LIU Ding-Wei, WANG Hui, HUANG Tao, CAO Xue, ZHANG Ke-Deng
{"title":"亚暴期间等离子体和中性速度的时空变化","authors":"LIU Ding-Wei, WANG Hui, HUANG Tao, CAO Xue, ZHANG Ke-Deng","doi":"10.1002/cjg2.20244","DOIUrl":null,"url":null,"abstract":"<p>This study statistically investigates the temporal and spatial variations of plasma convection velocity (<i>V</i><sub><i>y</i></sub>) and thermospheric zonal wind velocity (<i>U</i><sub><i>y</i></sub>) in the range of –4 hour (h) and +2 h MLT relative to substorm onsets (MLT onset) with both CHAMP and DMSP (F13, F15) satellites observations from 2001 to 2005. It shows that <i>V</i><sub><i>y</i></sub> increase significantly in all MLT sectors and the latitudes of the peak values move equatorward in 1.5 h after substorm onsets. In the subsequent 1.5 h <i>V</i><sub><i>y</i></sub> decrease in intensity and the peaks retreat poleward, which shows that the onsets of substorm can enhance the plasma convection velocity dramatically. The relative increase of <i>V</i><sub><i>y</i></sub> is largest from –2 h to MLT onset, which indicates that the substorm mainly affects the thermosphere in the westward 0∼2 h MLT sector. <i>U</i><sub><i>y</i></sub> increases steadily in 3 hours after substorm onsets, with a 1.5 h delay relative to <i>V</i><sub><i>y</i></sub> in response to the substorm onsets.</p>","PeriodicalId":100242,"journal":{"name":"Chinese Journal of Geophysics","volume":"59 4","pages":"395-403"},"PeriodicalIF":0.0000,"publicationDate":"2016-10-10","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://sci-hub-pdf.com/10.1002/cjg2.20244","citationCount":"0","resultStr":"{\"title\":\"TEMPORAL AND SPATIAL VARIATIONS OF PLASMA AND NEUTRAL VELOCITIES DURING SUBSTORM PERIODS\",\"authors\":\"LIU Ding-Wei, WANG Hui, HUANG Tao, CAO Xue, ZHANG Ke-Deng\",\"doi\":\"10.1002/cjg2.20244\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<p>This study statistically investigates the temporal and spatial variations of plasma convection velocity (<i>V</i><sub><i>y</i></sub>) and thermospheric zonal wind velocity (<i>U</i><sub><i>y</i></sub>) in the range of –4 hour (h) and +2 h MLT relative to substorm onsets (MLT onset) with both CHAMP and DMSP (F13, F15) satellites observations from 2001 to 2005. It shows that <i>V</i><sub><i>y</i></sub> increase significantly in all MLT sectors and the latitudes of the peak values move equatorward in 1.5 h after substorm onsets. In the subsequent 1.5 h <i>V</i><sub><i>y</i></sub> decrease in intensity and the peaks retreat poleward, which shows that the onsets of substorm can enhance the plasma convection velocity dramatically. The relative increase of <i>V</i><sub><i>y</i></sub> is largest from –2 h to MLT onset, which indicates that the substorm mainly affects the thermosphere in the westward 0∼2 h MLT sector. <i>U</i><sub><i>y</i></sub> increases steadily in 3 hours after substorm onsets, with a 1.5 h delay relative to <i>V</i><sub><i>y</i></sub> in response to the substorm onsets.</p>\",\"PeriodicalId\":100242,\"journal\":{\"name\":\"Chinese Journal of Geophysics\",\"volume\":\"59 4\",\"pages\":\"395-403\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"2016-10-10\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"https://sci-hub-pdf.com/10.1002/cjg2.20244\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Chinese Journal of Geophysics\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://onlinelibrary.wiley.com/doi/10.1002/cjg2.20244\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Chinese Journal of Geophysics","FirstCategoryId":"1085","ListUrlMain":"https://onlinelibrary.wiley.com/doi/10.1002/cjg2.20244","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
TEMPORAL AND SPATIAL VARIATIONS OF PLASMA AND NEUTRAL VELOCITIES DURING SUBSTORM PERIODS
This study statistically investigates the temporal and spatial variations of plasma convection velocity (Vy) and thermospheric zonal wind velocity (Uy) in the range of –4 hour (h) and +2 h MLT relative to substorm onsets (MLT onset) with both CHAMP and DMSP (F13, F15) satellites observations from 2001 to 2005. It shows that Vy increase significantly in all MLT sectors and the latitudes of the peak values move equatorward in 1.5 h after substorm onsets. In the subsequent 1.5 h Vy decrease in intensity and the peaks retreat poleward, which shows that the onsets of substorm can enhance the plasma convection velocity dramatically. The relative increase of Vy is largest from –2 h to MLT onset, which indicates that the substorm mainly affects the thermosphere in the westward 0∼2 h MLT sector. Uy increases steadily in 3 hours after substorm onsets, with a 1.5 h delay relative to Vy in response to the substorm onsets.