the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
| 14 Oct 2025
Trace Organic Gas Analyzer Time-of-Flight mass spectrometer (TOGA-TOF) system for airborne observations of formaldehyde
Abstract. Formaldehyde (HCHO) is a ubiquitous atmospheric constituent, originating from primary emissions (natural and anthropogenic) and secondary production via the oxidation of volatile organic compounds (VOCs). In addition to being a regulated pollutant, HCHO is a key species used as a tracer of recent photochemical activity due to its short atmospheric lifetime and its role as a source of HOx radicals. Given its diverse sources and high spatial variability, HCHO is challenging to represent accurately in chemical transport models, often resulting in significant discrepancies with observations. Airborne in-situ measurements of HCHO, especially when combined with VOC precursor data, offer valuable insights into its atmospheric distributions for evaluating models. Here, we present HCHO observations from the NSF NCAR Trace Organic Gas Analyzer with Time-of-Flight mass spectrometer (TOGA-TOF), deployed during the 2019 Fire Influence on Regional to Global Environments and Air Quality (FIREX-AQ) campaign. While most HCHO instruments target at most a few selected species for measurement, the TOGA-TOF employs a rapid gas chromatography-mass spectrometry (GC/MS) technique and provides discrete VOC measurements—including >100 C1–C10 species—at a time resolution of less than 2 minutes. We compare TOGA-TOF HCHO data to measurements from three 1-Hz instruments aboard the NASA DC-8: the Compact Atmospheric Multi-species Spectrometer (CAMS), the In Situ Airborne Formaldehyde (ISAF) instrument, and a proton-transfer-reaction time-of-flight mass spectrometer (PTR-ToF-MS). The wide dynamic range of observed HCHO concentrations (from < 100 ppt to ~100 ppb) during FIREX-AQ enabled a robust intercomparison. TOGA-TOF HCHO agreed well with CAMS (slope = 1.1), with similar agreement with the PTR-ToF-MS, while larger discrepancies were observed with ISAF (slope = 1.5), likely due to differences in calibrations. Normalized excess mixing ratios (NEMRs) of HCHO relative to CO in wildfire plumes exhibited consistent trends with plume age across instruments. These findings highlight the TOGA-TOF’s capability for highly sensitive and accurate airborne HCHO measurements.
Competing interests: At least one of the (co-)authors is a member of the editorial board of Atmospheric Measurement Techniques.
Publisher's note: Copernicus Publications remains neutral with regard to jurisdictional claims made in the text, published maps, institutional affiliations, or any other geographical representation in this paper. While Copernicus Publications makes every effort to include appropriate place names, the final responsibility lies with the authors. Views expressed in the text are those of the authors and do not necessarily reflect the views of the publisher.- Preprint
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Status: open (until 19 Nov 2025)
- RC1: 'Comment on egusphere-2025-4703', Anonymous Referee #1, 02 Nov 2025 reply
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- 1
Summary Evaluation
This is an excellent and well-prepared paper that presents a valuable intercomparison of airborne formaldehyde (HCHO) measurements from four instruments (TOGA-TOF, CAMS, PTR-ToF, and ISAF) during the FIREX-AQ campaign. The study is well designed and supported by a large dataset of co-located observations, allowing robust statistical analysis across a broad concentration range. The close agreement between TOGA-TOF, CAMS, and PTR-ToF confirms that TOGA-TOF provides what the author’s describe as reliable and accurate in situ HCHO data.
The TOGA-TOF measurements seem especially useful because it can measure both HCHO plus a large suite of precursor VOCs. As they are on the same instrument this can eliminate some of the sources of instrumental and sampling error. It would be nice if some recommendations could be made with regards to maintaining sample integrity and calibration best practise.
The authors’ use of volume-weighted averaging demonstrates careful consideration of the different temporal resolutions among the instruments, rather than simple averaging. This approach can be considered for all instruments taking discrete samples, such as a sample pre-concentration or quite commonly, the capture of whole air samples (where fill rate is not constant across the entire sampling period) and is a useful demonstration of this type of analysis.
The manuscript is clearly written, easy to follow, and provides an important contribution to airborne trace gas measurement science. The results are directly relevant to ongoing efforts to improve instrument consistency and model–measurement comparison
Specific Comments
1. Calibration methodology
Different instruments have different inlets, pumping speeds, pressures etc. Can the authors suggest what might have an effect on HCHO sampling integrity? Is there an understanding of the favourable parameters from each instrument and what would be the optimal sampling strategy for HCHO?
The authors note that differences among instruments (TOGA-TOF, CAMS, ISAF, PTR-ToF) may stem partly from different calibration approaches and standards. What are the pros and cons of the different methods and is there a preferred technique? Is there one instrumental technique that shows the best accuracy, or are certain techniques limited by practicalities?
It is stated that calibration differences likely explain the observed offsets, if possible, it would also be useful to indicate how much of the stated total uncertainty (≈35%) is attributed to calibration versus instrumental variability or sample integrity?
2. Sampling frequency and averaging
The use of volume-weighted averaging is a good way to align the slower TOGA-TOF data (33 s) with the faster instruments (1 Hz). It might be worth adding one or two sentences to acknowledge that while this approach slightly limits the instrument’s ability to resolve rapid plume variability, the time resolution and inherent averaging is actually well suited for model comparison and regional-scale studies, if of course this is the conclusion.
3. Use of CO as a strictly conservative tracer of dilution. CO is useful because it is as separate measurement to all the instruments being compared, but I believe it can have secondary production in the plume from VOC oxidation and could be oxidised itself? perhaps a VOC that TOGA measures could be used for estimating plume aging, perhaps acetonitrile? This would be interesting in future analysis because by being measured by the same instrument, some systematic errors could be eliminated.
technical corrections:
Excellent with just a few inconsistencies such as hypens in situ/ in-situ, 1 Hz /1-Hz and some spacing around parentheses.