{"title":"层状雨和对流雨中雨滴形态、大小和倾斜角分布:若干实例及其对XPD-CPA关系的影响","authors":"M. Thurai, V. Bringi, Gwo-Jong Huang","doi":"10.1109/ANTEM.2010.5552528","DOIUrl":null,"url":null,"abstract":"1-minute drop size distributions in rain from measurements using 2D video disdrometer are used to identify stratiform and convective rain, and the respective drop shapes are examined separately. Canting angle distributions have also been determined in stratiform rain, under low wind conditions and confirmed independently using polarimetric radar based estimates. Studies are ongoing in this area.","PeriodicalId":161657,"journal":{"name":"2010 14th International Symposium on Antenna Technology and Applied Electromagnetics & the American Electromagnetics Conference","volume":"32 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"2010-07-05","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Drop shape, size and canting angle Distributions in stratiform and convective rain: Some examples and their impact on XPD-CPA relation\",\"authors\":\"M. Thurai, V. Bringi, Gwo-Jong Huang\",\"doi\":\"10.1109/ANTEM.2010.5552528\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"1-minute drop size distributions in rain from measurements using 2D video disdrometer are used to identify stratiform and convective rain, and the respective drop shapes are examined separately. Canting angle distributions have also been determined in stratiform rain, under low wind conditions and confirmed independently using polarimetric radar based estimates. Studies are ongoing in this area.\",\"PeriodicalId\":161657,\"journal\":{\"name\":\"2010 14th International Symposium on Antenna Technology and Applied Electromagnetics & the American Electromagnetics Conference\",\"volume\":\"32 1\",\"pages\":\"0\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"2010-07-05\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"2010 14th International Symposium on Antenna Technology and Applied Electromagnetics & the American Electromagnetics Conference\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.1109/ANTEM.2010.5552528\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"2010 14th International Symposium on Antenna Technology and Applied Electromagnetics & the American Electromagnetics Conference","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.1109/ANTEM.2010.5552528","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
Drop shape, size and canting angle Distributions in stratiform and convective rain: Some examples and their impact on XPD-CPA relation
1-minute drop size distributions in rain from measurements using 2D video disdrometer are used to identify stratiform and convective rain, and the respective drop shapes are examined separately. Canting angle distributions have also been determined in stratiform rain, under low wind conditions and confirmed independently using polarimetric radar based estimates. Studies are ongoing in this area.