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{"title":"积雨云微物理过程的数值模拟——(一)微物理模式","authors":"胡志晋, 何观芳","doi":"10.11676/QXXB1987.060","DOIUrl":null,"url":null,"abstract":"本文提出了一个比较完整的层状云参数化微物理方程组。根据理论和实验结果推导了18种层状云中常见的微物理过程中云滴、雨滴、冰晶、雪团和霰的群体比水量和比浓度的转化率,它们包括凝结(蒸发)、凝华、碰并、聚合、凇附、冰晶的核化、繁生以及冰—霰、雪—霰、云—雨的自动转化率等。","PeriodicalId":50890,"journal":{"name":"Acta Meteorologica Sinica","volume":null,"pages":null},"PeriodicalIF":0.0000,"publicationDate":"2013-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"4","resultStr":"{\"title\":\"积雨云微物理过程的数值模拟——(一)微物理模式\",\"authors\":\"胡志晋, 何观芳\",\"doi\":\"10.11676/QXXB1987.060\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"本文提出了一个比较完整的层状云参数化微物理方程组。根据理论和实验结果推导了18种层状云中常见的微物理过程中云滴、雨滴、冰晶、雪团和霰的群体比水量和比浓度的转化率,它们包括凝结(蒸发)、凝华、碰并、聚合、凇附、冰晶的核化、繁生以及冰—霰、雪—霰、云—雨的自动转化率等。\",\"PeriodicalId\":50890,\"journal\":{\"name\":\"Acta Meteorologica Sinica\",\"volume\":null,\"pages\":null},\"PeriodicalIF\":0.0000,\"publicationDate\":\"2013-01-01\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"4\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Acta Meteorologica Sinica\",\"FirstCategoryId\":\"1089\",\"ListUrlMain\":\"https://doi.org/10.11676/QXXB1987.060\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q2\",\"JCRName\":\"Engineering\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Acta Meteorologica Sinica","FirstCategoryId":"1089","ListUrlMain":"https://doi.org/10.11676/QXXB1987.060","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q2","JCRName":"Engineering","Score":null,"Total":0}
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