 2009;110:533 –72. https://doi.org/10.1016/j.jqsrt.2009.02.013

  49. [53]

    On Atmospheric Retrievals of Exoplanets with Inhomogeneous Terminators

    Welbanks L, Madhusudhan N. On Atmospheric Retrievals of Exoplanets with Inhomogeneous Terminators. Astrophys J 2022;933:79. https://doi.org/10.3847/1538-4357/AC6DF1

  50. [54]

    Simultaneous retrieval of orbital phase resolved JWST/MIRI emission spectra of the hot Jupiter WASP-43b: evidence of water, ammonia, and carbon monoxide

    Yang J, Hammond M, Piette AAA, Blecic J, Bell TJ, Irwin PGJ, et al. Simultaneous retrieval of orbital phase resolved JWST/MIRI emission spectra of the hot Jupiter WASP-43b: evidence of water, ammonia, and carbon monoxide. Mon Not R Astron Soc 2024;532:460–75. https://doi.org/10.1093/MNRAS/STAE1427

  51. [55]

    Erratum: N2, O2, and air broadening of NH3 in ν2 band measured by FTIR spectroscopy (Journal of Molecular Spectroscopy (1995) 173 (591-602) DOI: 10.1006/jmsp.1995.1260)

    Fabian M, Ito F, Yamada KMT. Erratum: N2, O2, and air broadening of NH3 in ν2 band measured by FTIR spectroscopy (Journal of Molecular Spectroscopy (1995) 173 (591-602) DOI: 10.1006/jmsp.1995.1260). J Mol Spectrosc 2006;236:150. https://doi.org/10.1016/j.jms.2005.12.015. 44

  52. [56]

    Gas-phase databases for quantitative infrared spectroscopy

    Sharpe SW, Johnson TJ, Sams RL, Chu PM, Rhoderick GC, Johnson PA. Gas-phase databases for quantitative infrared spectroscopy. Appl Spectrosc 2004;58:1452–61