Zou Xuanyu, Zhao Shoudong, Tang Jie, Zheng Xiangdong, Zhang Dongqi, Bian Lingen. 2023. Observations of atmospheric trace gases along the R/V Beijing cruise track between China and Antarctica: Data QA/QC and preliminary results. Acta Meteorologica Sinica, 81(5):838-852. DOI: 10.11676/qxxb2023.20220211
Citation: Zou Xuanyu, Zhao Shoudong, Tang Jie, Zheng Xiangdong, Zhang Dongqi, Bian Lingen. 2023. Observations of atmospheric trace gases along the R/V Beijing cruise track between China and Antarctica: Data QA/QC and preliminary results. Acta Meteorologica Sinica, 81(5):838-852. DOI: 10.11676/qxxb2023.20220211

Observations of atmospheric trace gases along the R/V Beijing cruise track between China and Antarctica: Data QA/QC and preliminary results

  • Atmospheric chemistry observations aboard ships are vulnerable to pollution from ship fuel engine exhaust. This local pollution leads to an increase in CO and CO2 and a decrease in O3. Concentrations (presented as volume mixing ratio) of CO, CO2, O3, CH4 and N2O in the marine-atmosphere boundary layer were measured along the R/V Beijing cruise track between Bohai bay of China and the Ross sea in Antarctica from January to April 2020. Based on the successive observations of 1-minute resolution, the impact of local pollution emission on the measured values of each trace gas is respectively implied by the persistence of variations in CO, CO2, and combinations of CO and CO2 and CO/CO2 for the study of data quality assessment quality controls (QA/QC). The results show that CO, CO2 and O3 (CH4 and N2O) data are significantly (slightly) contaminated by local pollution. A method of trace concentration difference threshold between any immediate adjacent 1-minute is proposed, which can effectively remove the outliers of CH4 and N2O from their time series datasets. The pollution period implied by CO or CO2 can be partially but not completely used to identify the contaminations in the dataset. The ratio of CO/CO2 implication can effectively determine the global baseline concentration of CO or CO2 in highly polluted region but at a high cost of discarding many data samples. The combination of CO2 and CO (CO2+CO) is the best method to imply the pollution signals in the CO2, CO and O3 datasets, and this method decreases the measured values of CO and CO2 concentrations in the southern hemisphere and the pristine region by (5—11)×10−9 (10%—18%) and (3—7)×10−6 (1%—2%) respectively, while O3 increases by (3—5)×10−9 (20%—25%). The final version concentration data of each trace gas are reasonably comparable with those measured at continental sites and the concentration differences of CO, CO2, CH4 and N2O in the southern ocean and Antarctica are respectively within 2×10−9, 0.7 ×10−6, 1.4×10−9 and 0.5×10−9. All the atmospheric trace gases data after QA/QC display their concentration features of high (low) in the northern (southern) hemisphere, and they remain stable in the south of the Southern Ocean and Antarctica region. Additionally, regional distribution characteristics of atmospheric O3 and their mechanisms are quite reasonable. All these reflect the rationality and accuracy of the proposed QA/QC method applied for the trace gases observations along the R/V Beijing cruise.
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