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| DOI | 10.5194/acp-21-18573-2021 |
| Linkages between the atmospheric transmission originating from the North Atlantic Oscillation and persistent winter haze over Beijing | |
| Li M.; Yao Y.; Simmonds I.; Luo D.; Zhong L.; Pei L. | |
| 发表日期 | 2021 |
| ISSN | 1680-7316 |
| 起始页码 | 18573 |
| 结束页码 | 18588 |
| 卷号 | 21期号:24 |
| 英文摘要 | In this study, the persistent winter haze that occurred over Beijing during 1980 to 2016 is examined using reanalysis and station data. On both interannual and daily-to-weekly timescales, the winter haze weather in Beijing is found to be associated with a pronounced atmospheric teleconnection pattern from the North Atlantic to Eurasia (Beijing). A positive western-type North Atlantic Oscillation (WNAO+) phase and a positive East Atlantic/West Russia (EA/WR+) phase are observed as part of this teleconnection pattern (an arched wave train). This study focuses on the role of the WNAO pattern, because the WNAO+ pattern acts as the origin of the atmospheric transmission, 8-10 d before the persistent haze events. Further analyses reveal that the WNAO+ pattern can increase the number of haze days and persistent haze events on interannual and daily-to-weekly timescales. Specifically, strong WNAO+ winters (above the 95th percentile) can increase the number of haze days and persistent haze events by 26.0% and 42.3%, respectively. In addition, a high WNAO index for the 5 d average (above the 95th percentile) predicts a 16.9% increase in the probability of haze days on Day 8 and a higher proportion of persistent haze days compared with an unknown WNAO state. Thus, the WNAO+ pattern is as a necessary prior background condition for the formation of the wave train and is a skillful predictor for persistent hazy weather. Corresponding to the WNAO+ pattern, intensified zonal wind and a north-south sea surface temperature tripolar mode over the North Atlantic also appear before persistent haze events on the daily-to-weekly timescale. On the interannual timescale, winters with a greater number of persistent haze days are also associated with a tripolar sea surface temperature (SST) mode over the North Atlantic that is situated farther northward. © 2021 Muyuan Li et al. |
| 语种 | 英语 |
| 来源期刊 | ATMOSPHERIC CHEMISTRY AND PHYSICS
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| 文献类型 | 期刊论文 |
| 条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/246347 |
| 作者单位 | Public Meteorological Service Center, China Meteorological Administration, Beijing, 100081, China; Key Laboratory of Regional Climate-Environment for Temperate East Asia, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing, 100029, China; University of Chinese Academy of Sciences, Beijing, 100049, China; School of Geography Earth and Atmospheric Sciences, University of Melbourne, Parkville, VIC 3010, Australia; National Institute of Natural Hazards, Ministry of Emergency Management of China, Beijing, 100085, China; Institute of Urban Meteorology, China Meteorological Administration, Beijing, 100089, China |
| 推荐引用方式 GB/T 7714 | Li M.,Yao Y.,Simmonds I.,et al. Linkages between the atmospheric transmission originating from the North Atlantic Oscillation and persistent winter haze over Beijing[J],2021,21(24). |
| APA | Li M.,Yao Y.,Simmonds I.,Luo D.,Zhong L.,&Pei L..(2021).Linkages between the atmospheric transmission originating from the North Atlantic Oscillation and persistent winter haze over Beijing.ATMOSPHERIC CHEMISTRY AND PHYSICS,21(24). |
| MLA | Li M.,et al."Linkages between the atmospheric transmission originating from the North Atlantic Oscillation and persistent winter haze over Beijing".ATMOSPHERIC CHEMISTRY AND PHYSICS 21.24(2021). |
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