the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Measurement report: Analysis of aerosol optical depth variation at Zhongshan Station in Antarctica
Abstract. Our understanding of aerosol optical depth (AOD) in Antarctica remains limited due to the scarcity of ground observation stations and limited daylight days. Utilizing data from the CE318-T photometer spanning from January 2020 to April 2023 at Zhongshan Station, we analysed the seasonal, monthly, and diurnal variations in AOD and Ångström exponent (AE). AOD median values increased from spring (0.033) to winter (0.115), while AE peaked during summer (1.010) and autumn (1.034), declining in winter (0.381), indicating a transition in dominant aerosol particle size from fine to coarse mode between summer and winter. Monthly mean AOD variation closely paralleled the proportion of AE<1, suggesting fluctuations in coarse mode particle proportions drive AOD variation. Increases in AOD during spring and winter correlated with decreases in fine mode fraction, while increases during summer and winter related to fine mode particle growth and aging. We observed a peak in AOD (~0.06) at 14:00 local time at Zhongshan Station, possibly associated with a slight decrease in boundary layer height (BLH). Additionally, higher (lower) wind speeds corresponded to lower (higher) AOD values, indicating the diffusion (accumulation) effect. The temperature and AOD showed an insignificant positive correlation between (R = 0.22, p = 0.40), relative humidity exhibited a significant negative correlation with AOD (R = -0.59, p = 0.02). Backward trajectory analysis revealed that coarse particles from the ocean predominantly contributed to high AOD daily mean values in summer, while fine particles on low AOD days originated mainly from the air mass over the Antarctic Plateau.
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Status: open (until 19 Sep 2024)
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RC1: 'Comment on egusphere-2024-798', Anonymous Referee #1, 01 Aug 2024
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This study is too simple and may be well-suited as a measurement report. Undoubtedly, the aerosols in that location are very important to study, but the paper lacks enough depth to it.
However, I have some minor comments
“The increase in AOD during spring and winter correlates with a reduction in the fine mode fraction, whereas the increase observed in summer and autumn may be attributed to the growth and aging of fine particles.” How can both increase? Please correct
“Increases in AOD during spring and winter correlated with decreases in fine mode fraction, while increases during summer and winter related to fine mode particle growth and aging.” This line is very confusing with the usage of ‘increase’’
The last line in abstract only talks about the origins of particles in the summer. Why specifically summer? Why not other seasons?
The abstract is incomplete. I suggest you to add a conclusion line to your abstract as to why this study is important or how it can help others?
How is DMS found in the plateau? Does it come from transportation from ocean? But you have mentioned about katabatic winds that drive from interior to coastal
“AOD675 nm is associated with the declining 𝜂”….. introduce 𝜂 before using it
Citation: https://doi.org/10.5194/egusphere-2024-798-RC1 -
AC1: 'Reply on RC1', Lijing Chen, 19 Aug 2024
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Thank you for your comments. We have revised the type of the manuscript to "Measurement Report". The supplement is our responds to your comments. And we hope our responds can address your concerns.
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AC1: 'Reply on RC1', Lijing Chen, 19 Aug 2024
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Data sets
Analysis of aerosol optical depth variation at Zhongshan Station in Antarctica L. Chen https://doi.org/10.5281/zenodo.10983097
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