{"title":"葡萄牙内地闪电概率预测","authors":"João Rio, S. Correia, M. Lopes","doi":"10.31978/639-19-010-0.199","DOIUrl":null,"url":null,"abstract":"• A study based on 13 years of lightning data is presented using Cloud-to-Ground (CG) flash density maps on a 0.2°x0.2° resolution grid (Fig.1), as well as intra annual distributions (Fig.2). Thunderstorm events in mainland Portugal result primarily from frontal systems approaching in the winter/spring seasons and convective instability in the summer/autumn seasons, especially due to diurnal surface heating, particularly observed during the months of May to September.","PeriodicalId":166428,"journal":{"name":"Sexto Simposio Nacional de Predicción \"Memorial Antonio Mestre\"","volume":"124 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"1900-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Lightning probability forecast in Mainland Portugal\",\"authors\":\"João Rio, S. Correia, M. Lopes\",\"doi\":\"10.31978/639-19-010-0.199\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"• A study based on 13 years of lightning data is presented using Cloud-to-Ground (CG) flash density maps on a 0.2°x0.2° resolution grid (Fig.1), as well as intra annual distributions (Fig.2). Thunderstorm events in mainland Portugal result primarily from frontal systems approaching in the winter/spring seasons and convective instability in the summer/autumn seasons, especially due to diurnal surface heating, particularly observed during the months of May to September.\",\"PeriodicalId\":166428,\"journal\":{\"name\":\"Sexto Simposio Nacional de Predicción \\\"Memorial Antonio Mestre\\\"\",\"volume\":\"124 1\",\"pages\":\"0\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"1900-01-01\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Sexto Simposio Nacional de Predicción \\\"Memorial Antonio Mestre\\\"\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.31978/639-19-010-0.199\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Sexto Simposio Nacional de Predicción \"Memorial Antonio Mestre\"","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.31978/639-19-010-0.199","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
Lightning probability forecast in Mainland Portugal
• A study based on 13 years of lightning data is presented using Cloud-to-Ground (CG) flash density maps on a 0.2°x0.2° resolution grid (Fig.1), as well as intra annual distributions (Fig.2). Thunderstorm events in mainland Portugal result primarily from frontal systems approaching in the winter/spring seasons and convective instability in the summer/autumn seasons, especially due to diurnal surface heating, particularly observed during the months of May to September.
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