{"title":"Variations in the Thermosphere During the 2018 SSW Event at Beijing and Wuhan","authors":"Shaoyang Li, Zhipeng Ren, Tingting Yu, Guozhu Li, Xinan Yue, Libo Liu, Yong Wei, Xing Li","doi":"10.1029/2025JA033767","DOIUrl":null,"url":null,"abstract":"<p>Daytime thermospheric responses to the 2018 sudden stratospheric warming (SSW) are investigated in this study. The method proposed by Li et al. (2023), https://doi.org/10.1029/2022ja030988 for deriving exospheric temperature (Tex) from electron density (Ne) profiles was employed. Reliability of this method was verified through comparisons with observations from incoherent scatter radar and the Swarm-C satellite, showing Tex relative deviations within ±2% at most cases. At Beijing, SSW effects manifested as cooling, with a reduction in average Tex by −1–−17 K and average neutral density decreasing by 3%–15% compared to non-SSW. Differently, at Wuhan, SSW effects exhibited semi-diurnal-like variations consistent with previous studies. Average Tex increased by up to 13 and 9 K, and average neutral density increased by up to ∼13% and ∼5% near the dawn and dusk sectors, respectively. Decreases of up to −15 K and ∼−12% were observed near the noon sector. These distinct characteristics, including latitude-dependence and semi-diurnal-like variations, highlight the role of SSW in modulating the thermosphere, providing an opportunity to better understand the vertical coupling between different atmospheric regions.</p>","PeriodicalId":15894,"journal":{"name":"Journal of Geophysical Research: Space Physics","volume":"130 4","pages":""},"PeriodicalIF":2.6000,"publicationDate":"2025-03-30","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Journal of Geophysical Research: Space Physics","FirstCategoryId":"89","ListUrlMain":"https://onlinelibrary.wiley.com/doi/10.1029/2025JA033767","RegionNum":2,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q2","JCRName":"ASTRONOMY & ASTROPHYSICS","Score":null,"Total":0}
引用次数: 0
Abstract
Daytime thermospheric responses to the 2018 sudden stratospheric warming (SSW) are investigated in this study. The method proposed by Li et al. (2023), https://doi.org/10.1029/2022ja030988 for deriving exospheric temperature (Tex) from electron density (Ne) profiles was employed. Reliability of this method was verified through comparisons with observations from incoherent scatter radar and the Swarm-C satellite, showing Tex relative deviations within ±2% at most cases. At Beijing, SSW effects manifested as cooling, with a reduction in average Tex by −1–−17 K and average neutral density decreasing by 3%–15% compared to non-SSW. Differently, at Wuhan, SSW effects exhibited semi-diurnal-like variations consistent with previous studies. Average Tex increased by up to 13 and 9 K, and average neutral density increased by up to ∼13% and ∼5% near the dawn and dusk sectors, respectively. Decreases of up to −15 K and ∼−12% were observed near the noon sector. These distinct characteristics, including latitude-dependence and semi-diurnal-like variations, highlight the role of SSW in modulating the thermosphere, providing an opportunity to better understand the vertical coupling between different atmospheric regions.