3-D Changes of Tropospheric O3 in Central and Eastern China Induced by Tropical Cyclones over the Northwest Pacific: Recent-Year Characterization with Multi-Source Observations

• Published in: Remote sensing (Basel, Switzerland) Switzerland), 2024-04, Vol.16 (7), p.1178
• Main Authors: Jiang, Yongcheng, Zhao, Tianliang, Meng, Kai, Cheng, Xugeng, Lv, Qiaoyi
• Format: Article
• Language: English
• Subjects: Air pollution; Anomalies; Climate; Climatology; Cyclones; Datasets; Intrusion; meteorological condition; Monsoons; Outdoor air quality; Peripheral circulation; Photochemicals; Radiation; Remote sensing; Seasonal variations; Stratosphere; stratospheric intrusion; tropical cyclone; Tropical cyclones; Troposphere; tropospheric O3; VOCs; Volatile organic compounds; Weather; Wind
• ISSN: 2072-4292; 2072-4292
• DOI: 10.3390/rs16071178

In this study, the multi-year data of meteorology and O3 from remote sensing and ground observations are applied to characterize the 3-D changes of O3 in the troposphere over central and eastern China (CEC) induced by the tropical cyclones (TCs) in the tropical and subtropical ocean regions over Northwest Pacific. The CEC-regional average of near-surface O3 levels is significantly elevated with 6.0 ppb in the large coverage by the TCs in the subtropical ocean, while the TCs in the tropical ocean alter near-surface O3 weakly, indicating the latitudinal-located TCs in the subtropical offshore ocean could largely influence the O3 variations over CEC. The sub-seasonal change with the positive and negative anomalies of near-surface O3 is induced by the tropical TCs from June to July and from August to October. The peripheral circulation of TCs in the subtropical offshore ocean persistently enhances the O3 concentrations over CEC during the season of East Asian summer monsoons. The positive O3 anomalies maintain from the entire troposphere to the lower stratosphere over CEC in the peripheries of subtropical TCs, while the tropical TCs cause the positive O3 anomalies merely in the lower troposphere. The O3 transport and accumulation, photochemical production and stratospheric intrusion are climatologically confirmed as the major meteorological mechanisms of TCs affecting the O3 variations. This study reveals that the downward transport of stratospheric O3 of TCs in the subtropical ocean exerts a large impact on the atmospheric environment over CEC, while the regional O3 transport and photochemical productions dominate the lower troposphere over CEC with less impact of stratospheric intrusion from the TCs in the tropical ocean region. These results present the climatology of tropospheric O3 anomalies in China induced by the TCs over the Northwest Pacific with enhancing our comprehension of the meteorological impact on O3 variations over the East Asian monsoon region.