M. Lacerda, R. Jaques, Marcelo Magalhaes Fares Saba, D. R. Campos, Kleber Pinheiro Nacaratto
{"title":"南美地区梅吉曲线的比较","authors":"M. Lacerda, R. Jaques, Marcelo Magalhaes Fares Saba, D. R. Campos, Kleber Pinheiro Nacaratto","doi":"10.1109/SIPDA.2013.6729198","DOIUrl":null,"url":null,"abstract":"In this paper we obtained the “Carnegie's” curve for South America by using data from a global lightning detection system in a scale of seconds. Carnegie's curve is a measurement of electrical activity of the planet. It can be obtained by direct averaging the measurements of electric field (in a scale of hours) [1], or can be obtained (in the same scale of time) from lightning activity [2], [3], [4]. The lightning data used to monitor lightning activity in this study was recorded by the sensors of the BrasilDAT lightning location system. The dataset consists of cloud and cloud-to-ground discharges detected within a 100km-radius circle centered on latitude -23.4587° and longitude -46.7667°, corresponding to an area in and around the city of São Paulo, SP, Brazil. The methodology consists of calculating the Carnegie's curve in a scale of hours, plotting the lightning activity data collected of BrasilDAT.","PeriodicalId":216871,"journal":{"name":"2013 International Symposium on Lightning Protection (XII SIPDA)","volume":"21 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"2013-10-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"1","resultStr":"{\"title\":\"Comparison of camegie's curve for South America\",\"authors\":\"M. Lacerda, R. Jaques, Marcelo Magalhaes Fares Saba, D. R. Campos, Kleber Pinheiro Nacaratto\",\"doi\":\"10.1109/SIPDA.2013.6729198\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"In this paper we obtained the “Carnegie's” curve for South America by using data from a global lightning detection system in a scale of seconds. Carnegie's curve is a measurement of electrical activity of the planet. It can be obtained by direct averaging the measurements of electric field (in a scale of hours) [1], or can be obtained (in the same scale of time) from lightning activity [2], [3], [4]. The lightning data used to monitor lightning activity in this study was recorded by the sensors of the BrasilDAT lightning location system. The dataset consists of cloud and cloud-to-ground discharges detected within a 100km-radius circle centered on latitude -23.4587° and longitude -46.7667°, corresponding to an area in and around the city of São Paulo, SP, Brazil. The methodology consists of calculating the Carnegie's curve in a scale of hours, plotting the lightning activity data collected of BrasilDAT.\",\"PeriodicalId\":216871,\"journal\":{\"name\":\"2013 International Symposium on Lightning Protection (XII SIPDA)\",\"volume\":\"21 1\",\"pages\":\"0\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"2013-10-01\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"1\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"2013 International Symposium on Lightning Protection (XII SIPDA)\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.1109/SIPDA.2013.6729198\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"2013 International Symposium on Lightning Protection (XII SIPDA)","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.1109/SIPDA.2013.6729198","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
In this paper we obtained the “Carnegie's” curve for South America by using data from a global lightning detection system in a scale of seconds. Carnegie's curve is a measurement of electrical activity of the planet. It can be obtained by direct averaging the measurements of electric field (in a scale of hours) [1], or can be obtained (in the same scale of time) from lightning activity [2], [3], [4]. The lightning data used to monitor lightning activity in this study was recorded by the sensors of the BrasilDAT lightning location system. The dataset consists of cloud and cloud-to-ground discharges detected within a 100km-radius circle centered on latitude -23.4587° and longitude -46.7667°, corresponding to an area in and around the city of São Paulo, SP, Brazil. The methodology consists of calculating the Carnegie's curve in a scale of hours, plotting the lightning activity data collected of BrasilDAT.