文献类型：期刊文献

英文题名：The Impact of Different Types of El Ni?o Events on the Ozone Valley of the Tibetan Plateau Based on the WACCM4 Mode

作者：Wan, Yishun[1];Xu, Feng[1];Chang, Shujie[1,2];Wan, Lingfeng[3];Li, Yongchi[1]

机构：[1]Guangdong Ocean Univ, South China Sea Inst Marine Meteorol, Coll Ocean & Meteorol, Lab Coastal Ocean Variat & Disaster Predict,Key La, Zhanjiang 524088, Peoples R China;[2]Univ Leeds, Sch Earth & Environm, Leeds LS2 9JT, England;[3]Ocean Univ China, Inst Adv Ocean Study IAOS, Frontier Sci Ctr Deep Ocean Multispheres & Earth S, Phys Oceanog Lab POL, Qingdao 266100, Peoples R China

年份：2024

卷号：14

期号：3

外文期刊名：APPLIED SCIENCES-BASEL

收录：SCI-EXPANDED(收录号：WOS:001160117100001)、、WOS

基金：The authors would like to thank the editors and the reviewers for their valuable suggestions.

语种：英文

外文关键词：El Nino; ozone valley; Tibetan Plateau; WACCM

外文摘要：This study integrates the sea surface temperature, ozone and meteorological data of ERA5 to count the El Nino events since 1979 and has classified these events into eastern and central types in space as well as spring and summer types in time. The impacts of different types of El Nino events on the ozone valley of the Tibetan Plateau are discussed. The eastern (and spring) type of El Nino events are generally more intense and longer in duration than the central (and summer) type of El Nino events. Overall, in the summer of the following year after El Nino events, the total column ozone (TCO) anomalies near the Tibetan Plateau have a regular zonal distribution. At low latitudes, TCO exhibits negative anomalies, which become more negative approaching the equator. The TCO in the region north of 30 degrees N mainly shows positive anomalies with the high-value region around 40 degrees N. The responses of ozone to different types of El Nino events over the Tibetan Plateau are different, which is further validated by the WACCM4 simulation results. The greater intensity of the eastern (and spring) type of El Nino events caused stronger upward movement of the middle and upper atmosphere in the 20 degrees N region in the subsequent summer as well as a stronger South Asian High. These have resulted in a wider range of negative TCO anomalies in the southern low-latitude region of the South Asian High. In addition, the growing intensity of El Nino extreme events over more than half a century warrants significant concern.