Articles | Volume 25, issue 20
https://doi.org/10.5194/acp-25-13975-2025
© Author(s) 2025. This work is distributed under the Creative Commons Attribution 4.0 License.
The sources and diurnal variations of submicron aerosols in a coastal–rural environment near Houston, US
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- Final revised paper (published on 28 Oct 2025)
- Supplement to the final revised paper
- Preprint (discussion started on 24 Mar 2025)
- Supplement to the preprint
Interactive discussion
Status: closed
Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor
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- RC1: 'Comment on egusphere-2025-726', Anonymous Referee #1, 27 Apr 2025
- RC2: 'Comment on egusphere-2025-726', Anonymous Referee #2, 26 May 2025
- AC1: 'Comment on egusphere-2025-726', Jing Li, 21 Jul 2025
Peer review completion
AR: Author's response | RR: Referee report | ED: Editor decision | EF: Editorial file upload
AR by Jing Li on behalf of the Authors (21 Jul 2025)
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ED: Publish as is (08 Aug 2025) by Sergio Rodríguez
AR by Jing Li on behalf of the Authors (11 Aug 2025)
Manuscript
Li et al., present a study of aerosol characteristics conducted at rural site southwest of Houston during the intensive operation periods (IOP) of the Tracking Aerosol Convection Interactions ExpeRiment. They report significant differences in aerosol properties among marine, urban, and regional air masses, and identified six OA factors using PMF analysis. The results emphasize the roles of both atmospheric chemistry and meteorological conditions in this coastal-rural site. Overall, the manuscript is well-written and fits within the scope of the journal. However, the following comments need to be addressed before publication.
Line 185: Although the CWT map of ammonium is consistent with sulfate, the sources of ammonium could not from marine emissions. The authors should provide further discussion or references regarding potential terrestrial or anthropogenic sources of ammonium. Additionally, the organic nitrate mentioned also needs stronger supporting evidence.
Section 3.2: The time series of all six PMF-resolved OA factors display high similarity, particularly during urban air mass periods. This raises questions about the robustness of the factor separation. For example, how to explain the co-variation of primary and secondary factors during the air mass from urban areas. In addition, how is the six-solution result determined? Providing diagnostics for this six-solution is beneficial for reader to understand.
Line 215-225 paragraph: The attribution of 91FAC to monoterpene oxidation is reasonable based on spectral comparisons, but a few concerns remain: (1) the O/C ratio is higher in previous study using HR-ToF-AMS observation; (2) the name of 91FAC may cause confusion and a more descriptive term may improve clarity.
Section 3.2.2: OOA1 is characterized by strong signals from m/z 55 and 57, which are typically associated with primary OA. However, the authors classify it as a secondary factor and link it to ship emissions. This conclusion needs further justification, such as its high O/C ratio and diurnal variation consistent with OOA2 and OOA3.
OOA3: The decomposition of OOA3 by air masses is novel and provides useful insights. However, the explanation for the noon peak being due to longer land residence is somewhat inconsistent. Based on wind direction, southerly winds from the sea dominated during the daytime which contradicts the interpretation of increased urban influence. If the different diurnal variations between different air masses, it is generally not combined into one factor during the decomposition of PMF. In addition, the diurnal pattern of OOA3 within individual air mass is nearly flat, however the box model results show daytime production. Why is this happening?