{"title":"电离层-地面区域由带电云引起的电场的准直流模型","authors":"P.T. Tonev, P.I.Y. Velinov","doi":"10.1016/0021-9169(95)00112-3","DOIUrl":null,"url":null,"abstract":"<div><p>The penetration of the quasi-DC electric fields, <strong>E</strong> due to electrified clouds, into the middle- and high-latitude ionosphere is theoretically studied during the initial stage of cloud charge separation. The electrification process is characterized by a source function <em>S</em>(<em>t</em>), whose variations are on the time scale of the relaxation process in the cloud. A first-order approximation solution for the time variation of <strong>E</strong> is obtained as an explicit function of the electric field in the steady-state case. Some features of the time variations of <strong>E</strong> at different altitudes (in the ionosphere and also in the atmosphere) are investigated, depending on the source function and the relaxation time constants. This result can also be applied for slowly electrifying clouds which do not produce lightning.</p></div>","PeriodicalId":100754,"journal":{"name":"Journal of Atmospheric and Terrestrial Physics","volume":"58 10","pages":"Pages 1117-1124"},"PeriodicalIF":0.0000,"publicationDate":"1996-07-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://sci-hub-pdf.com/10.1016/0021-9169(95)00112-3","citationCount":"7","resultStr":"{\"title\":\"A quasi-DC model of electric fields in the ionosphere-ground region due to electrified clouds\",\"authors\":\"P.T. Tonev, P.I.Y. Velinov\",\"doi\":\"10.1016/0021-9169(95)00112-3\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><p>The penetration of the quasi-DC electric fields, <strong>E</strong> due to electrified clouds, into the middle- and high-latitude ionosphere is theoretically studied during the initial stage of cloud charge separation. The electrification process is characterized by a source function <em>S</em>(<em>t</em>), whose variations are on the time scale of the relaxation process in the cloud. A first-order approximation solution for the time variation of <strong>E</strong> is obtained as an explicit function of the electric field in the steady-state case. Some features of the time variations of <strong>E</strong> at different altitudes (in the ionosphere and also in the atmosphere) are investigated, depending on the source function and the relaxation time constants. This result can also be applied for slowly electrifying clouds which do not produce lightning.</p></div>\",\"PeriodicalId\":100754,\"journal\":{\"name\":\"Journal of Atmospheric and Terrestrial Physics\",\"volume\":\"58 10\",\"pages\":\"Pages 1117-1124\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"1996-07-01\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"https://sci-hub-pdf.com/10.1016/0021-9169(95)00112-3\",\"citationCount\":\"7\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Journal of Atmospheric and Terrestrial Physics\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://www.sciencedirect.com/science/article/pii/0021916995001123\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Journal of Atmospheric and Terrestrial Physics","FirstCategoryId":"1085","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/0021916995001123","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
A quasi-DC model of electric fields in the ionosphere-ground region due to electrified clouds
The penetration of the quasi-DC electric fields, E due to electrified clouds, into the middle- and high-latitude ionosphere is theoretically studied during the initial stage of cloud charge separation. The electrification process is characterized by a source function S(t), whose variations are on the time scale of the relaxation process in the cloud. A first-order approximation solution for the time variation of E is obtained as an explicit function of the electric field in the steady-state case. Some features of the time variations of E at different altitudes (in the ionosphere and also in the atmosphere) are investigated, depending on the source function and the relaxation time constants. This result can also be applied for slowly electrifying clouds which do not produce lightning.