{"title":"与部分逆转的赤道电喷流有关的电流系统的鉴定","authors":"M. James, R. G. Rastogi, D. Rao","doi":"10.5636/JGG.49.633","DOIUrl":null,"url":null,"abstract":"An abnormality among a series of geomagnetic quiescent days during July 1978 has been identified on 26 July using geomagnetic data from a network of 13 observatories in Indo-Russian longitude belt. This abnormality has been explained by invoking an additional clockwise loop current system centered around 5° dip latitude superimposed on the normal Sq current system centered at 20° dip latitude, thereby shifting the focus of the combined current system to 35° dip latitude. Probable causes of this additional currents in the low-latitude have been discussed.","PeriodicalId":156587,"journal":{"name":"Journal of geomagnetism and geoelectricity","volume":"49 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"1997-05-20","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"3","resultStr":"{\"title\":\"Identification of the current system associated with a partially reversed equatorial electrojet\",\"authors\":\"M. James, R. G. Rastogi, D. Rao\",\"doi\":\"10.5636/JGG.49.633\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"An abnormality among a series of geomagnetic quiescent days during July 1978 has been identified on 26 July using geomagnetic data from a network of 13 observatories in Indo-Russian longitude belt. This abnormality has been explained by invoking an additional clockwise loop current system centered around 5° dip latitude superimposed on the normal Sq current system centered at 20° dip latitude, thereby shifting the focus of the combined current system to 35° dip latitude. Probable causes of this additional currents in the low-latitude have been discussed.\",\"PeriodicalId\":156587,\"journal\":{\"name\":\"Journal of geomagnetism and geoelectricity\",\"volume\":\"49 1\",\"pages\":\"0\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"1997-05-20\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"3\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Journal of geomagnetism and geoelectricity\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.5636/JGG.49.633\",\"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 geomagnetism and geoelectricity","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.5636/JGG.49.633","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
Identification of the current system associated with a partially reversed equatorial electrojet
An abnormality among a series of geomagnetic quiescent days during July 1978 has been identified on 26 July using geomagnetic data from a network of 13 observatories in Indo-Russian longitude belt. This abnormality has been explained by invoking an additional clockwise loop current system centered around 5° dip latitude superimposed on the normal Sq current system centered at 20° dip latitude, thereby shifting the focus of the combined current system to 35° dip latitude. Probable causes of this additional currents in the low-latitude have been discussed.