Articles | Volume 21, issue 24
https://doi.org/10.5194/acp-21-18319-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/acp-21-18319-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Formaldehyde evolution in US wildfire plumes during the Fire Influence on Regional to Global Environments and Air Quality experiment (FIREX-AQ)
Jin Liao
CORRESPONDING AUTHOR
Atmospheric Chemistry and Dynamics Laboratory, NASA Goddard Space Flight Center, Greenbelt, MD, USA
Goddard Earth Science Technology and Research (GESTAR) II, University of Maryland Baltimore County, Baltimore, MD, USA
Glenn M. Wolfe
Atmospheric Chemistry and Dynamics Laboratory, NASA Goddard Space Flight Center, Greenbelt, MD, USA
Reem A. Hannun
Atmospheric Chemistry and Dynamics Laboratory, NASA Goddard Space Flight Center, Greenbelt, MD, USA
Joint Center for Earth Systems Technology, University of Maryland Baltimore County, Baltimore, MD, USA
Jason M. St. Clair
Atmospheric Chemistry and Dynamics Laboratory, NASA Goddard Space Flight Center, Greenbelt, MD, USA
Joint Center for Earth Systems Technology, University of Maryland Baltimore County, Baltimore, MD, USA
Thomas F. Hanisco
Atmospheric Chemistry and Dynamics Laboratory, NASA Goddard Space Flight Center, Greenbelt, MD, USA
Jessica B. Gilman
NOAA Chemical Science Laboratory (CSL), Boulder, CO, USA
Aaron Lamplugh
NOAA Chemical Science Laboratory (CSL), Boulder, CO, USA
Cooperative Institute for Research in Environmental Science (CIRES), University of Colorado, Boulder, CO, USA
Vanessa Selimovic
Department of Chemistry, University of Montana, Missoula, MT, USA
Glenn S. Diskin
NASA Langley Research Center, Hampton, VA, USA
John B. Nowak
NASA Langley Research Center, Hampton, VA, USA
Hannah S. Halliday
Environmental Protection Agency, Durham, NC, USA
Joshua P. DiGangi
NASA Langley Research Center, Hampton, VA, USA
Samuel R. Hall
Atmospheric Chemistry Observations & Modeling Laboratory, National Center for Atmospheric Research, Boulder, CO, USA
Kirk Ullmann
Atmospheric Chemistry Observations & Modeling Laboratory, National Center for Atmospheric Research, Boulder, CO, USA
Christopher D. Holmes
Earth, Ocean and Atmospheric Science, Florida State University, Tallahassee, FL, USA
Charles H. Fite
Earth, Ocean and Atmospheric Science, Florida State University, Tallahassee, FL, USA
Anxhelo Agastra
Earth, Ocean and Atmospheric Science, Florida State University, Tallahassee, FL, USA
Thomas B. Ryerson
NOAA Chemical Science Laboratory (CSL), Boulder, CO, USA
now at: Scientific Aviation, Boulder, CO, USA
Jeff Peischl
NOAA Chemical Science Laboratory (CSL), Boulder, CO, USA
Cooperative Institute for Research in Environmental Science (CIRES), University of Colorado, Boulder, CO, USA
Ilann Bourgeois
NOAA Chemical Science Laboratory (CSL), Boulder, CO, USA
Cooperative Institute for Research in Environmental Science (CIRES), University of Colorado, Boulder, CO, USA
Carsten Warneke
NOAA Chemical Science Laboratory (CSL), Boulder, CO, USA
Matthew M. Coggon
NOAA Chemical Science Laboratory (CSL), Boulder, CO, USA
Cooperative Institute for Research in Environmental Science (CIRES), University of Colorado, Boulder, CO, USA
Georgios I. Gkatzelis
NOAA Chemical Science Laboratory (CSL), Boulder, CO, USA
Cooperative Institute for Research in Environmental Science (CIRES), University of Colorado, Boulder, CO, USA
now at: Forschungszentrum Jülich GmbH, Jülich, Nordrhein-Westfalen, Germany
Kanako Sekimoto
Yokohama City University, Yokohama, Japan
Alan Fried
Institute of Arctic and Alpine Research (INSTAAR), University of Colorado, Boulder, CO, USA
Dirk Richter
Institute of Arctic and Alpine Research (INSTAAR), University of Colorado, Boulder, CO, USA
Petter Weibring
Institute of Arctic and Alpine Research (INSTAAR), University of Colorado, Boulder, CO, USA
Eric C. Apel
Atmospheric Chemistry Observations & Modeling Laboratory, National Center for Atmospheric Research, Boulder, CO, USA
Rebecca S. Hornbrook
Atmospheric Chemistry Observations & Modeling Laboratory, National Center for Atmospheric Research, Boulder, CO, USA
Steven S. Brown
NOAA Chemical Science Laboratory (CSL), Boulder, CO, USA
Caroline C. Womack
NOAA Chemical Science Laboratory (CSL), Boulder, CO, USA
Cooperative Institute for Research in Environmental Science (CIRES), University of Colorado, Boulder, CO, USA
Michael A. Robinson
NOAA Chemical Science Laboratory (CSL), Boulder, CO, USA
Cooperative Institute for Research in Environmental Science (CIRES), University of Colorado, Boulder, CO, USA
Rebecca A. Washenfelder
NOAA Chemical Science Laboratory (CSL), Boulder, CO, USA
Patrick R. Veres
NOAA Chemical Science Laboratory (CSL), Boulder, CO, USA
J. Andrew Neuman
NOAA Chemical Science Laboratory (CSL), Boulder, CO, USA
Cooperative Institute for Research in Environmental Science (CIRES), University of Colorado, Boulder, CO, USA
Download
- Final revised paper (published on 17 Dec 2021)
- Supplement to the final revised paper
- Preprint (discussion started on 31 May 2021)
- Supplement to the preprint
Interactive discussion
Status: closed
Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor
| : Report abuse
-
RC1: 'Comment on acp-2021-389', Anonymous Referee #1, 25 Jun 2021
-
AC1: 'Reply on RC1', Jin Liao, 27 Aug 2021
The comment was uploaded in the form of a supplement: https://acp.copernicus.org/preprints/acp-2021-389/acp-2021-389-AC1-supplement.pdf
-
AC1: 'Reply on RC1', Jin Liao, 27 Aug 2021
-
RC2: 'Comment on acp-2021-389', Anonymous Referee #2, 02 Jul 2021
The comment was uploaded in the form of a supplement: https://acp.copernicus.org/preprints/acp-2021-389/acp-2021-389-RC2-supplement.pdf
-
AC2: 'Reply on RC2', Jin Liao, 27 Aug 2021
The comment was uploaded in the form of a supplement: https://acp.copernicus.org/preprints/acp-2021-389/acp-2021-389-AC2-supplement.pdf
-
AC2: 'Reply on RC2', Jin Liao, 27 Aug 2021
Peer review completion
AR: Author's response | RR: Referee report | ED: Editor decision | EF: Editorial file upload
AR by Jin Liao on behalf of the Authors (13 Sep 2021)
Author's response
Author's tracked changes
Manuscript
ED: Referee Nomination & Report Request started (15 Oct 2021) by Manvendra Krishna Dubey
RR by Anonymous Referee #1 (27 Oct 2021)
RR by Anonymous Referee #2 (29 Oct 2021)


ED: Publish subject to minor revisions (review by editor) (08 Nov 2021) by Manvendra Krishna Dubey


AR by Jin Liao on behalf of the Authors (09 Nov 2021)
Author's response
Author's tracked changes
Manuscript
ED: Publish as is (10 Nov 2021) by Manvendra Krishna Dubey


AR by Jin Liao on behalf of the Authors (10 Nov 2021)
Manuscript
Short summary
Formaldehyde (HCHO) is an important oxidant precursor and affects the formation of O3 and other secondary pollutants in wildfire plumes. We disentangle the processes controlling HCHO evolution from wildfire plumes sampled by NASA DC-8 during FIREX-AQ. We find that OH abundance rather than normalized OH reactivity is the main driver of fire-to-fire variability in HCHO secondary production and estimate an effective HCHO yield per volatile organic compound molecule oxidized in wildfire plumes.
Formaldehyde (HCHO) is an important oxidant precursor and affects the formation of O3 and other...
Altmetrics
Final-revised paper
Preprint
This manuscript analyzes formaldehyde data from select FIREX flights to better understand its production and loss and the drivers of secondary HCHO production. Overall, I found the science hard to follow as limited detail were given for the analyses. The descriptions and explanations need to be expanded to elevate the contribution and scientific the impact of the paper.
Specific Comments:
Line 192: How consistent was the background HCHO concentration? Was a single value appropriate to use as a cutoff?
Line 210: cited the paper! Coggon, Matthew M., Christopher Y. Lim, Abigail R. Koss, Kanako Sekimoto, Bin Yuan, Jessica B. Gilman, David H. Hagan, et al. “OH Chemistry of Non-Methane Organic Gases (NMOGs) Emitted from Laboratory and Ambient Biomass Burning Smoke: Evaluating the Influence of Furans and Oxygenated Aromatics on Ozone and Secondary NMOG Formation.” Atmospheric Chemistry and Physics 19, no. 23 (December 10, 2019): 14875–99. https://doi.org/10.5194/acp-19-14875-2019.
Line 222: Which did you use or did the combination of the two help constrain the uncertainty? The slopes are different for each compound – that is due to the different k values of OH and O3 for the 2 compounds? The use of these two compounds should be more explicitly described with more specifics about what the different slopes indicate. Figure 2 or S2 (how are they different?) aren’t that helpful to your discussion. Yes all the slopes look pretty good - should we take away more than that?
Line 230: Including the k values you used here and whether they were corrected for the ambient temperature is important.
Line 235: Again which butane compound are you using for your OH calculation? Both? [This becomes apparent later but this is where I want to know the details]
Line 236: Often there are O3 deficits in the smoke plume center due to the rapid chemistry happening creating strong gradients in O3 concentration. How sensitive are your derived OH concentrations to the range of O3 in a particular transect? I realize that you say the uncertainty of O3 variation is taken into account in the total plume-average OH uncertainty but on a component by component basis how much uncertainty is each term contributing? Also reference your table in the supplement here with the OH uncertainty and add the OH concentration to the table too so we can compare the uncertainty to the value.
Line 252: 27% higher is not slight but from the figure it does appear to be within the error of the calculation. Either say that or do a hypothesis test to show they aren’t statistically different. Explain why there might be a systematic bias in the reaction rate at low temperature. Do you see a trend in the comparison with temperature? Is there a study you can cite to support the suspected bias in k?
Line 305: I suggest showing the OH concentrations first (Fig 3) since they are used in Figure 1 for the blue curves. When they are first mentioned is when I want to know more about them.
Line 309: Does it really represent an upper limit on the emitted HCHO? That implies you know that there was no loss of HCHO in the plume prior to measurement. What evidence do you have to support this?
Line 313: What is the difference between the blue and the black curves? Blue: predicted decay of primary nHCHO from J and OH. Black: calculated primary nHCHO. These seem to be almost the same definition - or is there very little loss of the primary nHCHO. Perhaps refer to the equations to highlight which terms are different? The two lines are pretty similar for all shown cases – do both need to be shown? What is the main goal of showing both of these calculated trends? It would be better to show a figure related to the discussion of the fraction of primary v secondary HCHO over the lifetime of the plume (as discussed in the text) and how it varies. A figure like I just described would facilitate your analysis of the drivers of HCHO.
Line 322: This is not obvious in the figure since most start out with a positive trend in the measured values with time and then the loss overtakes the production. It just happens faster in the 3 you highlight with larger loss rates than production in the table. Perhaps you can color the fit line to show if the plume net loss exceeded production to make it clearer? It might be more informative to show the role of J and OH loss and the balance with production across the physical ages of the plume. A figure like this would more clearly show the point that I believe you are trying to make (what are the controls on HCHO concentration in fire plumes and how do they vary).
Section 3.2: This section needs to be the first part of the results and discussion section since the OH concentration is used to calculate the loss of primary nHCHO.
Section 3.3: At the beginning of this section remind the reader how you are determining secondary HCHO production - a mass balance approach with loss, production, and dilution terms - and not from VOC chemistry.
Line 360: Since secondary production was calculated with the OH concentrations I would expect there to be a correlation between the 2 terms. How does the correlation with J compare to that with OH? Or other oxidants? A more comprehensive analysis and discussion would guide the reader to the same conclusion that you make.
Line 366: A high R2 doesn’t necessarily mean that the relationship is significant. Including a statistical analysis with the p values with strengthen the conclusions you are making.
Line 368: What other potential drives of secondary HCHO production did you look at? How does the trend/relationship change if the eastern US fire is excluded? It looks pretty different (high VOCs and nHCHO) and there is only one fire from that region.
Line 370: Why exclude NO2 and CO in the OH reactivity analysis? If interested in the role of VOCs I understand but the controls on OH concentration will still include NO2 and CO. I more complete analysis looking at both the total and VOC reactivity would improve the work since I expect there is variability in the NO2 (and CO) that makes the VOC/total reactivity vary by plume.
Line 372: This sentence is a repeat of 368 and it still isn’t clear if you actually are showing this.
Line 380: I don’t understand this logic since it seems to contradict your analysis in the previous paragraph where you said a strong correlation indicated OH was an important driver. I can’t really tell how different [OH-VOC reactivity/CO] is from [OH-VOC reactivity/CO * OH] but I imagine the valves are scaled pretty linearly. It might be more informative [OH-VOC reactivity/CO] on the x-axis and getting rid of the colors in 4a since they are hard to see anyway. You could also show with [OH-VOC reactivity/CO * OH] to get the effective yield.
Line 401: What were the PTRMS measurements used for? It is unclear as written and how this information is related to the current discussion. Why is this one compound so important?
Line 407-11: You should not be comparing western and eastern fires give the number of eastern fires in this analysis is 1. You have no idea what if the fire was representative of other fires in the region. I suggest rewriting/adding that more data from eastern fires are needed to understand how they may be different as suggested by this one fire.
Line 436: Did you show that the variability in the reactive VOC pool is not playing an important role? I’m not sure the analysis presented before this does a good job of this since the figure is weighted by OH.
No technical comments.